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other provinces and regions in Vietnam and other country.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Address\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Headquarters of Can Tho Journal of Medicine and Pharmacy, located Scientific Research and International Cooperation Office: 179 Nguyen Van Cu Street, An Khanh Ward, Ninh Kieu District, Can Tho City, Vietnam.\u003C\u002Fspan>\u003C\u002Fp>","\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Ngày 16\u002F7\u002F2015, Tạp chí Y Dược học Cần Thơ được cấp chỉ số quốc tế: ISSN 2354-1210.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 4\u002F2016, Tạp chí đã được Hội đồng Giáo sư ngành Y đưa vào danh sách các tạp chí khoa học Y học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Năm 2020 Tạp chí Y Dược học Cần Thơ đã được phê duyệt vào danh mục của các Hội đồng Giáo sư ngành Dược học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ ra 12 số\u002Fnăm, 180-200 trang\u002Fsố.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 12\u002F2022 Tạp chí Y Dược học Cần Thơ là thành viên của hệ thống Crossref và từ tháng 01\u002F2023 tạp chí thực hiện bình duyệt online kín 2 chiều nhằm tăng tính minh bạch, tin cậy của các công trình nghiên cứu khoa học và đảm bảo tốt nhất chất lượng khoa học của bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ, mục đích và phạm vi của tạp chí\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ và mục đích hoạt động của tạp chí: xuất bản nhằm mục đích phổ biến kết quả từ các đề tài nghiên cứu khoa học; giao lưu trao đổi khoa học, chia sẻ kinh nghiệm, học tập, đồng thời cập nhật thông tin khoa học mới trong các lĩnh vực y, sinh, dược học trong và ngoài nước.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phạm vi của tạp chí: Tạp chí xuất bản được chia thành 3 chuyên mục: (i) Bài báo nghiên cứu khoa học là kết quả công trình nghiên cứu khoa học có giá trị đã được triển khai nghiên cứu, (ii) Bài tổng quan y, sinh, dược học: phục vụ mục tiêu đào tạo liên tục trong lĩnh vực y, sinh, dược học; nhằm hệ thống hóa những kiến thức kinh điển và hiện đại; (iii) Thông tin cập nhật kiến thức mới về y, sinh, dược học trong nước và trên thế giới.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Chính sách truy cập mở\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ áp dụng chính sách truy cập mở đối với các bài báo đã xuất bản đến với độc giả, nhằm mở rộng cơ hội tiếp cận các kết quả nghiên cứu chất lượng cao và tăng cường trao đổi kiến thức. Tạp chí đăng tải trực tuyến (miễn phí) toàn văn các bài báo được công bố trên website của Tạp chí (https:\u002F\u002Ftapchi.ctump.edu.vn).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đạo đức xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ cam kết tuân thủ đạo đức xuất bản phù hợp với các hướng dẫn và tiêu chuẩn của the Committee on Publication Ethics (COPE), tuân thủ các nguyên tắc của COPE’s Core Practices, Best Practices Guidelines for Journal Editors và Guidelines on Good Publication Practices.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Bản thảo bài báo chỉ được chấp nhận khi được tác giả chịu trách nhiệm chính cam kết các nội dung sau: Các nội dung của bản thảo chưa được đăng tải toàn bộ hoặc một phần ở các tạp chí khác; Tất cả các tác giả đều có đóng góp một cách đáng kể vào quá trình nghiên cứu hoặc chuẩn bị bản thảo và cùng chịu trách nhiệm về các nội dung của bản thảo; Tuân thủ các biện pháp đảm bảo đạo đức nghiên cứu (ví dụ thỏa thuận đồng ý tham gia nghiên cứu).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Cam kết bảo mật\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí cam kết thực hiện và tuân thủ các quy định của luật và các văn bản hướng dẫn liên quan đến bảo mật thông tin cá nhân trên không gian mạng. Các thông tin mà người dùng (tác giả, độc giả, biên tập viên, người phản biện) nhập vào các biểu mẫu trên Hệ thống Quản lý xuất bản trực tuyến của tạp chí chỉ được sử dụng vào các mục đích đã được tuyên bố rõ ràng và sẽ không được cung cấp cho bất kỳ bên thứ ba nào khác, hay dùng vào bất kỳ mục đích nào khác.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phí gửi bài\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng bài: 1.000.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng nhanh: 1.500.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với tác giả là cán bộ viên chức thuộc Trường Đại học Y Dược Cần Thơ thì được hỗ trợ 50% lệ phí gửi đăng bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với sinh viên thực hiện đề tài nghiên cứu khoa học cấp trường được hỗ trợ 100% lệ phí đăng bài ( Tác giả gửi đính kèm “ Quyết định về việc giao tổ chức thực hiện đề tài nghiên cứu khoa học cấp Trường của sinh viên”).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Hình thức nộp lệ phí:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Tiền mặt:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Nộp trực tiếp tại Phòng Tài chính - Kế toán, Trường Đại học Y Dược Cần Thơ, số 179 Nguyễn Văn Cừ, P. An Khánh, Q. Ninh Kiều, thành phố Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Chuyển khoản:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tên Tài khoản: Trường ĐHYD Cần Thơ, Số TK: 0111000115668, tại ngân hàng Vietcombank chi nhánh Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Thời gian: Áp dụng từ ngày 01\u002F02\u002F2023.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">* Phí gửi bài không được hoàn trả khi bài viết bị từ chối hoặc tác giả xin rút bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Quy trình phản biện bài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ thực hiện quy trình phản biện kín hai chiều nghiêm ngặt. Danh tính của những người phản biện không được tiết lộ cho các tác giả và ngược lại. Quy trình thẩm định bài báo đăng gồm các bước sau:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tiếp nhận bản thảo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tác giả liên hệ gửi bản thảo đến Tạp chí qua hệ thống trực tuyến tại website: https:\u002F\u002Ftapchi.ctump.edu.vn. Hướng dẫn về cách đăng ký, gửi bài và chuẩn bị bản thảo được cung cấp trên website của Tạp chí.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sàng lọc sơ bộ\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sau khi Tòa soạn nhận được bài báo của tác giả, Ban Thư ký sẽ tiến hành kiểm tra sơ bộ bài báo (các yêu cầu về nội dung và hình thức). Những bài báo không đúng quy cách hoặc có nội dung không phù hợp hoặc vi phạm bản quyền sẽ bị từ chối (Ban Thư ký thông báo phản hồi đến tác giả trong vòng 1 tuần). Những bài báo đủ điều kiện, được Ban Thư ký tòa soạn chuyển đến Ban Biên tập có cùng chuyên môn với nội dung bài báo để đề xuất người phản biện. Thời gian kể từ khi Ban Biên tập nhận bài báo đến khi đề xuất người phản biện bài báo chậm nhất là 5 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Vòng phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký gửi bài và yêu cầu phản biện đến 02 phản biện độc lập.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Các phản biện gởi nhận xét cho Ban Thư ký. Thời gian từ khi gửi bài cho phản biện đến khi nhận ý kiến của phản biện tối đa là 20 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xử ký kết quả phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Nếu ý kiến đồng ý cho đăng và không cần chỉnh sửa, Ban Thư ký tiếp tục đăng bài theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Nếu ý kiến đồng ý đăng và cần chỉnh sửa, Ban Thư ký sẽ thông tin đến tác giả chỉnh sửa theo yêu cầu của người phản biện. Thời gian chỉnh sửa và gửi lại kéo dài không quá 2 tuần, từ khi tác giả bài báo nhận được thông tin (Quá trình này có thể lặp lại tối đa 2 lần\u002F1 bài báo). Khi có sự thống nhất, đồng ý của người phản biện; bài báo được tiếp tục đăng theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Những bài báo có chất lượng không đạt yêu cầu, cả 2 phản biện không đồng ý cho đăng sẽ bị Tòa soạn từ chối đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký tổng hợp các bản thảo đã được tác giả hoàn thiện sau thẩm định trình Ban Biên tập xem xét, Tổng Biên tập phê duyệt, quyết định bài đăng theo các tiêu chí: sự phù hợp nội dung với tôn chỉ và mục đích, thể loại bài viết (ưu tiên các bài có bài có nghiên cứu chuyên sâu, hàm lượng khoa học cao), đóng góp mới bài báo, bài báo được ưu tiên đăng trong số gần nhất của Tạp chí theo thứ tự: tính thời sự, chất lượng bài báo và thời gian gửi bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Ban Biên tập và Ban Thư ký biên tập bản thảo, chế bản, đọc rà soát lỗi. Thời gian hoàn thành từ 10-15 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Ban Thư ký có trách nhiệm thông báo cho tác giả bài báo (bằng e-mail) về tình hình phê duyệt bài báo, thời gian, số kỳ, tập xuất bản bài báo theo qui định.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">4. 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This has led to considerable confusion of nomenclature in the literature. This paper attempts to clarify this situation by presenting a simple classification of sedimentary density flows, based on physical flow properties and grain‐support mechanisms, and briefly discusses the likely characteristics of the deposited sediments. Cohesive flows are commonly referred to as debris flows and mud flows and defined on the basis of sediment characteristics. The boundary between cohesive and non‐cohesive density flows (frictional flows) is poorly constrained, but dimensionless numbers may be of use to define flow thresholds. Frictional flows include a continuous series from sediment slides to turbidity currents. Subdivision of these flows is made on the basis of the dominant particle‐support mechanisms, which include matrix strength (in cohesive flows), buoyancy, pore pressure, grain‐to‐grain interaction (causing dispersive pressure), Reynolds stresses (turbulence) and bed support (particles moved on the stationary bed). The dominant particle‐support mechanism depends upon flow conditions, particle concentration, grain‐size distribution and particle type. In hyperconcentrated density flows, very high sediment concentrations (>25 volume%) make particle interactions of major importance. The difference between hyperconcentrated density flows and cohesive flows is that the former are friction dominated. With decreasing sediment concentration, vertical particle sorting can result from differential settling, and flows in which this can occur are termed concentrated density flows. The boundary between hyperconcentrated and concentrated density flows is defined by a change in particle behaviour, such that denser or larger grains are no longer fully supported by grain interaction, thus allowing coarse‐grain tail (or dense‐grain tail) normal grading. The concentration at which this change occurs depends on particle size, sorting, composition and relative density, so that a single threshold concentration cannot be defined. Concentrated density flows may be highly erosive and subsequently deposit complete or incomplete Lowe and Bouma sequences. Conversely, hydroplaning at the base of debris flows, and possibly also in some hyperconcentrated flows, may reduce the fluid drag, thus allowing high flow velocities while preventing large‐scale erosion. Flows with concentrations <9% by volume are true turbidity flows (\u003Cjats:italic>sensu\u003C\u002Fjats:italic>\u003Cjats:ext-link xmlns:xlink=\"http:\u002F\u002Fwww.w3.org\u002F1999\u002Fxlink\" xlink:href=\"#b4\">Bagnold, 1962\u003C\u002Fjats:ext-link>), in which fluid turbulence is the main particle‐support mechanism. Turbidity flows and concentrated density flows can be subdivided on the basis of flow duration into instantaneous surges, longer duration surge‐like flows and quasi‐steady currents. Flow duration is shown to control the nature of the resulting deposits. Surge‐like turbidity currents tend to produce classical Bouma sequences, whose nature at any one site depends on factors such as flow size, sediment type and proximity to source. In contrast, quasi‐steady turbidity currents, generated by hyperpycnal river effluent, can deposit coarsening‐up units capped by fining‐up units (because of waxing and waning conditions respectively) and may also include thick units of uniform character (resulting from prolonged periods of near‐steady conditions). Any flow type may progressively change character along the transport path, with transformation primarily resulting from reductions in sediment concentration through progressive entrainment of surrounding fluid and\u002For sediment deposition. The rate of fluid entrainment, and consequently flow transformation, is dependent on factors including slope gradient, lateral confinement, bed roughness, flow thickness and water depth. Flows with high and low sediment concentrations may co‐exist in one transport event because of downflow transformations, flow stratification or shear layer development of the mixing interface with the overlying water (mixing cloud formation). Deposits of an individual flow event at one site may therefore form from a succession of different flow types, and this introduces considerable complexity into classifying the flow event or component flow types from the deposits.\u003C\u002Fjats:p>",{"EN":856},"The physical character of subaqueous sedimentary density flows and their deposits",{"VOID":858},"10.1046\u002Fj.1365-3091.2001.00360.x","PUBLICATION","2024-10-01T02:56:51.682+00:00","Auto 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Plenum Press New York.",{"doi":1317},"10.1007\u002F978-1-4613-3362-3_3",{"id":26,"text":1319,"url":26,"identifiers":1320},"10.1130\u002F0091-7613(1986)14\u003C581:ASTAAF>2.0.CO;2",{"doi":1319},{"id":26,"text":1322,"url":26,"identifiers":1323},"10.1126\u002Fscience.237.4820.1330",{"doi":1322},{"id":26,"text":1325,"url":26,"identifiers":1326},"10.1038\u002F341047a0",{"doi":1325},{"id":26,"text":1328,"url":26,"identifiers":1329},"10.2516\u002Fogst:1983017",{"doi":1328},{"id":26,"text":1331,"url":26,"identifiers":1332},"10.1046\u002Fj.1365-3091.1996.d01-21.x",{"doi":1331},{"id":26,"text":1334,"url":26,"identifiers":1335},"10.1111\u002Fj.1365-3091.1976.tb00047.x",{"doi":1334},{"id":26,"text":1337,"url":26,"identifiers":1338},"10.1111\u002Fj.1365-2117.1992.tb00147.x",{"doi":1337},{"id":26,"text":1340,"url":26,"identifiers":1341},"10.1017\u002FS0022112089000340",{"doi":1340},{"id":26,"text":1343,"url":26,"identifiers":1344},"10.1016\u002F0264-8172(93)90059-2",{"doi":1343},{"id":26,"text":1346,"url":26,"identifiers":1347},"Schwab W.C., 1996, Sediment mass‐flow processes on a depositional lobe, outer Mississippi fan, J. 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Res., 65, 45",{},{"id":26,"text":1429,"url":26,"identifiers":1430},"10.1016\u002Fs0169-555x(98)00021-x",{"doi":1429},false,{"id":1433,"createTime":1434,"updateTime":1434,"relativeEntities":1435,"slug":1436,"properties":1437,"entityType":859,"verifyStatus":25,"verifyTime":1434,"verifyNote":861,"syncStatus":28,"languages":1449,"translateLanguages":26,"viewCount":36,"primaryUrl":1450,"fullTextUrl":26,"authors":1451,"publicationType":902,"publisherRelationship":1490,"citationCount":770,"citationInfo":1528,"publishDate":1531,"publishYear":1532,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":1533,"isForceReanalyzing":1431},"5d79bf83-ddf0-4382-99b9-1e762e7de11e","2024-10-05T22:06:31.819+00:00",[],"Fluvial-responses-to-climate-and-sea-level-change-a-review-and-look-forward",{"mag":1438,"keywords":1440,"openalex":1441,"abstract":1443,"title":1445,"doi":1447},{"VOID":1439},"2130432031",{},{"VOID":1442},"W2130432031",{"EN":1444},"\u003Cjats:title>Summary\u003C\u002Fjats:title>\u003Cjats:p>Fluvial landforms and deposits provide one of the most readily studied Quaternary continental records, and alluvial strata represent an important component in most ancient continental interior and continental margin successions. Moreover, studies of the long‐term dynamics of fluvial systems and their responses to external or ‘allogenic' controls, can play important roles in research concerning both global change and sequence‐stratigraphy, as well as in studies of the dynamic interactions between tectonic activity and surface processes. These themes were energized in the final decades of the twentieth century, and may become increasingly important in the first decades of this millennium.\u003C\u002Fjats:p>\u003Cjats:p>This review paper provides a historical perspective on the development of ideas in the fields of geomorphology\u002FQuaternary geology vs. sedimentary geology, and then summarizes key processes that operate to produce alluvial stratigraphic records over time‐scales of 10\u003Cjats:sup>3\u003C\u002Fjats:sup>−10\u003Cjats:sup>6\u003C\u002Fjats:sup> years. Of particular interest are changes in discharge regimes, sediment supply and sediment storage en route from source terrains to sedimentary basins, as well as changes in sea‐level and the concept of accommodation. Late Quaternary stratigraphic records from the Loire (France), Mississippi (USA), Colorado (Texas, USA) and Rhine–Meuse (The Netherlands) Rivers are used to illustrate the influences of climate change on continental interior rivers, as well as the influence of interacting climate and sea‐level change on continental margin systems.\u003C\u002Fjats:p>\u003Cjats:p>The paper concludes with a look forward to a bright future for studies of fluvial response to climate and sea‐level change. At present, empirical field‐based research on fluvial response to climate and sea‐level change lags behind: (a) the global change community's understanding of the magnitude and frequency of climate and sea‐level change; (b) the sequence‐stratigraphic community's desire to interpret climate and, especially, sea‐level change as forcing mechanisms; and (c) the modelling community's ability to generate numerical and physical models of surface processes and their stratigraphic results. A major challenge for the future is to catch up, which will require the development of more detailed and sophisticated Quaternary stratigraphic, sedimentological and geochronological frameworks in a variety of continental interior and continental margin settings. There is a particular need for studies that seek to document fluvial responses to allogenic forcing over both shorter (10\u003Cjats:sup>2\u003C\u002Fjats:sup>−10\u003Cjats:sup>3\u003C\u002Fjats:sup> years) and longer (10\u003Cjats:sup>4\u003C\u002Fjats:sup>−10\u003Cjats:sup>6\u003C\u002Fjats:sup> years) time‐scales than has commonly been the case to date, as well as in larger river systems, from source to sink. Studies of Quaternary systems in depositional basin settings are especially critical because they can provide realistic analogues for interpretation of the pre‐Quaternary rock record.\u003C\u002Fjats:p>",{"EN":1446},"Fluvial responses to climate and sea‐level change: a review and look forward",{"VOID":1448},"10.1046\u002Fj.1365-3091.2000.00008.x",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1046\u002Fj.1365-3091.2000.00008.x",[1452,1473],{"id":1453,"sortIndex":115,"researcher":26,"roles":1454,"affiliations":1455,"properties":1466},"4e9c38b8-4c7c-49d6-8bff-e5864f7284b3",[],[1456],{"id":1457,"sortIndex":36,"affiliation":1458,"properties":26},"24d9d5c2-77cd-4984-892b-5f24149adee7",{"id":1459,"createTime":1460,"updateTime":1460,"relativeEntities":1461,"slug":1462,"properties":1463,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"37091bc3-b423-4a8b-b9e3-af8fc3512b63","2024-10-05T22:06:31.839+00:00",[],"Department-of-Geosciences-University-of-Nebraska-Lincoln-214-Bessey-Hall-Lincoln-",{"title":1464},{"EN":1465},"Department of Geosciences, University of Nebraska – Lincoln, 214 Bessey Hall, Lincoln,",{"openalex":1467,"orcid":1469,"title":1471},{"VOID":1468},"A5076713154",{"VOID":1470},"https:\u002F\u002Forcid.org\u002F0000-0002-1563-1716",{"EN":1472},"Torbjörn E. 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These properties are related to the physiographic occurrence and hydraulic geometry of streams and to the dynamics of flowing water as controlling sediment transport‐deposition and stream morphological activities. Based on this data, three‐dimensional facies models are presented as an aid to the identification of ancient alluvial sediments, which are briefly reviewed also.\u003C\u002Fjats:p>",{"EN":2439},"A REVIEW OF THE ORIGIN AND CHARACTERISTICS OF RECENT ALLUVIAL SEDIMENTS",{"VOID":2441},"10.1111\u002Fj.1365-3091.1965.tb01561.x","2024-10-01T02:56:49.307+00:00",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-3091.1965.tb01561.x",[2446],{"id":2447,"sortIndex":36,"researcher":26,"roles":2448,"affiliations":2449,"properties":2461},"c1810d85-e79d-42c8-9449-310ef88be149",[],[2450],{"id":2451,"sortIndex":36,"affiliation":2452,"properties":26},"d1191c5d-24e2-4b55-9363-245a74705f71",{"id":2453,"createTime":2454,"updateTime":2455,"relativeEntities":2456,"slug":2457,"properties":2458,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"59bb7f3c-7c41-45cd-9ab0-1d25fb4f3e46","2023-12-20T13:04:56.190+00:00","2024-10-01T02:56:49.325+00:00",[],"Sedimentology-Research-Laboratory-Department-of-Geology-University-of-Reading-Reading-Great-Britain",{"title":2459},{"VI":2460},"Sedimentology Research Laboratory, Department of Geology, University of Reading, Reading Great Britain",{"openalex":2462,"title":2464},{"VOID":2463},"A5103371644",{"EN":2465},"J. 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P., 1964, Experiments on small streams in alluvium. Proc. Am. Soc. Civil Engrs, , J. Hydraulics Div., 90, 1, 10.1061\u002FJYCEAJ.0001060",{"doi":2511},"10.1061\u002FJYCEAJ.0001060",{"id":26,"text":2513,"url":26,"identifiers":2514},"ADLER A. A., 1961, Bull. Mineral Ind. Expt. Sta., 1",{},{"id":26,"text":2516,"url":26,"identifiers":2517},"ALLEN J. R. L., 1962, Petrology origin and deposition of the highest Lower Old Red Sandstone of Shropshire, England, J. Sediment. Petrol., 32, 657",{},{"id":26,"text":2519,"url":26,"identifiers":2520},"10.1038\u002F1931148a0",{"doi":2519},{"id":26,"text":2522,"url":26,"identifiers":2523},"10.1002\u002Fgj.3350030101",{"doi":2522},{"id":26,"text":2525,"url":26,"identifiers":2526},"10.1002\u002Fgj.3350030201",{"doi":2525},{"id":26,"text":2528,"url":26,"identifiers":2529},"10.1111\u002Fj.1365-3091.1963.tb01204.x",{"doi":2528},{"id":26,"text":2531,"url":26,"identifiers":2532},"ALLEN J. R. L., 1963, Henry Clifton Sorby and the sedimentary structures of sands and sandstones in relation to flow conditions, Geol. Mijnbouw, 42, 223",{},{"id":26,"text":2534,"url":26,"identifiers":2535},"10.1111\u002Fj.1365-3091.1964.tb00459.x",{"doi":2534},{"id":26,"text":2537,"url":26,"identifiers":2538},"10.1111\u002Fj.1365-3091.1964.tb00635.x",{"doi":2537},{"id":26,"text":2540,"url":26,"identifiers":2541},"10.1016\u002FS0070-4571(08)70463-1",{"doi":2540},{"id":26,"text":2543,"url":26,"identifiers":2544},"10.1086\u002F627047",{"doi":2543},{"id":26,"text":2546,"url":26,"identifiers":2547},"10.1002\u002Fgj.3350040201",{"doi":2546},{"id":26,"text":2549,"url":26,"identifiers":2550},"ALLEN J. R. L., 1965, Upper Old Red Sandstone palaeogeography (Farlovian) in South Wales and the Welsh Borderland, J. Sediment. Petrol., 35, 167",{},{"id":26,"text":2552,"url":26,"identifiers":2553},"ALLEN J. R. L., 1965, Late Quaternary Niger delta, and adjacent areas: sedimentary environments and lithofacies, Bull. Am. Assoc. Petrol. Geologists, 49, 547",{},{"id":26,"text":2555,"url":26,"identifiers":2556},"ALLEN J. R. L., 1964, Cross‐stratified units, some with silt bands, in the Folkestone Beds (Lower Greensand) of Southeast England, Geol. Mijnbouw, 43, 451",{},{"id":26,"text":2558,"url":26,"identifiers":2559},"10.1017\u002FS0016756800055345",{"doi":2558},{"id":26,"text":2561,"url":26,"identifiers":2562},"10.1029\u002FTR023i002p00678",{"doi":2561},{"id":26,"text":2564,"url":26,"identifiers":2565},"ANDERSON A. G., 1953, The characteristics of sediment waves formed by flow in open channels, 379",{},{"id":26,"text":2567,"url":26,"identifiers":2568},"ANDERSON B. 1961.The Rufiji Basin Tanganyika. 7. Soils of the Main Irrigable Areas. Rept. Govt. Tanganyika Prelim. Reconnaissance Surv. Rufiji Basin 125pp.",{},{"id":26,"text":2570,"url":26,"identifiers":2571},"ANDERSON M. J., 1961, Geology and petrology of the Trivoli Sandstone in the Illinois Basin, Illinois State Geol. Surv., Circ., 316, 31",{},{"id":26,"text":2573,"url":26,"identifiers":2574},"10.2307\u002F520341",{"doi":2573},{"id":26,"text":2576,"url":26,"identifiers":2577},"ARNBORG L., 1958, The lower part of the River Ångermanälven. 1, Publ. Geograf. Inst. Univ. Uppsala, 1, 181",{},{"id":26,"text":2579,"url":26,"identifiers":2580},"BAGNOLD R. A., 1960, Some aspects of the shape of river meanders. U.S, Geol. Surv., Profess Papers, 282, 135",{},{"id":26,"text":2582,"url":26,"identifiers":2583},"BALL H. W., 1961, The Old Red Sandstone of Brown Clee Hill and adjacent area, Bull. Brit. Museum, Geol., 5, 178",{},{"id":26,"text":2585,"url":26,"identifiers":2586},"BALLADE P., 1953, Etudes des fonds sableux en Loire maritime. Nature et évolution des rides, Bull. Inform. Comité Central Océanog. Élude Côtes, 4, 163",{},{"id":26,"text":2588,"url":26,"identifiers":2589},"10.2475\u002Fajs.s4-36.215.429",{"doi":2588},{"id":26,"text":2591,"url":26,"identifiers":2592},"10.1111\u002Fj.1467-8306.1963.tb00464.x",{"doi":2591},{"id":26,"text":2594,"url":26,"identifiers":2595},"BECKMAN E. W., 1962, Flow characteristics of Elkhorn River near Waterloo, Nebraska, U.S., Geol. Surv., Water Supply Papers, 1498, 34",{},{"id":26,"text":2597,"url":26,"identifiers":2598},"10.1130\u002F0016-7606(1961)72[1029:OOCOTD]2.0.CO;2",{"doi":2597},{"id":26,"text":2600,"url":26,"identifiers":2601},"BERNARD H. A., 1963, Recent meander belt deposits of the Brazos River: an alluvial “sand” model, Bull. Am. Assoc. Petrol. Geologists, 47, 350",{},{"id":26,"text":2603,"url":26,"identifiers":2604},"BERNARD H. A., 1962, Geology of Gulf Coast and Guidebook of Excursion, 175",{},{"id":26,"text":2606,"url":26,"identifiers":2607},"BERSIER A., 1958, Examples de sédimentation cyclothématique dans l'Aquitanien de Lausanne, Eclogue Geol. Helv., 51, 842",{},{"id":26,"text":2609,"url":26,"identifiers":2610},"BERSIER A., 1958, Sequences détritiques et divagations fluviales, Eclogae Geol. Helv., 54, 854",{},{"id":26,"text":2612,"url":26,"identifiers":2613},"BIEBER C. L., 1953, Current directions indicated by cross‐bedding in deposits of early Mansfield age in southeastern Indiana, Proc. Indiana Acad. Sci., 62, 228",{},{"id":26,"text":2615,"url":26,"identifiers":2616},"10.1130\u002FGSAB-39-465",{"doi":2615},{"id":26,"text":2618,"url":26,"identifiers":2619},"10.1086\u002F623802",{"doi":2618},{"id":26,"text":2621,"url":26,"identifiers":2622},"10.1306\u002FD42694A4-2B26-11D7-8648000102C1865D",{"doi":2621},{"id":26,"text":2624,"url":26,"identifiers":2625},"10.1130\u002F0016-7606(1954)65[175:GOAFIS]2.0.CO;2",{"doi":2624},{"id":26,"text":2627,"url":26,"identifiers":2628},"BLOCK B. J., 1964, Sedimentation of an alluvial fan in southern Nevada, J. Sediment. Petrol., 34, 395",{},{"id":26,"text":2630,"url":26,"identifiers":2631},"10.1111\u002Fj.1365-3091.1963.tb01199.x",{"doi":2630},{"id":26,"text":2633,"url":26,"identifiers":2634},"10.1029\u002FJZ066i010p03337",{"doi":2633},{"id":26,"text":2636,"url":26,"identifiers":2637},"N BOTVINKINA. L., 1954, Alluvial Deposits in the Coal Measures in the Middle Carboniferous of the Donets Basin, 30",{},{"id":26,"text":2639,"url":26,"identifiers":2640},"BRICE J. C., 1964, Channel patterns and terraces of the Loup Rivers in Nebraska, U.S., Geol. Surv., Profess. Papers, 422, 41",{},{"id":26,"text":2642,"url":26,"identifiers":2643},"BRINKMANN R., 1933, Über Kreutzschichtung im Deutschen Buntsandstein, Nachr. Akad. Wiss. Göttingen, Math. Physik. Kl., 1",{},{"id":26,"text":2645,"url":26,"identifiers":2646},"BROOKS N. H., 1955, Mechanics of streams with moveable beds of fine sand, Proc. Am. Soc. Civil Engrs., 81, 1",{},{"id":26,"text":2648,"url":26,"identifiers":2649},"BRUSH L. M., 1961, Drainage basins, channels, and flow characteristics of selected streams in central Pennsylvania, U.S., Geol. Surv., Profess. Papers, 282, 145",{},{"id":26,"text":2651,"url":26,"identifiers":2652},"BRUSH L. M., 1964, Sediment sorting in alluvial channels, Bull. Am. Assoc. Petrol. Geologists, 48, 519",{},{"id":26,"text":2654,"url":26,"identifiers":2655},"10.2475\u002Fajs.s4-47.279.149",{"doi":2654},{"id":26,"text":2657,"url":26,"identifiers":2658},"BULL W. B., 1960, Types of deposition on alluvial fans in western Fresno County, California, Bull. Geol. Soc. Am., 71, 2052",{},{"id":26,"text":2660,"url":26,"identifiers":2661},"BULL W. B., 1962, Relation of textural (CM) patterns to depositional environment of alluvial fan deposits, J. Sediment. Petrol., 32, 211",{},{"id":26,"text":2663,"url":26,"identifiers":2664},"10.2475\u002Fajs.262.2.249",{"doi":2663},{"id":26,"text":2666,"url":26,"identifiers":2667},"BULL W. B., 1964, Geomorphology of segmented alluvial fans in western Fresno County, California, U. S., Geol. Surv., Profess. Papers, 352, 89",{},{"id":26,"text":2669,"url":26,"identifiers":2670},"BULL W. B., 1964, Alluvial fans and near‐surface subsidence in western Fresno County, California, U.S., Geol. Surv., Profess. Papers, 437, 71",{},{"id":26,"text":2672,"url":26,"identifiers":2673},"BURRI C., 1929, Sedimentpetrographische Untersuchungen an Alpinen Flüsssanden, Schweiz. Mineral. Petrog. Mitt., 9, 205",{},{"id":26,"text":2675,"url":26,"identifiers":2676},"BURTNER R. L., 1963, Symposium on Middle and Upper Devonian stratigraphy of Pennsylvania and adjacent states, 7",{},{"id":26,"text":2678,"url":26,"identifiers":2679},"BUTLER B. E., 1958, Depositional Systems of the Riverine Plain of Southeastern Australia in Relation to Soils, 35",{},{"id":26,"text":2681,"url":26,"identifiers":2682},"BUWALDA J. F., 1951, Transportation of coarse material of alluvial fans, Bull. Geol. Soc. Am., 62, 1497",{},{"id":26,"text":2684,"url":26,"identifiers":2685},"10.2307\u002F211190",{"doi":2684},{"id":26,"text":2687,"url":26,"identifiers":2688},"CAREY W. C., 1957, Systematic changes in the beds of alluvial rivers. Proc. Am. Soc. Civil Engrs, J. Hydraulics Div., 83, 1",{},{"id":26,"text":2690,"url":26,"identifiers":2691},"10.2307\u002F3625878",{"doi":2690},{"id":26,"text":2693,"url":26,"identifiers":2694},"CARLSTON W. B., 1963, Drainage density and streamflow, U.S., Geol. Surv., Profess. Papers, 422, 8",{},{"id":26,"text":2696,"url":26,"identifiers":2697},"10.1017\u002FS0016756800077578",{"doi":2696},{"id":26,"text":2699,"url":26,"identifiers":2700},"10.2307\u002F209600",{"doi":2699},{"id":26,"text":2702,"url":26,"identifiers":2703},"CHIEN N., 1961, The braided stream of the lower Yellow River, Sci. Sinica (Peking), 10, 734",{},{"id":26,"text":2705,"url":26,"identifiers":2706},"10.1017\u002FS0016756800068412",{"doi":2705},{"id":26,"text":2708,"url":26,"identifiers":2709},"10.1086\u002F626608",{"doi":2708},{"id":26,"text":2711,"url":26,"identifiers":2712},"10.2475\u002Fajs.255.2.138",{"doi":2711},{"id":26,"text":2714,"url":26,"identifiers":2715},"CHOW V. T., 1959, Open‐channel Hydraulics, 680",{},{"id":26,"text":2717,"url":26,"identifiers":2718},"COLBY B. R., 1960, Discontinuous rating curves for Pigeon Roost and Cuffawa Creeks in northern Mississippi, U.S. Dept. Agr., A. R. S., 41, 31",{},{"id":26,"text":2720,"url":26,"identifiers":2721},"COLBY B. R., 1963, Fluvial sediments—a summary of source, transportation, deposition and measurement of sediment discharge, U.S., Geol. Surv., Bull., 1181, 1",{},{"id":26,"text":2723,"url":26,"identifiers":2724},"COLBY B. R., 1964, Discharge of sands and mean‐velocity relationships in sand‐bed streams, U.S., Geol. Surv., Profess. Papers, 462, 47",{},{"id":26,"text":2726,"url":26,"identifiers":2727},"COLBY B. R., 1964, Scour and fill in sand‐bed streams, U.S., Geol. Surv., Profess. Papers, 462, 32",{},{"id":26,"text":2729,"url":26,"identifiers":2730},"10.1016\u002F0025-3227(64)90062-3",{"doi":2729},{"id":26,"text":2732,"url":26,"identifiers":2733},"10.2475\u002Fajs.s5-34.202.293",{"doi":2732},{"id":26,"text":2735,"url":26,"identifiers":2736},"10.1029\u002FTR016i002p00478",{"doi":2735},{"id":26,"text":2738,"url":26,"identifiers":2739},"CRAIG L. C., 1955, Stratigraphy of Morrison and related formations, Colorado Plateau region: a preliminary report, U.S., Geol. Surv., Bull., 1009, 125",{},{"id":26,"text":2741,"url":26,"identifiers":2742},"10.1086\u002F626672",{"doi":2741},{"id":26,"text":2744,"url":26,"identifiers":2745},"10.1029\u002FJZ067i004p01511",{"doi":2744},{"id":26,"text":2747,"url":26,"identifiers":2748},"CROUZEL F., 1957, Le Miocène continentale du Bassin d'Aquitaine, Bull. Serv. Carte Géol. France, 248, 264",{},{"id":26,"text":2750,"url":26,"identifiers":2751},"CULBERTSON J. K., 1964, A study of fluvial characteristics and hydraulic variables, Middle Rio Grande, New Mexico, U.S., Geol. Surv., Water Supply Papers, 1498, 74",{},{"id":26,"text":2753,"url":26,"identifiers":2754},"DAVIS W. M., 1889, The rivers and valleys of Pennsylvania, Natl. Geograph. Mag., 1, 183",{},{"id":26,"text":2756,"url":26,"identifiers":2757},"DAVIS W. M., 1890, The rivers of north New Jersey with notes on the classification of rivers in general, Natl. Geograph. Mag., 2, 81",{},{"id":26,"text":2759,"url":26,"identifiers":2760},"10.1130\u002FGSAB-49-1337",{"doi":2759},{"id":26,"text":2762,"url":26,"identifiers":2763},"DAWDY D. R., 1961, Depth‐discharge relations of alluvial streams—discontinuous rating curves, U.S., Geol. Surv., Water Supply Papers, 1498, 16",{},{"id":26,"text":2765,"url":26,"identifiers":2766},"DENNY C. S., 1965, Alluvial fans in the Death Valley region, California, Nevada, U.S., Geol. Surv., Profess. Papers, 466, 62",{},{"id":26,"text":2768,"url":26,"identifiers":2769},"DERRUAU M., 1958, Precis de Géomorphologie, 395",{},{"id":26,"text":2771,"url":26,"identifiers":2772},"10.1111\u002Fj.1365-3091.1962.tb00453.x",{"doi":2771},{"id":26,"text":2774,"url":26,"identifiers":2775},"10.1111\u002Fj.1365-3091.1962.tb01144.x",{"doi":2774},{"id":26,"text":2777,"url":26,"identifiers":2778},"10.1144\u002FGSL.JGS.1873.029.01-02.39",{"doi":2777},{"id":26,"text":2780,"url":26,"identifiers":2781},"DREWES H., 1963, Geology of the Funeral Peak Quadrangle, California, on the east flank of Death Valley, U.S., Geol. Surv., Profess. Papers, 413, 1",{},{"id":26,"text":2783,"url":26,"identifiers":2784},"DRURY W. H., 1956, Bog Flats and Physiographic Processes in the Upper Kuskokwim River Region, Alaska, 130",{},{"id":26,"text":2786,"url":26,"identifiers":2787},"10.1029\u002FTR016i002p00467",{"doi":2786},{"id":26,"text":2789,"url":26,"identifiers":2790},"10.1130\u002FGSAB-49-343",{"doi":2789},{"id":26,"text":2792,"url":26,"identifiers":2793},"10.1086\u002F623509",{"doi":2792},{"id":26,"text":2795,"url":26,"identifiers":2796},"EINSTEIN H. A., 1952, River channel roughness, Trans. Am. Soc. Civil Engrs., 117, 1121, 10.1061\u002FTACEAT.0006666",{"doi":2797},"10.1061\u002FTACEAT.0006666",{"id":26,"text":2799,"url":26,"identifiers":2800},"FAHNESTOCK R. K., 1963, Morphology and hydrology of a glacial stream, White River, mount Rainier, Washington, U.S., Geol. Surv., Profess. Papers, 422, 70",{},{"id":26,"text":2802,"url":26,"identifiers":2803},"10.1130\u002F0016-7606(1962)73[1431:FSOTTO]2.0.CO;2",{"doi":2802},{"id":26,"text":2805,"url":26,"identifiers":2806},"FAHNESTOCK R. K., 1964, Preliminary report on bed forms and flow phenomena in the Rio Grande near El Paso, Texas, U.S., Geol. Surv., Profess. Papers, 501, 191",{},{"id":26,"text":2808,"url":26,"identifiers":2809},"FAHRIG W. F., 1961, The geology of the Athabasca Formation, Can., Dept. Mines Tech. Surv., Geol. Surv. Can., Geol. Surv. Bull., 68, 41",{},{"id":26,"text":2811,"url":26,"identifiers":2812},"FENNEMAN N. M., 1906, Floodplains produced without floods, Am. Geograph. Soc., Bull., 38, 89",{},{"id":26,"text":2814,"url":26,"identifiers":2815},"FISK H. N., 1944, Geological Investigation of the Alluvial Valley of the Lower Mississippi River, 78",{},{"id":26,"text":2817,"url":26,"identifiers":2818},"FISK H. N., 1947, Fine Grained Alluvial Deposits and their Effects on Mississippi River Activity, 82",{},{"id":26,"text":2820,"url":26,"identifiers":2821},"FISK H. N., 1952, Mississippi River Valley geology relation to river regime, Trans. Am. Soc. Civil Engrs., 117, 667, 10.1061\u002FTACEAT.0006733",{"doi":2822},"10.1061\u002FTACEAT.0006733",{"id":26,"text":2824,"url":26,"identifiers":2825},"FISK H. N., 1960, Recent Mississippi river sedimentation and peat accumulation. Congr. Avan. Études Stratigraph, 4",{},{"id":26,"text":2827,"url":26,"identifiers":2828},"FISK H. N., 1961, Geometry of Sandstone Bodies, 29",{},{"id":26,"text":2830,"url":26,"identifiers":2831},"10.1306\u002FD4269661-2B26-11D7-8648000102C1865D",{"doi":2830},{"id":26,"text":2833,"url":26,"identifiers":2834},"10.1306\u002F74D70646-2B21-11D7-8648000102C1865D",{"doi":2833},{"id":26,"text":2836,"url":26,"identifiers":2837},"FORCHE F., 1935, Stratigraphie und Paläogeographie des Buntsandsteins im Umkreis der Vosgen, Mitt. Geol. Staatsinst. Hamburg, 15, 15",{},{"id":26,"text":2839,"url":26,"identifiers":2840},"FRAZIER D. E., 1961, Point‐bar deposits, Old River Locksite, Louisiana, Trans. Gulf Coast Assoc. Geol. Soc., 11, 121",{},{"id":26,"text":2842,"url":26,"identifiers":2843},"FRIEDKIN J. F., 1945, A Laboratory Study of the Meandering of Alluvial Rivers, 40",{},{"id":26,"text":2845,"url":26,"identifiers":2846},"FRIEDMANN S. A., 1960, Channel‐fill sandstones in the Middle Pennsylvanian rocks of Indiana, Indiana, Dept. Conserv., Geol. Surv., Rept. Progr., 23, 59",{},{"id":26,"text":2848,"url":26,"identifiers":2849},"10.1144\u002Fpygs.33.1.77",{"doi":2848},{"id":26,"text":2851,"url":26,"identifiers":2852},"GILBERT G. K., 1914, The transportation of debris by running water, U.S., Geol. Surv., Profess. Papers, 86, 263",{},{"id":26,"text":2854,"url":26,"identifiers":2855},"10.1097\u002F00010694-196502000-00002",{"doi":2854},{"id":26,"text":2857,"url":26,"identifiers":2858},"GLENN J. L., 1959, Characteristics and distribution of some Missouri River deposits, Proc. Iowa Acad. Sci., 66, 302",{},{"id":26,"text":2860,"url":26,"identifiers":2861},"GRABAU A., 1960, Principles of Stratigraphy, 1185",{},{"id":26,"text":2863,"url":26,"identifiers":2864},"GUY H. P., 1964, An analysis of some storm‐period variables affecting stream sediment transport, U.S., Geol. Surv., Profess. Papers, 462, 46",{},{"id":26,"text":2866,"url":26,"identifiers":2867},"10.1306\u002F74D71113-2B21-11D7-8648000102C1865D",{"doi":2866},{"id":26,"text":2869,"url":26,"identifiers":2870},"HACK J. T., 1957, Studies of longitudinal stream profiles in Virginia and Maryland, U.S., Geol. Surv., Profess. Papers, 294, 45",{},{"id":26,"text":2872,"url":26,"identifiers":2873},"HAMBLIN W. K., 1958, Cambrian sandstones of northern Michigan, Mich. Dept. Conserv., Geol. Surv. Div., Publ., 51, 146",{},{"id":26,"text":2875,"url":26,"identifiers":2876},"HAMBLIN W. K., 1961, Micro‐cross‐lamination in Upper Keeweenawan sediments of northern Michigan, J. Sediment. Petrol., 31, 390",{},{"id":26,"text":2878,"url":26,"identifiers":2879},"10.1130\u002F0016-7606(1961)72[1:PEOTLS]2.0.CO;2",{"doi":2878},{"id":26,"text":2881,"url":26,"identifiers":2882},"HAPP S. C, 1940, Significance of texture and density of alluvial deposits in the middle Rio Grande valley, J. Sediment. Petrol., 14, 3",{},{"id":26,"text":2884,"url":26,"identifiers":2885},"10.1130\u002F0016-7606(1948)59[1191:SITMRG]2.0.CO;2",{"doi":2884},{"id":26,"text":2887,"url":26,"identifiers":2888},"HAPP S. C., 1940, Some aspects of accelerated stream and valley sedimentation, U.S. Dept. Agr., Tech. Bull., 695, 134",{},{"id":26,"text":2890,"url":26,"identifiers":2891},"HARMS J. C., 1964, Stratification, bed forms, and flow phenomena, Bull. Am. Assoc. Petrol. Geologists, 48, 530",{},{"id":26,"text":2893,"url":26,"identifiers":2894},"10.1086\u002F626933",{"doi":2893},{"id":26,"text":2896,"url":26,"identifiers":2897},"HARSHBARGER J. W., 1957, Stratigraphy of the uppermost Triassic and the Jurassic rocks of the Navajo country, U.S., Geol. Surv., Profess. Papers, 291, 74",{},{"id":26,"text":2899,"url":26,"identifiers":2900},"HAWKINS C. A., 1956, Study of layered sedimentary materials in the Riverine Plain, N.S.W, J. Roy. Soc. New South Wales, 90, 110, 10.5962\u002Fp.360715",{"doi":2901},"10.5962\u002Fp.360715",{"id":26,"text":2903,"url":26,"identifiers":2904},"HJULSTRÖM F., 1935, Studies of the morphological activity of rivers as illustrated by the river Fyris, Bull. Geol. Inst. Univ. Uppsala, 25, 221",{},{"id":26,"text":2906,"url":26,"identifiers":2907},"HJULSTRÖM F, 1952, The geomorphology of the alluvial outwash plains (Sandurs) of Iceland and the mechanics of braided rivers, 337",{},{"id":26,"text":2909,"url":26,"identifiers":2910},"HJULSTRÖM F., 1953, På expedition till isländska sandurfält 1951 och 1952, Ymer, 73, 161",{},{"id":26,"text":2912,"url":26,"identifiers":2913},"HOPKINS M. E., 1958, Geology and petrology of the Anvil Rock sandstone of southern Illinois, Illinois State Geol. Surv., Circ., 256, 48",{},{"id":26,"text":2915,"url":26,"identifiers":2916},"10.2307\u002F520384",{"doi":2915},{"id":26,"text":2918,"url":26,"identifiers":2919},"HORTON R. E., 1941, Sheet erosion—past and present, Trans. Am. Geophys. Union, 22, 299",{},{"id":26,"text":2921,"url":26,"identifiers":2922},"10.1130\u002F0016-7606(1945)56[275:EDOSAT]2.0.CO;2",{"doi":2921},{"id":26,"text":2924,"url":26,"identifiers":2925},"HOWARD C. S., 1947, Suspended sediment in the Colorado River, U.S., Geol. Surv., Water Supply Papers, 998, 165",{},{"id":26,"text":2927,"url":26,"identifiers":2928},"HUBBELL D. W., 1959, Investigations of sediment transportation, Middle Loup River at Dunning, Nebraska, U.S., Geol. Surv., Water Supply Papers, 1476, 123",{},{"id":26,"text":2930,"url":26,"identifiers":2931},"INMAN D. L., 1949, Sorting of sediment in the light of fluid mechanics, J. Sediment. Petrol., 19, 51",{},{"id":26,"text":2933,"url":26,"identifiers":2934},"10.2475\u002Fajs.s5-32.191.349",{"doi":2933},{"id":26,"text":2936,"url":26,"identifiers":2937},"JABLOKOV V. S., 1961, Sedimentation in the Carboniferous and the significance of alluvial deposits, 4",{},{"id":26,"text":2939,"url":26,"identifiers":2940},"JAHNS R. H., 1947, Geologic features of the Connecticut Valley, Massachusetts, as related to recent floods, U.S., Geol. Surv., Water Supply Papers, 996, 158",{},{"id":26,"text":2942,"url":26,"identifiers":2943},"JAHNS R. H. 1949.Desert floods. Eng. Sci. Monthly 1949:10–15.",{},{"id":26,"text":2945,"url":26,"identifiers":2946},"10.2307\u002F520386",{"doi":2945},{"id":26,"text":2948,"url":26,"identifiers":2949},"JOPLING A. V., 1962, Origin of regressive ripples explained in terms of fluid mechanics processes, U.S., Geol. Surv., Profess. Papers, 429, 408",{},{"id":26,"text":2951,"url":26,"identifiers":2952},"10.1029\u002FJZ069i016p03403",{"doi":2951},{"id":26,"text":2954,"url":26,"identifiers":2955},"10.1126\u002Fscience.136.3519.839",{"doi":2954},{"id":26,"text":2957,"url":26,"identifiers":2958},"KALINSKE A. A., 1940, Experimental studies of liquid turbulence, Iowa, Univ., Studies Eng., Bull., 20, 31",{},{"id":26,"text":2960,"url":26,"identifiers":2961},"KALINSKE A. A., 1943, The role of turbulence in river hydraulics, Iowa, Univ., Studies Eng., Bull., 27, 266",{},{"id":26,"text":2963,"url":26,"identifiers":2964},"KARTASHOV I. P., 1961, Facies, dynamic phases and formation of alluvium, Izv. Akad. Nauk S.S.S.R., Ser. Geol., 9, 77",{},{"id":26,"text":2966,"url":26,"identifiers":2967},"KELLER W. D., 1949, Missouri River sediments in river water, ocean water, and sodium oxalate solution, J. Sediment. Petrol., 19, 78",{},{"id":26,"text":2969,"url":26,"identifiers":2970},"KENNEDY J. F., 1961, Stationary waves and antidunes in alluvial channels, 146",{},{"id":26,"text":2972,"url":26,"identifiers":2973},"10.1017\u002FS0022112063000975",{"doi":2972},{"id":26,"text":2975,"url":26,"identifiers":2976},"10.1029\u002FJZ069i008p01517",{"doi":2975},{"id":26,"text":2978,"url":26,"identifiers":2979},"KILPATRICK F. A., 1964, Channel geometry of piedmont streams as related to frequency of floods, U.S., Geol. Surv., Profess. Papers, 422, 10",{},{"id":26,"text":2981,"url":26,"identifiers":2982},"KINDLE E. M., 1917, Recent and fossil ripple mark, Geol. Surv. Can., Museum Bull., 25, 121",{},{"id":26,"text":2984,"url":26,"identifiers":2985},"10.1130\u002F0016-7606(1962)73[1127:TSMPC]2.0.CO;2",{"doi":2984},{"id":26,"text":2987,"url":26,"identifiers":2988},"10.1086\u002F626957",{"doi":2987},{"id":26,"text":2990,"url":26,"identifiers":2991},"KOLB C. R., 1962, Distribution of soils bordering the Mississippi River from Donaldsonville to Head of Passes, 61",{},{"id":26,"text":2993,"url":26,"identifiers":2994},"10.1111\u002Fj.1365-3091.1963.tb01216.x",{"doi":2993},{"id":26,"text":2996,"url":26,"identifiers":2997},"10.2307\u002F520318",{"doi":2996},{"id":26,"text":2999,"url":26,"identifiers":3000},"KRUIT C., 1955, Sediments of the Rhone delta. Grainsize and microfauna, Verhandel. Koninkl. Ned. Geol. Mijnbouwk. Genoot., Geol. Ser., 15, 357",{},{"id":26,"text":3002,"url":26,"identifiers":3003},"10.1130\u002FGSAB-53-1355",{"doi":3002},{"id":26,"text":3005,"url":26,"identifiers":3006},"KRYNINE P. D., 1950, Petrology, stratigraphy and origin of Triassic sedimentary rocks of Connecticut, Conn., State Geol. Nat. Hist. Surv. Bull., 73, 247",{},{"id":26,"text":3008,"url":26,"identifiers":3009},"KURDYUKOV K. V., 1957, Fundamental problems in the study of subaerial deltas, Akad. Nauk S.S.S.R., 21, 5",{},{"id":26,"text":3011,"url":26,"identifiers":3012},"LAMAKIN V. V., 1947, On the dynamics of some particular alluvial deposits, Dokl. Akad. Nauk S.S.S.R., 57, 65",{},{"id":26,"text":3014,"url":26,"identifiers":3015},"LANE D. W., 1963, Cross‐stratification in San Bernard River, Texas, point bar deposits, J. Sediment. Petrol., 33, 350",{},{"id":26,"text":3017,"url":26,"identifiers":3018},"LANE D. W., 1963, Sedimentary environments in Cretaceous Dakota Sandstone in northwestern Colorado, Bull. Am. Assoc. Petrol. Geologists, 47, 229",{},{"id":26,"text":3020,"url":26,"identifiers":3021},"LANE E. W., 1957, A study of the shape of channels formed by natural streams flowing in erodible material, U.S. Corps Engr., Missouri River Div., Omaha, Neb., Sediment Ser., 9, 106",{},{"id":26,"text":3023,"url":26,"identifiers":3024},"LANE E. W., 1954, River bed scour during floods, Trans. Am. Soc. Civil Engrs., 119, 1069, 10.1061\u002FTACEAT.0007046",{"doi":3025},"10.1061\u002FTACEAT.0007046",{"id":26,"text":3027,"url":26,"identifiers":3028},"LANE E. W., 1940, Sand waves in the lower Mississippi River, J. Western Soc. Engrs., 45, 281",{},{"id":26,"text":3030,"url":26,"identifiers":3031},"10.2475\u002Fajs.262.6.782",{"doi":3030},{"id":26,"text":3033,"url":26,"identifiers":3034},"10.2307\u002F212281",{"doi":3033},{"id":26,"text":3036,"url":26,"identifiers":3037},"10.1306\u002F74D70A1A-2B21-11D7-8648000102C1865D",{"doi":3036},{"id":26,"text":3039,"url":26,"identifiers":3040},"LAWSON A. C., 1913, The petrographic description of alluvial fan deposits, Univ. Calif. (Berkeley), Publ. Geol. Sci., 7, 325",{},{"id":26,"text":3042,"url":26,"identifiers":3043},"LEBLANC R. J., 1959, Origin and development of the Texas shoreline, 57",{},{"id":26,"text":3045,"url":26,"identifiers":3046},"LEEPER W. S., 1963, Symposium on Middle and Upper Devonian Stratigraphy of Pennsylvania and Adjacent States, 165",{},{"id":26,"text":3048,"url":26,"identifiers":3049},"10.2307\u002F208917",{"doi":3048},{"id":26,"text":3051,"url":26,"identifiers":3052},"LELIAVSKY S., 1955, An Introduction to Fluvial Hydraulics, 257",{},{"id":26,"text":3054,"url":26,"identifiers":3055},"ENGELHARDT LEMCKE K., 1953, Geologische und sedimentpetro‐graphische Untersuchungen im Westteil der ungefalteten Molasse des süddeutschen Alpen‐vorlandes, Geol. Jahrb., Beih., 11, 110",{},{"id":26,"text":3057,"url":26,"identifiers":3058},"LEOPOLD L. B., 1962, Rivers, Am. Scientist, 50, 511",{},{"id":26,"text":3060,"url":26,"identifiers":3061},"LEOPOLD L. B., 1962, The concept of entropy in landscape evolution, U.S., Geol. Surv., Profess. Papers, 500, 20",{},{"id":26,"text":3063,"url":26,"identifiers":3064},"LEOPOLD L. B., 1953, The hydraulic geometry of stream channels and some physiographic implications, U.S., Geol. Surv., Profess. Papers, 252, 1",{},{"id":26,"text":3066,"url":26,"identifiers":3067},"LEOPOLD L. B., 1956, Ephemeral streams—hydraulic factors and their relationship to the drainage net, U.S., Geol. Surv., Profess. Papers, 282, 1",{},{"id":26,"text":3069,"url":26,"identifiers":3070},"LEOPOLD L. B., 1956, Floods in relation to river channels, Intern. Assoc. Hydrol. Publ. 42, Symp. Darcy (Dijon, 1956), 3, 85",{},{"id":26,"text":3072,"url":26,"identifiers":3073},"LEOPOLD L. B., 1957, River channel patterns; braided, meandering and straight, U.S., Geol. Surv., Profess. Papers, 282, 39",{},{"id":26,"text":3075,"url":26,"identifiers":3076},"10.1130\u002F0016-7606(1960)71[769:RM]2.0.CO;2",{"doi":3075},{"id":26,"text":3078,"url":26,"identifiers":3079},"LEOPOLD L. B., 1960, Flow resistance in sinuous or irregular channels, U.S., Geol. Surv., Profess. Papers, 282, 111",{},{"id":26,"text":3081,"url":26,"identifiers":3082},"LEOPOLD L. B., 1964, Fluvial Processes in Geomorphology, 522",{},{"id":26,"text":3084,"url":26,"identifiers":3085},"LEVI I. I., 1957, Dynamics of Channel Currents, 252",{},{"id":26,"text":3087,"url":26,"identifiers":3088},"10.2475\u002Fajs.s5-20.115.1",{"doi":3087},{"id":26,"text":3090,"url":26,"identifiers":3091},"LOPATIN G. V., 1952, Alluvium of Russian rivers (transport and formation), Vses. Geogr. Obshch., Zap., 14, 366",{},{"id":26,"text":3093,"url":26,"identifiers":3094},"LORENS P. J., 1955, Seepage Conditions in Sacramento Valley, A1",{},{"id":26,"text":3096,"url":26,"identifiers":3097},"10.2475\u002Fajs.262.3.325",{"doi":3096},{"id":26,"text":3099,"url":26,"identifiers":3100},"LUGN A. L., 1927, An observed origin of some mud pebbles, Proc. Iowa Acad. Sci., 34, 249",{},{"id":26,"text":3102,"url":26,"identifiers":3103},"LUSTIG L. K., 1963, Competence of transport on alluvial fans, 126",{},{"id":26,"text":3105,"url":26,"identifiers":3106},"MACKENZIE F. T., 1962, Cloverly‐Lakota and Fall River paleocurrents in the Wyoming Rockies, 44",{},{"id":26,"text":3108,"url":26,"identifiers":3109},"10.1130\u002FGSAB-48-813",{"doi":3108},{"id":26,"text":3111,"url":26,"identifiers":3112},"MANSFIELD G. R., 1938, Flood deposits of the Ohio River, January‐February, 1937—a study of sedimentation, U.S., Geol. Surv., Water Supply Papers, 838, 693",{},{"id":26,"text":3114,"url":26,"identifiers":3115},"MAPEL W. J., 1962, Stream directions in the Lakota formation (Cretaceous) in the north Black Hills, Wyoming and South Dakota, U.S., Geol. Surv., Profess. Papers, 450, 35",{},{"id":26,"text":3117,"url":26,"identifiers":3118},"10.1029\u002FTR028i002p00255",{"doi":3117},{"id":26,"text":3120,"url":26,"identifiers":3121},"10.1086\u002F624364",{"doi":3120},{"id":26,"text":3123,"url":26,"identifiers":3124},"10.1306\u002F74D71163-2B21-11D7-8648000102C1865D",{"doi":3123},{"id":26,"text":3126,"url":26,"identifiers":3127},"MCDOWELL J. P., 1957, The sedimentary petrology of the Mississagi Quartzite in the Blind River area, Ontario Dept. Mines, Geol. Circ., 6, 31",{},{"id":26,"text":3129,"url":26,"identifiers":3130},"MCDOWELL J. P., 1960, Cross‐bedding formed by sand waves in Mississippi River point bar deposits, Bull. Geol. Soc. Am, Bull. Geol. Soc. Am",{},{"id":26,"text":3132,"url":26,"identifiers":3133},"10.1130\u002FGSAB-8-87",{"doi":3132},{"id":26,"text":3135,"url":26,"identifiers":3136},"10.1086\u002F624737",{"doi":3135},{"id":26,"text":3138,"url":26,"identifiers":3139},"MCKEE E. D., 1954, Stratigraphy and history of the Moenkopi formation of Triassic age, Geol. Soc. Am., Mem, Geol. Soc. Am., Mem, 133",{},{"id":26,"text":3141,"url":26,"identifiers":3142},"MCKEE E. D., 1957, Primary structures of some recent sediments, Bull. Am. Assoc. Petrol. Geologists, 41, 1704",{},{"id":26,"text":3144,"url":26,"identifiers":3145},"10.2307\u002F209717",{"doi":3144},{"id":26,"text":3147,"url":26,"identifiers":3148},"10.1086\u002F627044",{"doi":3147},{"id":26,"text":3150,"url":26,"identifiers":3151},"10.2110\u002Fjsr.20.148",{"doi":3150},{"id":26,"text":3153,"url":26,"identifiers":3154},"MIKHAILOVA N. A., 1952, On the mechanics of formation and movement of dunes, Izv. Akad. Nauk S.S.S.R., Ser. Geofiz., 1, 47",{},{"id":26,"text":3156,"url":26,"identifiers":3157},"MIKHAILOVA N. A., 1953, On the flow structure in the presence of dunes, Izv. Akad. Nauk S.S.S.R., Ser. Geofiz., 5, 445",{},{"id":26,"text":3159,"url":26,"identifiers":3160},"MILLER V. C., 1961, Photogeology, 248",{},{"id":26,"text":3162,"url":26,"identifiers":3163},"10.1130\u002F0016-7606(1960)71[1137:MCASMF]2.0.CO;2",{"doi":3162},{"id":26,"text":3165,"url":26,"identifiers":3166},"MOORE R. C., 1958, Introduction to Historical Geology, 656",{},{"id":26,"text":3168,"url":26,"identifiers":3169},"10.2475\u002Fajs.262.3.340",{"doi":3168},{"id":26,"text":3171,"url":26,"identifiers":3172},"MUDGE M. R., 1956, Sandstones and channels in Upper Pennsylvanian and Lower Permian in Kansas, Bull. Am. Assoc. Petrol. Geologists, 40, 654",{},{"id":26,"text":3174,"url":26,"identifiers":3175},"MUNDORF J. C., 1964, Fluvial sediment in Kiowa Creek Basin, Colorado, 70",{},{"id":26,"text":3177,"url":26,"identifiers":3178},"MURRAY G. E., 1961, Geology of the Atlantic and Gulf Coastal Plains of North America, 692",{},{"id":26,"text":3180,"url":26,"identifiers":3181},"NEDECO, 1959, River Studies and Recommendations on Improvement of Niger and Benue, 1000",{},{"id":26,"text":3183,"url":26,"identifiers":3184},"NORDIN C. F., 1963, A preliminary study of sediment transport parameters, Rio Puerco near Bernado, New Mexico, 20",{},{"id":26,"text":3186,"url":26,"identifiers":3187},"NORDIN C. F., 1964, Aspects of flow resistance and sediment transport, Rio Grande near Bernalillo, New Mexico, 41",{},{"id":26,"text":3189,"url":26,"identifiers":3190},"NORDIN C. F., 1964, Temporary storage of fine sediment in islands and point bars of alluvial channels of the Rio Grande, New Mexico and Texas, 138",{},{"id":26,"text":3192,"url":26,"identifiers":3193},"NORDIN C. F., 1963, Vertical distribution of velocity and suspended sediment, Middle Rio Grande, New Mexico, 20",{},{"id":26,"text":3195,"url":26,"identifiers":3196},"10.1306\u002FD42692A6-2B26-11D7-8648000102C1865D",{"doi":3195},{"id":26,"text":3198,"url":26,"identifiers":3199},"10.1130\u002F0016-7606(1958)69[1033:PPIPAM]2.0.CO;2",{"doi":3198},{"id":26,"text":3201,"url":26,"identifiers":3202},"PEMBERTON E. L., 1964, Sediment investigations—middle Rio Grande, Proc. Am. Assoc. Civil Engrs., J. Hydraulics Div., 90, 163",{},{"id":26,"text":3204,"url":26,"identifiers":3205},"PEPPER J. F., 1954, Geology of the Bedford Shale and Berea Sandstone in the Appalachian Basin, 111",{},{"id":26,"text":3207,"url":26,"identifiers":3208},"PICARD K., 1950, Sedimentations‐Verhältnisse des Hauptbuntsandsteins in der Bucht von Mechernich‐Nideggen, Geol. Jahrb., 64, 331",{},{"id":26,"text":3210,"url":26,"identifiers":3211},"10.1007\u002FBF01803506",{"doi":3210},{"id":26,"text":3213,"url":26,"identifiers":3214},"10.1086\u002F625559",{"doi":3213},{"id":26,"text":3216,"url":26,"identifiers":3217},"POOLE F. G., 1961, Stream directions in the Triassic rocks of the Colorado Plateau, U.S., Geol. Surv., Profess. Papers, 424, 139",{},{"id":26,"text":3219,"url":26,"identifiers":3220},"10.1086\u002F626223",{"doi":3219},{"id":26,"text":3222,"url":26,"identifiers":3223},"POTTER P. E., 1962, Late Mississippian sandstones of Illinois, Illinois State Geol. Surv., Circ, 340, 36",{},{"id":26,"text":3225,"url":26,"identifiers":3226},"POTTER P. E., 1962, Shape and distribution of Pennsylvanian sand bodies in Illinois, Illinois State Geol. Surv., Circ, 339, 35",{},{"id":26,"text":3228,"url":26,"identifiers":3229},"POTTER P. E., 1962, Regional distribution patterns of Pennsylvanian sandstones in Illinois Basin, Bull. Am. Assoc. Petrol. Geologists, 46, 1890",{},{"id":26,"text":3231,"url":26,"identifiers":3232},"POTTER P. E., 1963, Late Palaeozoic sandstone of the Illinois Basin, Illinois State Geol. Surv., Rept. Invest, 217, 92",{},{"id":26,"text":3234,"url":26,"identifiers":3235},"POTTER P. E., 1958, Petrology and sedimentation of the Pennsylvanian sediments in southern Illinois: a vertical profile, Illinois State Geol. Surv., Rept. Invest, 204, 60",{},{"id":26,"text":3237,"url":26,"identifiers":3238},"10.1086\u002F626133",{"doi":3237},{"id":26,"text":3240,"url":26,"identifiers":3241},"10.1007\u002F978-3-662-01020-4",{"doi":3240},{"id":26,"text":3243,"url":26,"identifiers":3244},"10.1086\u002F626346",{"doi":3243},{"id":26,"text":3246,"url":26,"identifiers":3247},"POTTER P. E., 1961, Anvil Rock sandstone and channel cutouts of Herrin (no. 6) coal in west‐central Illinois, Illinois State Geol. Surv., Circ, 314, 12",{},{"id":26,"text":3249,"url":26,"identifiers":3250},"POTTER P. E., 1958, Chester cross‐bedding and sandstone trends in Illinois Basin, Bull. Am. Assoc. Petrol. Geologists, 42, 1013",{},{"id":26,"text":3252,"url":26,"identifiers":3253},"PRANDTL L., 1957, Fundamental of Hydro‐ and Aeromechanics, 270",{},{"id":26,"text":3255,"url":26,"identifiers":3256},"PRANDTL L., 1957, Applied Hydro‐ and Aeromechanics, 311",{},{"id":26,"text":3258,"url":26,"identifiers":3259},"PRETIOUS E. S., 1951, Final Report on Special Observations of Bed Movement in Lower Fraser River at Ladner Reach during 1950 Freshet, 12",{},{"id":26,"text":3261,"url":26,"identifiers":3262},"QURAISHY M. S., 1944, The origin of curves in rivers, Current Sci. (India), 13, 36",{},{"id":26,"text":3264,"url":26,"identifiers":3265},"QURESHY M. A., 1962, Report on Regime Relations in a Gravel Reach of the Red Deer River, Alberta, 192",{},{"id":26,"text":3267,"url":26,"identifiers":3268},"RAUDKIVI A. J., 1964, Study of sediment ripple formation, Proc. Am. Soc. Civil Engrs., J. Hydraulics Div., 89, 15",{},{"id":26,"text":3270,"url":26,"identifiers":3271},"REINEMUND J. A., 1955, Geology of the Deep River Coal field, North Carolina, 159",{},{"id":26,"text":3273,"url":26,"identifiers":3274},"10.1017\u002FS0022112065000630",{"doi":3273},{"id":26,"text":3276,"url":26,"identifiers":3277},"10.1098\u002Frspa.1937.0204",{"doi":3276},{"id":26,"text":3279,"url":26,"identifiers":3280},"ROUSE H., 1937, Modern conceptions of the mechanics of fluid turbulence, Trans. Am. Soc. Civil Engrs., 102, 463, 10.1061\u002FTACEAT.0004872",{"doi":3281},"10.1061\u002FTACEAT.0004872",{"id":26,"text":3283,"url":26,"identifiers":3284},"ROUSE H., 1963, On the role of turbulence in fluid motion, Am. Scientist, 51, 285",{},{"id":26,"text":3286,"url":26,"identifiers":3287},"10.1111\u002Fj.1467-8306.1964.tb00480.x",{"doi":3286},{"id":26,"text":3289,"url":26,"identifiers":3290},"10.1086\u002F624526",{"doi":3289},{"id":26,"text":3292,"url":26,"identifiers":3293},"RUSSELL R. J., 1942, Geomorphology of the Rhône delta, Ann. Assoc. Am. Geographers, 32, 149",{},{"id":26,"text":3295,"url":26,"identifiers":3296},"10.1080\u002F00045605409352142",{"doi":3295},{"id":26,"text":3298,"url":26,"identifiers":3299},"10.1007\u002F978-3-662-01034-1",{"doi":3298},{"id":26,"text":3301,"url":26,"identifiers":3302},"SCHEIDEGGER A., 1965, The algebra of stream‐order numbers, U.S., Geol. Surv., Profess. Papers, 525, 187",{},{"id":26,"text":3304,"url":26,"identifiers":3305},"10.1130\u002F0016-7606(1957)68[1371:UGOSM]2.0.CO;2",{"doi":3304},{"id":26,"text":3307,"url":26,"identifiers":3308},"10.1130\u002F0016-7606(1963)74[1439:EPCITS]2.0.CO;2",{"doi":3307},{"id":26,"text":3310,"url":26,"identifiers":3311},"SCHLEE J., 1961, Geometry of Sandstone Bodies, 134",{},{"id":26,"text":3313,"url":26,"identifiers":3314},"10.1111\u002Fj.1467-8306.1963.tb00433.x",{"doi":3313},{"id":26,"text":3316,"url":26,"identifiers":3317},"10.1130\u002F0016-7606(1956)67[597:EODSAS]2.0.CO;2",{"doi":3316},{"id":26,"text":3319,"url":26,"identifiers":3320},"SCHUMM S. A., 1960, The shape of alluvial channels in relation to sediment type, U.S., Geol. Surv., Profess. Papers, 352, 17",{},{"id":26,"text":3322,"url":26,"identifiers":3323},"10.2475\u002Fajs.258.3.177",{"doi":3322},{"id":26,"text":3325,"url":26,"identifiers":3326},"SCHUMM S. A., 1961, Effect of sediment characteristics on erosion and deposition in ephemeral stream channels, U.S., Geol. Surv., Profess. Papers, 352, 31",{},{"id":26,"text":3328,"url":26,"identifiers":3329},"10.1130\u002F0016-7606(1963)74[1089:SOAROT]2.0.CO;2",{"doi":3328},{"id":26,"text":3331,"url":26,"identifiers":3332},"SCHUMM S. A., 1963, A tentative classification of alluvial river channels, U.S., Geol. Surv., Circ, 477, 10",{},{"id":26,"text":3334,"url":26,"identifiers":3335},"SCHUMM S. A., 1963, Channel widening and floodplain construction along Cimarron River in southwestern Kansas, U.S., Geol. Surv., Profess. Papers, 352, 71",{},{"id":26,"text":3337,"url":26,"identifiers":3338},"SEIFERT A., 1942, Schrägschichtung im Mittleren Buntsandstein des Saarlandes und angrenzender Gebiete, Z. Deut. Geol. Ges., 94, 489",{},{"id":26,"text":3340,"url":26,"identifiers":3341},"SELLARDS E. H., 1923, Geologic and soil studies on the alluvial lands of the Red River Valley, Texas, Univ., Bull., 2327, 27",{},{"id":26,"text":3343,"url":26,"identifiers":3344},"SERR E. F., 1950, Progress report, investigations of fluvial sediments of the Niobrara River near Cody, Nebraska, U.S., Geol. Surv., Circ, 67, 25",{},{"id":26,"text":3346,"url":26,"identifiers":3347},"10.1002\u002Fgj.3350030109",{"doi":3346},{"id":26,"text":3349,"url":26,"identifiers":3350},"SHAMOV G. I., 1959, Alluvial rivers, 378",{},{"id":26,"text":3352,"url":26,"identifiers":3353},"SHANTZER E. V., 1951, Alluvium of river plains in a temperate zone and its significance for understanding the laws governing the structure and formation of alluvial suites, Tr. Inst. Geol. Nauk, Akad. Nauk S.S.S.R., Geol. Ser., 135, 1",{},{"id":26,"text":3355,"url":26,"identifiers":3356},"SHEPARD F. P., 1956, Marginal sediments of Mississippi delta, Bull. Am. Assoc. Petrol. Geologists, 40, 2537",{},{"id":26,"text":3358,"url":26,"identifiers":3359},"SHINOHARA K., 1959, On the characteristics of the sand waves formed upon the beds of the open channels and rivers, Rept. Res. Inst. Appl. Mech. Kyushu Univ., Fukuoka, 7, 15",{},{"id":26,"text":3361,"url":26,"identifiers":3362},"SIGAFOOS R. S., 1964, Botanical evidence of floods and floodplain deposition, 35",{},{"id":26,"text":3364,"url":26,"identifiers":3365},"SIMONS D. B., 1961, Forms of bed roughness in alluvial channels, Proc. Am. Assoc. Civil Engrs., J. Hydraulics Div., 87, 87",{},{"id":26,"text":3367,"url":26,"identifiers":3368},"SIMONS D. 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Geologists, 48, 547",{},{"id":26,"text":3379,"url":26,"identifiers":3380},"10.1007\u002FBF02296856",{"doi":3379},{"id":26,"text":3382,"url":26,"identifiers":3383},"10.2307\u002F520380",{"doi":3382},{"id":26,"text":3385,"url":26,"identifiers":3386},"10.1029\u002FJZ070i008p01831",{"doi":3385},{"id":26,"text":3388,"url":26,"identifiers":3389},"STERNBERG H., 1875, Untersuchungen über Langen‐ und Querprofile geschieberführender Flüsse Z, 483",{},{"id":26,"text":3391,"url":26,"identifiers":3392},"10.1086\u002F625393",{"doi":3391},{"id":26,"text":3394,"url":26,"identifiers":3395},"STOKES W. L., 1953, Primary sedimentary trend indicators as applied to ore finding in the Carizzo Mountains, Arizona and New Mexico, U.S. At. Energy Comm, 3043, 48",{},{"id":26,"text":3397,"url":26,"identifiers":3398},"STOKES W. L., 1954, Some stratigraphic, sedimentary and structural relations of uranium deposits in the Salt Wash sandstone, U.S. At. Energy Comm, 3102, 50",{},{"id":26,"text":3400,"url":26,"identifiers":3401},"STOKES W. L., 1961, Geometry of Sandstone Bodies, Am Assoc. Petrol, 151",{},{"id":26,"text":3403,"url":26,"identifiers":3404},"10.1130\u002F0016-7606(1952)63[1117:HAAOET]2.0.CO;2",{"doi":3403},{"id":26,"text":3406,"url":26,"identifiers":3407},"STRAHLER A. N., 1956, Qualitative analysis of watershed geomorphology, Trans. Am. Geophys. Union, 37, 359",{},{"id":26,"text":3409,"url":26,"identifiers":3410},"10.1130\u002F0016-7606(1961)72[19:DSDOTB]2.0.CO;2",{"doi":3409},{"id":26,"text":3412,"url":26,"identifiers":3413},"10.1144\u002Fgsjgs.119.1.0175",{"doi":3412},{"id":26,"text":3415,"url":26,"identifiers":3416},"SUNDBORG Å., 1956, The River Klarälven: a study of fluvial processes, Geograf. Ann., 38, 127",{},{"id":26,"text":3418,"url":26,"identifiers":3419},"SUNDBORG Å, 1963, Gota älv, hydrologi och morfologi, Sveriges Geol. Undersökn. Arsbok, Ser. 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Civil Engrs., 111, 67, 10.1061\u002FTACEAT.0005975",{"doi":3454},"10.1061\u002FTACEAT.0005975",{"id":26,"text":3456,"url":26,"identifiers":3457},"VEEN J., 1935, Sand waves in the North Sea, Hydrograph. Rev., 12, 1",{},{"id":26,"text":3459,"url":26,"identifiers":3460},"VELIKANOV M. A., 1958, Stream‐bed Processes: Basic Theory, 395",{},{"id":26,"text":3462,"url":26,"identifiers":3463},"10.1144\u002Fpygs.30.2.115",{"doi":3462},{"id":26,"text":3465,"url":26,"identifiers":3466},"WHIPPLE W., 1942, Missouri River slope and sediment, Trans. Am. Soc. Civil Engrs., 107, 1178, 10.1061\u002FTACEAT.0005552",{"doi":3467},"10.1061\u002FTACEAT.0005552",{"id":26,"text":3469,"url":26,"identifiers":3470},"WILHELMY H., 1958, Umlaufen und Dammuferseen tropischer Tieflandflüsse, Z. Geomorphol., 2, 27",{},{"id":26,"text":3472,"url":26,"identifiers":3473},"WILLIAMS E. G., 1959, Aspects of the paleogeography of the coal measures in western Pennsylvania, Bull. Mineral Ind. Exp. Sta., Penna. State Univ., 28, 1",{},{"id":26,"text":3475,"url":26,"identifiers":3476},"WILLS L. J., 1952, A Palaeogeographical Atlas of the British Isles and Adjacent Parts of Europe, 64",{},{"id":26,"text":3478,"url":26,"identifiers":3479},"WOLMAN M. G., 1955, The natural channel of Branywine Creek, Pennsylvania, 56",{},{"id":26,"text":3481,"url":26,"identifiers":3482},"10.2475\u002Fajs.257.3.204",{"doi":3481},{"id":26,"text":3484,"url":26,"identifiers":3485},"WOLMAN M. G., 1961, Factors controlling the size and shape of stream channels in coarse non‐cohesive sands, U.S., Geol. Surv., Profess. Papers, 282, 183",{},{"id":26,"text":3487,"url":26,"identifiers":3488},"10.1029\u002FTR039i001p00001",{"doi":3487},{"id":26,"text":3490,"url":26,"identifiers":3491},"WOLMAN M. G., 1957, River floodplains: some observations on their formation, U.S., Geol. Surv., Profess. Papers, 282, 87",{},{"id":26,"text":3493,"url":26,"identifiers":3494},"10.1086\u002F626637",{"doi":3493},{"id":26,"text":3496,"url":26,"identifiers":3497},"10.1017\u002FS0016756800050081",{"doi":3496},{"id":26,"text":3499,"url":26,"identifiers":3500},"YALIN M. S., 1964, Geometrical properties of sand waves. Proc. Am. Soc. Civil Engrs, J. Hydraulics Div., 90, 105, 10.1061\u002FJYCEAJ.0001097",{"doi":3501},"10.1061\u002FJYCEAJ.0001097",{"id":26,"text":3503,"url":26,"identifiers":3504},"10.1130\u002F0016-7606(1962)73[1515:TJABEP]2.0.CO;2",{"doi":3503},{"id":26,"text":3506,"url":26,"identifiers":3507},"10.1130\u002F0016-7606(1955)66[177:SFAIIT]2.0.CO;2",{"doi":3506},{"id":26,"text":3509,"url":26,"identifiers":3510},"YOUNG R. G., 1957, Late Cretaceous cyclic deposits, Book Cliffs, eastern Utah, Bull. Am. Assoc. Petrol. Geologists, 41, 1760",{},{"id":26,"text":3512,"url":26,"identifiers":3513},"10.1086\u002F623976",{"doi":3512},{"id":26,"text":3515,"url":26,"identifiers":3516},"ZNAMENSKAYA N. S., 1963, Calculations of the dimensions and speed of shifting of channel formations, 111",{},{"id":26,"text":3518,"url":26,"identifiers":3519},"ZNAMENSKAYA N. S., 1963, Effect of average channel formations on the local scour at bridge piers, 325",{},{"id":26,"text":3521,"url":26,"identifiers":3522},"ZNAMENSKAYA N. S., 1964, Experimental study of the dune movement of sediment, 253",{},{"id":3524,"createTime":3525,"updateTime":3525,"relativeEntities":3526,"slug":3527,"properties":3528,"entityType":859,"verifyStatus":25,"verifyTime":3525,"verifyNote":861,"syncStatus":28,"languages":3540,"translateLanguages":26,"viewCount":36,"primaryUrl":3541,"fullTextUrl":26,"authors":3542,"publicationType":902,"publisherRelationship":3565,"citationCount":785,"citationInfo":3602,"publishDate":3604,"publishYear":3605,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":3606,"isForceReanalyzing":1431},"e9b3c23c-4b9a-4c1f-afa3-42092d36bbb5","2024-09-21T21:54:04.283+00:00",[],"Water-escape-structures-in-coarse-grained-sediments",{"mag":3529,"keywords":3531,"openalex":3532,"abstract":3534,"title":3536,"doi":3538},{"VOID":3530},"1995185494",{},{"VOID":3533},"W1995185494",{"EN":3535},"\u003Cjats:title>ABSTRACT\u003C\u002Fjats:title>\u003Cjats:p>Three processes of water escape characterize the consolidation of silt‐, sand‐and gravel‐sized sediments. Seepage involves the slow upward movement of pore fluids within existing voids or rapid flow within compact and confined sediments. Liquefaction is marked by the sudden breakdown of a metastable, loosely packed grain framework, the grains becoming temporarily suspended in the pore fluid and settling rapidly through the fluid until a grain‐supported structure is re‐established. Fluidization occurs when the drag exerted by moving pore fluids exceeds the effective weight of the grains; the particles are lifted, the grain framework destroyed, and the sediment strength reduced to nearly zero. Diagenetic sedimentary structures formed in direct response to processes of fluid escape are here termed water escape structures.\u003C\u002Fjats:p>\u003Cjats:p>Four main types of water escape structures form during the fluidization and liquefaction of sands: (1) soft‐sediment mixing bodies, (2) soft‐sedimsnt intrusions, (3) consolidation laminations, and (4) soft‐sediment folds. These structures represent both the direct rearrangement of sediment grains by escaping fluids and the deformation of hydroplastic, liquefied, or fluidized sediment in response to external stresses.\u003C\u002Fjats:p>\u003Cjats:p>Fundamental controls on sediment consolidation are exerted by the bulk sediment properties of grain size, packing, permeability, and strength, which together determine whether consolidation will occur and, if so the course it follows, and by external disturbances which act to trigger liquefaction and fluidization. The liquefaction and fluidization of natural sands usually accompanies the collapse of loosely packed cross‐bedded deposits. This collapse is commonly initiated by water forced into the units as underlying beds, especially muds and clays, consolidate. The consolidation of subjacent units is often triggered by the rapid deposition of the sand itself, although earthquakes or other disturbances are probably influential in some instances.\u003C\u002Fjats:p>\u003Cjats:p>Water escape structures most commonly form in fine‐ to medium‐grained sands deposited at high instantaneous and mean sedimentation rates; they are particularly abundant in cross‐laminated deposits but rare in units deposited under upper flow regime plane bed conditions. Their development is favoured by upward decreasing permeability within sedimentation units such as normally graded turbidites. They are especially common in sequences made up of alternating fine‐(clay and mud) and coarse‐grained (sand) units such as deep‐sea flysch prodelta, and, to a lesser extent, fluvial point bar, levee, and proximal overbank deposits.\u003C\u002Fjats:p>",{"EN":3537},"Water escape structures in coarse‐grained sediments",{"VOID":3539},"10.1111\u002Fj.1365-3091.1975.tb00290.x",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-3091.1975.tb00290.x",[3543],{"id":3544,"sortIndex":36,"researcher":26,"roles":3545,"affiliations":3546,"properties":3558},"bc98ae8c-7a20-4099-b4c7-45d16f455934",[],[3547],{"id":3548,"sortIndex":36,"affiliation":3549,"properties":26},"4c4c055c-4f42-4f2c-95d6-5aed5db8dc92",{"id":3550,"createTime":3551,"updateTime":3552,"relativeEntities":3553,"slug":3554,"properties":3555,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"a380b76f-0de5-4cee-bce3-a7775edc8be9","2023-12-06T21:32:20.822+00:00","2024-09-21T21:54:04.292+00:00",[],"Department-of-Geology-Louisiana-State-University-Baton-Rouge-Louisiana-70803-U-S-A-",{"title":3556},{"VI":3557},"Department of Geology, Louisiana State University, Baton Rouge, Louisiana 70803, U.S.A.",{"openalex":3559,"orcid":3561,"title":3563},{"VOID":3560},"A5019581661",{"VOID":3562},"https:\u002F\u002Forcid.org\u002F0000-0002-1387-2700",{"EN":3564},"Donald R. 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Soil Mechanics and Foundation Engineering, 1, 29",{},{"id":26,"text":3644,"url":26,"identifiers":3645},"Bouma A., 1962, Sedimentology of Some Flysch Deposits, 168",{},{"id":26,"text":3647,"url":26,"identifiers":3648},"10.1111\u002Fj.1365-3091.1970.tb02186.x",{"doi":3647},{"id":26,"text":3650,"url":26,"identifiers":3651},"Casagrande A., 1936, Characteristics of cohesionless soils affecting the stability of slopes and earth fills, J. Boston Soc. civ. Engrs, 23, 13",{},{"id":26,"text":3653,"url":26,"identifiers":3654},"Castro G., 1969, Liquefaction of sands, Harvard Soil Mech. 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Petrol., 33, 616",{},{"id":26,"text":3703,"url":26,"identifiers":3704},"10.1111\u002Fj.1365-3091.1965.tb02112.x",{"doi":3703},{"id":26,"text":3706,"url":26,"identifiers":3707},"10.2475\u002Fajs.264.5.350",{"doi":3706},{"id":26,"text":3709,"url":26,"identifiers":3710},"Florin V.A., 1961, Liquefaction of saturated sandy soils, Proc. 5th Int. Conf. Soil Mechanics and Foundation Engineering, 1, 107",{},{"id":26,"text":3712,"url":26,"identifiers":3713},"Fuller M.L., 1912, The New Madrid Earthquake, Bull. U.S. geol. Surv., 494, 119",{},{"id":26,"text":3715,"url":26,"identifiers":3716},"10.1086\u002F626251",{"doi":3715},{"id":26,"text":3718,"url":26,"identifiers":3719},"10.1144\u002FGSL.JGS.1957.113.01-04.19",{"doi":3718},{"id":26,"text":3721,"url":26,"identifiers":3722},"Goodman R.E., 1966, Earthquake‐induced displacements in sand embankments, J. Soil Mech. Fdns Div. Am. Soc. civ. 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Geol., 34, 717",{},{"id":26,"text":3835,"url":26,"identifiers":3836},"10.1017\u002FS0016756800061240",{"doi":3835},{"id":26,"text":3838,"url":26,"identifiers":3839},"Sanders J.R., 1963, Concepts of fluid mechanics provided by primary sedimentary structures, J. sedim. Petrol., 33, 173",{},{"id":26,"text":3841,"url":26,"identifiers":3842},"10.2110\u002Fpec.65.08.0192",{"doi":3841},{"id":26,"text":3844,"url":26,"identifiers":3845},"Seed H.B., 1968, Landslides during earthquakes due to liquefaction, J. Soil Mech. Fdns Div. Am. Soc. civ. Engrs, 94, 1053",{},{"id":26,"text":3847,"url":26,"identifiers":3848},"Seed H.B., 1964, Earthquake stability of slopes of cohesionless soils, J. Soil Mech. Fdns Am. Soc. civ. Engrs, 90, 43",{},{"id":26,"text":3850,"url":26,"identifiers":3851},"Seed H.B., 1971, Simplified procedures for evaluating soil liquefaction potential, J. Soil Mech. Fdns Div. Am Soc. civ. Engrs, 97, 1249",{},{"id":26,"text":3853,"url":26,"identifiers":3854},"Seed H.B., 1966, Liquefaction of saturated sands during cyclic loading, J. Soil Mech. Fdns Div. Am. Soc. civ. Engrs, 92, 105",{},{"id":26,"text":3856,"url":26,"identifiers":3857},"10.1016\u002FS0070-4571(08)70509-0",{"doi":3856},{"id":26,"text":3859,"url":26,"identifiers":3860},"10.1144\u002Fsjg05040328",{"doi":3859},{"id":26,"text":3862,"url":26,"identifiers":3863},"Selley R.C., 1962, Experimental production of sedimentary structures in quicksands, Proc. geol. Soc. Lond., 1599, 101",{},{"id":26,"text":3865,"url":26,"identifiers":3866},"10.1017\u002FS0016756800055175",{"doi":3865},{"id":26,"text":3868,"url":26,"identifiers":3869},"10.1016\u002FS0070-4571(08)70510-7",{"doi":3868},{"id":26,"text":3871,"url":26,"identifiers":3872},"Soo S.K., 1967, Fluid Dynamics of Multiphase Systems, 524",{},{"id":26,"text":3874,"url":26,"identifiers":3875},"Stanley D.J.(1969)Sedimentation in slope and base‐of‐slope environments.Am. geol. Inst. Short Course Lecture Notes The New Concepts of Continental Margin Sedimentation pp.DJS‐8‐1toDJS‐8‐25.",{},{"id":26,"text":3877,"url":26,"identifiers":3878},"Stauffer P.H., 1967, Grain‐flow deposits and their implications, Santa Ynez Mountains, California, J. sedim. Petrol., 37, 487",{},{"id":26,"text":3880,"url":26,"identifiers":3881},"Stewart H.B., 1956, Contorted sediments in modern coastal lagoon explained by laboratory experiments, Bull. Am. Ass. Petrol. Geol., 40, 153",{},{"id":26,"text":3883,"url":26,"identifiers":3884},"10.1017\u002FS0016756800055151",{"doi":3883},{"id":26,"text":3886,"url":26,"identifiers":3887},"10.2307\u002F520140",{"doi":3886},{"id":26,"text":3889,"url":26,"identifiers":3890},"10.1017\u002FS0016756800061227",{"doi":3889},{"id":26,"text":3892,"url":26,"identifiers":3893},"10.1016\u002F0037-0738(68)90023-7",{"doi":3892},{"id":26,"text":3895,"url":26,"identifiers":3896},"Ten haaf E., 1956, The significance of convolute lamination, Geol. Mijnb., 18, 188",{},{"id":26,"text":3898,"url":26,"identifiers":3899},"Terzaghi K.(1947)Shear characteristics of quicksand and soft clay.Proc. 7th Texas Conf. Soil Mechanics and Foundation Engineering 1–8.",{},{"id":26,"text":3901,"url":26,"identifiers":3902},"Terzaghi J.(1956)Varieties of submarine slope failures.Proc. 8th Texas Conf. Soil Mechanics and Foundation Engineering 41pp.",{},{"id":26,"text":3904,"url":26,"identifiers":3905},"10.1111\u002Fj.1365-3091.1968.tb00845.x",{"doi":3904},{"id":26,"text":3907,"url":26,"identifiers":3908},"Vanecek V., 1966, Fluidized Bed Drying, 195",{},{"id":26,"text":3910,"url":26,"identifiers":3911},"10.2475\u002Fajs.248.1.1",{"doi":3910},{"id":26,"text":3913,"url":26,"identifiers":3914},"10.1017\u002FS0016756800076640",{"doi":3913},{"id":26,"text":3916,"url":26,"identifiers":3917},"Weller J.M., 1959, Compaction of sediments, Bull. Am. Ass. Petrol. Geol., 43, 273",{},{"id":26,"text":3919,"url":26,"identifiers":3920},"Wentworth C.M.Jr(1966)The Upper Cretaceous and Lower Tertiary rocks of the Gualala area northern Coast Ranges California 198pp.Ph.D. thesis Stanford University.",{},{"id":26,"text":3922,"url":26,"identifiers":3923},"Wentworth C.M., 1967, Dish structure, a primary sedimentary structure in coarse turbidites, Bull. Am. Ass. Petrol. Geol., 51, 485",{},{"id":26,"text":3925,"url":26,"identifiers":3926},"10.1017\u002FS0016756800061380",{"doi":3925},{"id":3928,"createTime":3929,"updateTime":3929,"relativeEntities":3930,"slug":3931,"properties":3932,"entityType":859,"verifyStatus":25,"verifyTime":3929,"verifyNote":861,"syncStatus":28,"languages":3944,"translateLanguages":26,"viewCount":36,"primaryUrl":3945,"fullTextUrl":26,"authors":3946,"publicationType":902,"publisherRelationship":3966,"citationCount":4004,"citationInfo":4005,"publishDate":4007,"publishYear":4008,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":4009,"isForceReanalyzing":1431},"31dddb43-d04c-4bba-9425-7dd3c500632c","2024-10-08T09:37:42.616+00:00",[],"Basic-types-of-stratification-in-small-eolian-dunes",{"mag":3933,"keywords":3935,"openalex":3936,"abstract":3938,"title":3940,"doi":3942},{"VOID":3934},"2067948719",{},{"VOID":3937},"W2067948719",{"EN":3939},"\u003Cjats:title>ABSTRACT\u003C\u002Fjats:title>\u003Cjats:p>The thinnest recognizable strata in modern eolian dune sands can be grouped into six classes. They are herein named planebed laminae, rippleform laminae, ripple‐foreset crosslaminae, climbing translatent strata, grainfall laminae, and sandflow cross‐strata.\u003C\u002Fjats:p>\u003Cjats:p>Planebed laminae are formed by tractional deposition on smooth surfaces at high wind velocities. They are very rare in the deposits studied. Grainfall laminae are also formed on smooth surfaces, largely by grainfall deposition in zones of flow separation. They are much more common than planebed laminae, which they closely resemble.\u003C\u002Fjats:p>\u003Cjats:p>Eolian climbing‐ripple structures are composed primarily of climbing trans‐latent strata, each of which is the depositional product of a single climbing ripple. Climbing translatent strata that formed at relatively high or supercritical angles of ripple climb are typically accompanied by rippleform laminae, which are wavy layers parallel to the rippled depositional surfaces. Ripple‐foreset crosslaminae, which are incomplete rippleform laminae produced when the angle of ripple climb is relatively low or subcritical, are rarely visible in eolian sands.\u003C\u002Fjats:p>\u003Cjats:p>Sandflow cross‐strata are formed by the avalanching of noncohesive sand on dune slipfaces. Their form varies with slipface height and with other factors.\u003C\u002Fjats:p>",{"EN":3941},"Basic types of stratification in small eolian dunes",{"VOID":3943},"10.1111\u002Fj.1365-3091.1977.tb00128.x",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-3091.1977.tb00128.x",[3947],{"id":3948,"sortIndex":36,"researcher":26,"roles":3949,"affiliations":3950,"properties":3961},"43fc6539-ba40-44ae-869f-f5464a8a5e99",[],[3951],{"id":3952,"sortIndex":36,"affiliation":3953,"properties":26},"f23d6683-1304-4d68-a216-99a3a60549a9",{"id":3954,"createTime":3955,"updateTime":3955,"relativeEntities":3956,"slug":3957,"properties":3958,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"70f14045-16d7-477e-a8f7-a780d5a816fa","2024-10-08T09:37:42.637+00:00",[],"U-S-Geological-Survey-345-Middlefield-Rodd-Menlo-Park-California-94025-U-S-A-",{"title":3959},{"EN":3960},"U.S. Geological Survey, 345 Middlefield Rodd, Menlo Park, California 94025, U.S.A.",{"openalex":3962,"title":3964},{"VOID":3963},"A5081696213",{"EN":3965},"Ralph E. Hunter",{"url":26,"publisher":3967,"properties":3997},{"id":659,"createTime":660,"updateTime":661,"relativeEntities":3968,"slug":663,"properties":3969,"entityType":24,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36,"subjectFields":3975,"manageAffiliations":3976,"indexDatabases":3977,"url":751,"thumbnailPath":26,"statistic":3992,"gsStatistic":26,"type":26,"analyzePriority":26},[],{"country":3970,"issn":3971,"introduce":3972,"eissn":3973,"title":3974},{"VOID":666},{"VOID":668},{"EN":670},{"VOID":672},{"EN":663},[],[],[3978,3985],{"id":733,"indexDatabase":3979,"url":748,"indexYears":26,"academicFieldIds":3984,"indexDatabaseRanking":26},{"id":735,"createTime":736,"updateTime":737,"relativeEntities":3980,"label":3981,"description":3982,"key":744,"publicationTags":3983,"standard":26},[],{"EN":740,"VI":740},{"VI":742,"EN":743},[746,747],[750],{"id":713,"indexDatabase":3986,"url":726,"indexYears":727,"academicFieldIds":3991,"indexDatabaseRanking":731},{"id":715,"createTime":716,"updateTime":717,"relativeEntities":3987,"label":3988,"description":3989,"key":723,"publicationTags":3990,"standard":26},[],{"EN":720,"VI":720},{"EN":720,"VI":722},[725],[729,730],{"impactFactor":36,"impactFactorByYear":3993,"i10Index":243,"i10IndexLast5Year":114,"totalPublication":761,"totalPublicationByYear":3994,"totalCitation":763,"totalCitationByYear":3995,"totalCitationPerPublication":804,"totalCitationPerPublicationByYear":3996,"hindexLast5Year":117,"hindex":117},{"2012":754,"2013":131,"2014":755,"2015":756,"2016":757,"2017":162,"2018":162,"2019":758,"2020":759,"2021":59,"2022":760,"2023":239},{"1963":115,"1964":115,"1965":115,"1968":115,"1969":114,"1971":115,"1972":115,"1974":115,"1975":114,"1976":115,"1977":111,"1978":115,"1979":59,"1980":162,"1981":115,"1983":114,"1984":162,"1985":115,"1986":114,"1987":114,"1989":59,"1990":114,"1991":59,"1992":59,"1993":162,"1994":135,"1995":111,"1996":59,"1997":111,"1998":114,"1999":162,"2000":116,"2001":59,"2002":162,"2003":111,"2004":111,"2005":135,"2006":115,"2007":111,"2008":162,"2009":59,"2010":135,"2011":115,"2012":114,"2013":114,"2014":114,"2015":114,"2016":115,"2017":59,"2018":111,"2019":115,"2020":115,"2021":115},{"1963":765,"1964":360,"1965":766,"1968":242,"1969":767,"1971":768,"1972":44,"1974":769,"1975":770,"1976":771,"1977":772,"1978":366,"1979":773,"1980":774,"1981":394,"1983":775,"1984":776,"1985":777,"1986":778,"1987":779,"1989":780,"1990":781,"1991":782,"1992":783,"1993":784,"1994":785,"1995":786,"1996":787,"1997":788,"1998":789,"1999":790,"2000":791,"2001":792,"2002":793,"2003":794,"2004":795,"2005":796,"2006":797,"2007":798,"2008":799,"2009":800,"2010":801,"2011":142,"2012":628,"2013":258,"2014":285,"2015":362,"2016":168,"2017":802,"2018":803,"2019":252,"2020":158,"2021":43},{"1963":765,"1964":360,"1965":766,"1968":242,"1969":806,"1971":768,"1972":44,"1974":769,"1975":807,"1976":771,"1977":160,"1978":366,"1979":808,"1980":809,"1981":394,"1983":810,"1984":811,"1985":777,"1986":812,"1987":813,"1989":814,"1990":815,"1991":816,"1992":817,"1993":813,"1994":818,"1995":819,"1996":820,"1997":821,"1998":822,"1999":823,"2000":824,"2001":825,"2002":826,"2003":167,"2004":827,"2005":828,"2006":797,"2007":829,"2008":830,"2009":831,"2010":832,"2011":142,"2012":833,"2013":834,"2014":124,"2015":835,"2016":168,"2017":836,"2018":837,"2019":252,"2020":158,"2021":43},{"volume":3998,"pages":4000,"issue":4002},{"VOID":3999},"24",{"VOID":4001},"361-387",{"VOID":4003},"3",731,{"total":4004,"publishYear":26,"statisticByYear":4006},{"2012":222,"2013":234,"2014":336,"2015":287,"2016":234,"2017":516,"2018":222,"2019":260,"2020":287,"2021":222,"2022":396,"2023":242,"2024":336},"1977-06-01",1977,[4010,4013,4015,4018,4020,4023,4026,4028,4031,4034,4037,4040,4043,4046,4049,4052,4055,4058,4061,4064,4067,4070,4073,4076,4079,4082,4085,4087,4089,4092,4095,4098,4101,4104,4107,4110,4113,4116,4119,4122,4125,4128,4131,4134,4137,4140,4143,4146],{"id":26,"text":4011,"url":26,"identifiers":4012},"ALLEN J.R.L., 1968, Current Ripples, their Relation to Patterns of Water and Sediment Motion, 433",{},{"id":26,"text":3617,"url":26,"identifiers":4014},{"doi":3617},{"id":26,"text":4016,"url":26,"identifiers":4017},"10.1016\u002F0037-0738(71)90001-7",{"doi":4016},{"id":26,"text":3620,"url":26,"identifiers":4019},{"doi":3620},{"id":26,"text":4021,"url":26,"identifiers":4022},"BAARS D.L., 1970, Stratigraphic control of petroleum in White Rim Sandstone (Permian) in and near Canyonlands National Park, Utah, Bull. Am. Ass. Petrol. Geol., 54, 709",{},{"id":26,"text":4024,"url":26,"identifiers":4025},"BAGNOLD R.A., 1941, The Physics of Blown Sand and Desert Dunes, 265",{},{"id":26,"text":959,"url":26,"identifiers":4027},{"doi":959},{"id":26,"text":4029,"url":26,"identifiers":4030},"BIGARELLA J.J., 1972, Eolian environments; their characteristics, recognition, and importance. In: Recognition of Ancient Sedimentary Environments (Ed. by J. K. Rigby and W. K. Hamblin), Spec. Publs Soc. econ. Paleont. Miner., Tulsa, 16, 12",{},{"id":26,"text":4032,"url":26,"identifiers":4033},"10.1016\u002F0025-3227(69)90002-4",{"doi":4032},{"id":26,"text":4035,"url":26,"identifiers":4036},"10.1130\u002F0016-7606(1956)67[125:TFSISR]2.0.CO;2",{"doi":4035},{"id":26,"text":4038,"url":26,"identifiers":4039},"10.1111\u002Fj.1365-3091.1967.tb01301.x",{"doi":4038},{"id":26,"text":4041,"url":26,"identifiers":4042},"10.1016\u002F0025-3227(69)90023-1",{"doi":4041},{"id":26,"text":4044,"url":26,"identifiers":4045},"COOPER W.S., 1958, Coastal sand dunes of Oregon and Washington, Mem. geol. Soc. Am., 72, 169",{},{"id":26,"text":4047,"url":26,"identifiers":4048},"ELLWOOD J.M., 1975, Small scale aeolian bedforms, J. sedim. Petrol., 45, 554",{},{"id":26,"text":4050,"url":26,"identifiers":4051},"FREEMAN W.E., 1975, Stratigraphic analysis of the Navajo Sandstone, J. sedim. Petrol., 45, 651",{},{"id":26,"text":4053,"url":26,"identifiers":4054},"GLENNIE K.W., 1970, Desert Sedimentary Environments, Developments in Sedimentology, 14, 222",{},{"id":26,"text":4056,"url":26,"identifiers":4057},"GOLDSMITH V., 1973, Internal geometry and origin of vegetated coastal sand dunes, J. sedim. Petrol., 43, 1128",{},{"id":26,"text":4059,"url":26,"identifiers":4060},"GRIPP K., 1961, Über Werden und Vergehen von Barchanen an der Nordsee‐Küste Schleswig‐Holsteins, Z. Geomorph., 5, 24",{},{"id":26,"text":4062,"url":26,"identifiers":4063},"HARMS J.C., 1965, Stratification, bed forms, and flow phenomena (with an example from the Rio Grande). In: Sedimentary Structures and their Hydrodynamic Interpretation (Ed. by G. V. Middleton), Spec. Publs Soc. econ. Paleont. Miner., Tulsa, 12, 84",{},{"id":26,"text":4065,"url":26,"identifiers":4066},"HUNTER R.E., 1974, Types of eolian strata and pseudostrata (abstr.), Ann. Mtg Abstr.). Am. Ass. Petrol. Geol. and Soc. econ. Palaeont. Miner., Tulsa, 1, 47",{},{"id":26,"text":4068,"url":26,"identifiers":4069},"HUNTER R.E., 1976, Comparison of eolian and subaqueous sandflow cross‐strata (abstr), Bull. Am. Ass. Petrol. Geol., 60, 683",{},{"id":26,"text":4071,"url":26,"identifiers":4072},"HUNTER R.E., 1977, Terminology of cross‐stratified sedimentary layers and climbing‐ripple structures, J. sedim. Petrol.",{},{"id":26,"text":4074,"url":26,"identifiers":4075},"HUNTER R.E., 1970, Map showing landforms and sedimentary deposits of the Padre Island portion of the South Bird Island 7.5‐minute Quadrangle, Texas, Misc. Geol. Invest. Map U.S. Geol. Surv., 1659",{},{"id":26,"text":4077,"url":26,"identifiers":4078},"HUNTER R.E., 1972, Padre Island National Seashore Field Guide, 1",{},{"id":26,"text":4080,"url":26,"identifiers":4081},"10.1130\u002F0016-7606(1966)77[787:CSDOGN]2.0.CO;2",{"doi":4080},{"id":26,"text":4083,"url":26,"identifiers":4084},"JOPLING A.V., 1964, Interpreting the concept of the sedimentation unit, J. sedim. Petrol., 34, 165",{},{"id":26,"text":3758,"url":26,"identifiers":4086},{"doi":3758},{"id":26,"text":3135,"url":26,"identifiers":4088},{"doi":3135},{"id":26,"text":4090,"url":26,"identifiers":4091},"10.1086\u002F625291",{"doi":4090},{"id":26,"text":4093,"url":26,"identifiers":4094},"McKEE E.D., 1965, Experiments on ripple lamination. In: Sedimentary Structures and their Hydrodynamic Interpretation (Ed. by G. V. Middleton), Spec. Publs Soc. econ. Paleont. Miner., Tulsa, 12, 66",{},{"id":26,"text":4096,"url":26,"identifiers":4097},"10.1111\u002Fj.1365-3091.1966.tb01579.x",{"doi":4096},{"id":26,"text":4099,"url":26,"identifiers":4100},"10.1130\u002F0016-7606(1971)82[359:DOLLIE]2.0.CO;2",{"doi":4099},{"id":26,"text":4102,"url":26,"identifiers":4103},"McKEE E.D., 1964, Primary structures of a seif dune and associated deposits in Libya, J. sedim. Petrol., 34, 5",{},{"id":26,"text":4105,"url":26,"identifiers":4106},"10.1130\u002F0016-7606(1953)64[381:TFSACI]2.0.CO;2",{"doi":4105},{"id":26,"text":4108,"url":26,"identifiers":4109},"10.2475\u002Fajs.261.4.297",{"doi":4108},{"id":26,"text":4111,"url":26,"identifiers":4112},"10.1086\u002F624659",{"doi":4111},{"id":26,"text":4114,"url":26,"identifiers":4115},"10.1007\u002FBF02000468",{"doi":4114},{"id":26,"text":4117,"url":26,"identifiers":4118},"10.1111\u002Fj.1365-2389.1951.tb00600.x",{"doi":4117},{"id":26,"text":4120,"url":26,"identifiers":4121},"RIM M., 1953, Le classement des minéraux du sable par les agents naturels sur les dunes côtières. In:, Actions Eoliennes. Centre National de la Recherche Scientifique. Paris, Colloques Internationaux, 35, 261",{},{"id":26,"text":4123,"url":26,"identifiers":4124},"10.1086\u002F626936",{"doi":4123},{"id":26,"text":4126,"url":26,"identifiers":4127},"10.1130\u002F0016-7606(1966)77[1045:KDMDC]2.0.CO;2",{"doi":4126},{"id":26,"text":4129,"url":26,"identifiers":4130},"SIMONS D.B., 1965, Sedimentary structures generated by flow in alluvial channels. In: Sedimenary Structures and their Hydrodynamic Interpretation (Ed. by G. V. Middleton), Spec. Publs Soc. econ, Paleont. Miner., Tulsa, 12, 34",{},{"id":26,"text":4132,"url":26,"identifiers":4133},"10.1007\u002FBF02132769",{"doi":4132},{"id":26,"text":4135,"url":26,"identifiers":4136},"STANLEY K.O., 1971, New hypothesis of Early Jurassic paleogeography and sediment dispersal for western United States, Bull. Am. Ass. Petrol. Geol., 55, 10",{},{"id":26,"text":4138,"url":26,"identifiers":4139},"STOKES W.L., 1968, Multiple parallel‐truncation bedding planes—a feature of wind‐deposited sand‐stone formations, J. sedim. Petrol., 38, 510",{},{"id":26,"text":4141,"url":26,"identifiers":4142},"10.1130\u002F0016-7606(1971)82[1421:DPATNS]2.0.CO;2",{"doi":4141},{"id":26,"text":4144,"url":26,"identifiers":4145},"10.1306\u002F74D71866-2B21-11D7-8648000102C1865D",{"doi":4144},{"id":26,"text":4147,"url":26,"identifiers":4148},"YAALON D.H., 1971, Internal structures in eolianites and paleowinds, Mediterranean coast, Israel, J. sedim. Petrol., 41, 1059",{},{"id":4150,"createTime":4151,"updateTime":4151,"relativeEntities":4152,"slug":4153,"properties":4154,"entityType":859,"verifyStatus":25,"verifyTime":4166,"verifyNote":861,"syncStatus":28,"languages":4167,"translateLanguages":26,"viewCount":36,"primaryUrl":4168,"fullTextUrl":26,"authors":4169,"publicationType":902,"publisherRelationship":4222,"citationCount":4259,"citationInfo":4260,"publishDate":4262,"publishYear":4263,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":4264,"isForceReanalyzing":1431},"30442542-f22f-4b72-bd88-f8a1666d6bc7","2024-12-03T20:24:04.111+00:00",[],"Lithofacies-types-and-vertical-profile-models-an-alternative-approach-to-the-description-and-environmental-interpretation-of-glacial-diamict-and-diamictite-sequences",{"mag":4155,"keywords":4157,"openalex":4158,"abstract":4160,"title":4162,"doi":4164},{"VOID":4156},"2091643973",{},{"VOID":4159},"W2091643973",{"EN":4161},"\u003Cjats:p>\u003Cjats:bold>ABSTRACT\u003C\u002Fjats:bold> Increased knowledge of modern glacial depositional environments has resulted in rapidly evolving classifications of glacial tills. These are based to a large degree on theoretical considerations of likely depositional processes. The classifications are sophisticated and more advanced than the establishment of simple field criteria whereby individual till facies can be identified in Quaternary and Pre‐Quaternary successions. This situation is compounded in many Quaternary terrains by the continued description of ‘tills’ in terms of laboratory‐derived analytical data only, reflecting a traditional interest in stratigraphic correlation rather than reconstruction of depositional environment. Detailed sedimentological logging of lithofacies is rarely undertaken. There is thus considerable confusion as to what is being described or sampled when analytical data are presented for many Pleistocene ‘tills’. The same remarks apply to Pre‐Pleistocene ‘tillites’.\u003C\u002Fjats:p>\u003Cjats:p>A lithofacies code is presented here for the rapid description and visual appraisal of field sequences or drill cores containing unconsolidated diamicts or lithified diamictites; the term‘till’is not used as it has a strict genetic definition referring to direct aggregation and deposition by glacier ice. Use of a four part code, in conjunction with codes already published for fluvial sediments, allows fundamental field properties to be depicted independent of genetic terminology and provides a firm basis for subsequent environmental interpretation and analytical work. The value of this approach is illustrated by comparing a representative suite of vertical profiles of diamict assemblages deposited by modern grounded glaciers with a classic late Pleistocene glacigenic sequence at Scarborough Bluffs, Ontario.\u003C\u002Fjats:p>",{"EN":4163},"Lithofacies types and vertical profile models; an alternative approach to the description and environmental interpretation of glacial diamict and diamictite sequences",{"VOID":4165},"10.1111\u002Fj.1365-3091.1983.tb00679.x","2024-12-03T20:24:04.110+00:00",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-3091.1983.tb00679.x",[4170,4192,4207],{"id":4171,"sortIndex":115,"researcher":26,"roles":4172,"affiliations":4173,"properties":4185},"b03f9744-6f79-4d67-a4ea-4400103fa21c",[],[4174],{"id":4175,"sortIndex":36,"affiliation":4176,"properties":26},"0fd65bf2-77d0-40e8-91aa-f9dab1695044",{"id":4177,"createTime":4178,"updateTime":4179,"relativeEntities":4180,"slug":4181,"properties":4182,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"85887531-1e0b-4a77-82fe-bd4a35afd650","2023-12-13T13:07:17.761+00:00","2024-12-03T20:24:04.131+00:00",[],"Department-of-Geology-University-of-Toronto-Toronto-Ontario-M5S-1A1-Canada",{"title":4183},{"VI":4184},"Department of Geology, University of Toronto, Toronto, Ontario M5S 1A1 Canada",{"openalex":4186,"orcid":4188,"title":4190},{"VOID":4187},"A5005247855",{"VOID":4189},"https:\u002F\u002Forcid.org\u002F0000-0002-8586-7003",{"EN":4191},"Carolyn H. 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Prog. geol. Soc. Am., 14, 444",{},{"id":26,"text":4278,"url":26,"identifiers":4279},"10.1130\u002F0091-7613(1979)7\u003C532:NOAGDO>2.0.CO;2",{"doi":4278},{"id":26,"text":4281,"url":26,"identifiers":4282},"10.1144\u002Fgsjgs.128.4.0361",{"doi":4281},{"id":26,"text":4284,"url":26,"identifiers":4285},"Boulton G.S., 1975, Ice Ages Ancient and Modern, 7",{},{"id":26,"text":4287,"url":26,"identifiers":4288},"Boulton G.S., 1975, Glacial Geomorphology, 41",{},{"id":26,"text":4290,"url":26,"identifiers":4291},"Boulton G.S., 1976, A genetic classification of tills and criteria for distinguishing tills of different origin, Geografia, 12, 66",{},{"id":26,"text":4293,"url":26,"identifiers":4294},"Boulton G.S., 1977, A multiple till sequence by a Late Devensian Welsh Ice cap, Glanllynnau, Gwynedd, Cambria, 4, 10",{},{"id":26,"text":4296,"url":26,"identifiers":4297},"10.1111\u002Fj.1365-3091.1978.tb00329.x",{"doi":4296},{"id":26,"text":4299,"url":26,"identifiers":4300},"Boulton G.S., 1974, Subglacial shear deformation and crushing in lodgement tills from south‐east Iceland, Geogr. 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Penny L.F. Shotton F.W.&West R.G.(1973A correlation of Quaternary deposits in the British Isles.Spec. Rep. geol. Soc. London. No. 4 99pp.",{},{"id":26,"text":4435,"url":26,"identifiers":4436},"10.1017\u002FS0022143000015306",{"doi":4435},{"id":26,"text":4438,"url":26,"identifiers":4439},"Mulholland J.W., 1976, Texture of tills, central Massachusetts, J. sedim. Petrol., 46, 778",{},{"id":26,"text":4441,"url":26,"identifiers":4442},"Nardin T.R., 1979, Geology of Continental Slopes, 27",{},{"id":26,"text":4444,"url":26,"identifiers":4445},"10.1111\u002Fj.1365-3091.1980.tb01645.x",{"doi":4444},{"id":26,"text":4447,"url":26,"identifiers":4448},"Reading H.G., 1978, Sedimentary Environments and Facies, 557",{},{"id":26,"text":4450,"url":26,"identifiers":4451},"10.1139\u002Fe77-020",{"doi":4450},{"id":26,"text":4453,"url":26,"identifiers":4454},"Rust B.R., 1978, Fluvial Sedimentology, 5",{},{"id":26,"text":4456,"url":26,"identifiers":4457},"Rust B.R., 1979, Facies Models, 9",{},{"id":26,"text":4459,"url":26,"identifiers":4460},"Ryder J.M., 1971, The stratigraphy and morphology of paraglacial alluvial fans in south‐central British Columbia, Can. J. Earth Sci., 8, 279, 10.1139\u002Fe71-027",{"doi":4461},"10.1139\u002Fe71-027",{"id":26,"text":4463,"url":26,"identifiers":4464},"Schluchter C., 1979, Moraines and Varves",{},{"id":26,"text":4466,"url":26,"identifiers":4467},"10.1139\u002Fe77-113",{"doi":4466},{"id":26,"text":4469,"url":26,"identifiers":4470},"10.1111\u002Fj.1502-3885.1977.tb00348.x",{"doi":4469},{"id":26,"text":4472,"url":26,"identifiers":4473},"10.1111\u002Fj.1502-3885.1979.tb00437.x",{"doi":4472},{"id":26,"text":4475,"url":26,"identifiers":4476},"10.1306\u002FD426953A-2B26-11D7-8648000102C1865D",{"doi":4475},{"id":26,"text":4478,"url":26,"identifiers":4479},"Shroder J.F., 1981, Diamicton differentiation La Sal Mountains and high plateaus, Utah and Idaho, Abstr. Prog. geol. Soc. Am., 13, 553",{},{"id":26,"text":4481,"url":26,"identifiers":4482},"10.1144\u002Fgsjgs.137.2.0125",{"doi":4481},{"id":26,"text":4484,"url":26,"identifiers":4485},"Stankowski W., 1980, Tills and glacigene deposits, Univ. Adam Mickiewicza, Poznan, Geog. Ser., 20",{},{"id":26,"text":4487,"url":26,"identifiers":4488},"10.2307\u002F1550407",{"doi":4487},{"id":26,"text":4490,"url":26,"identifiers":4491},"Terasmae J., 1972, Quaternary stratigraphy and geomorphology of the eastern Great Lakes region of Southern Ontario, Geol. Cong. Excurs, 42",{},{"id":26,"text":4493,"url":26,"identifiers":4494},"Visher G.S., 1965, Use of vertical profile in environmental reconstruction, Bull. Am. Ass. Petrol. Geol., 49, 41",{},{"id":26,"text":4496,"url":26,"identifiers":4497},"10.1130\u002F0016-7606(1975)86\u003C737:GFMFRC>2.0.CO;2",{"doi":4496},{"id":26,"text":4499,"url":26,"identifiers":4500},"Walker R.C.(Ed.) (1979Facies Models.Geol. Ass. Can. Res. Series.",{},{"id":26,"text":4502,"url":26,"identifiers":4503},"Willman H.B., 1970, Pleistocene Stratigraphy of Illinois",{},{"id":4505,"createTime":4506,"updateTime":4506,"relativeEntities":4507,"slug":4508,"properties":4509,"entityType":859,"verifyStatus":25,"verifyTime":4520,"verifyNote":861,"syncStatus":28,"languages":4521,"translateLanguages":26,"viewCount":36,"primaryUrl":4522,"fullTextUrl":26,"authors":4523,"publicationType":902,"publisherRelationship":4570,"citationCount":4607,"citationInfo":4608,"publishDate":4610,"publishYear":4611,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":4612,"isForceReanalyzing":1431},"c8182185-dd71-4c71-82e8-4c1e850dae8d","2024-10-11T12:36:08.923+00:00",[],"Variability-of-deltaic-processes-in-terms-of-sediment-supply-with-particular-emphasis-on-grain-size",{"mag":4510,"keywords":4512,"openalex":4513,"abstract":4515,"title":4517,"doi":4519},{"VOID":4511},"2070821133",{},{"VOID":4514},"W2070821133",{"EN":4516},"\u003Cjats:title>ABSTRACT\u003C\u002Fjats:title>\u003Cjats:p>Short term variability in delta form and process can be partly explained by the relative strength of hydraulic parameters such as river discharge, discharge variability, wave energy flux and tidal range. However, the calibre or grain size is also important. The amount, mode of transport and grain size of the sediment load delivered to a delta front have a considerable effect on the facies, formative physical processes, related depositional environments and morphology of the deltaic depositional system. The available grain size influences (1) the gradient and channel pattern of the fluvial system on the delta plain; (2) the mixing behaviour of sediment as it discharges into the ambient basin waters at the river mouth; (3) the type of shoreline, whether reflective or dissipative, and its response to both wave energy and tidal regime; and (4) the deformation and resedimentation processes on the subaqueous delta front. Long term aspects of deltaic sedimentation, including a few generalized relationships between sediment supply and physiographic setting, are briefly introduced. The need for further detailed research on modern and ancient deltaic dispersal systems is emphasized, and specific suggestions are given for future research.\u003C\u002Fjats:p>",{"EN":4518},"Variability of deltaic processes in terms of sediment supply, with particular emphasis on grain size",{"VOID":2092},"2024-10-11T12:36:08.922+00:00",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-3091.1993.tb01347.x",[4524,4555],{"id":4525,"sortIndex":36,"researcher":26,"roles":4526,"affiliations":4527,"properties":4550},"58d3464d-ef82-490f-b957-eb377058b715",[],[4528,4539],{"id":4529,"sortIndex":36,"affiliation":4530,"properties":26},"0e24cc80-f97c-4f09-94ba-8ae93017f13b",{"id":4531,"createTime":4532,"updateTime":4533,"relativeEntities":4534,"slug":4535,"properties":4536,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"2cb9a1ac-4099-47a3-b6e0-6a94e94e7623","2024-01-09T08:06:59.253+00:00","2025-01-02T15:42:32.277+00:00",[],"Department-of-Earth-Sciences-Oxford-University-Parks-Road-Oxford-OX1-3PR-UK",{"title":4537},{"VI":4538},"Department of Earth Sciences, Oxford University, Parks Road, Oxford OX1 3PR, UK",{"id":4540,"sortIndex":115,"affiliation":4541,"properties":26},"ca821078-2224-4493-9578-8559bfe16065",{"id":4542,"createTime":4543,"updateTime":4544,"relativeEntities":4545,"slug":4546,"properties":4547,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"f34ccb6e-3c54-4c56-a64e-30bbb359a723","2024-02-11T23:49:56.185+00:00","2024-12-11T23:29:33.705+00:00",[],"Department-of-Geology-McMaster-University-Hamilton-Ontario-Canada-L8S-4M1",{"title":4548},{"VI":4549},"Department of Geology, McMaster University, Hamilton, Ontario, Canada, L8S 4M1",{"openalex":4551,"title":4553},{"VOID":4552},"A5015121664",{"EN":4554},"Geoff Orton",{"id":4556,"sortIndex":115,"researcher":26,"roles":4557,"affiliations":4558,"properties":4565},"8f309f3d-417b-44d8-945c-8cdd91a15309",[],[4559],{"id":4560,"sortIndex":36,"affiliation":4561,"properties":26},"79ede22f-107e-4865-8006-0904bc12bc32",{"id":4531,"createTime":4532,"updateTime":4533,"relativeEntities":4562,"slug":4535,"properties":4563,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":4564},{"VI":4538},{"openalex":4566,"title":4568},{"VOID":4567},"A5000207345",{"EN":4569},"H. 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Geol., Calgary, 10, 331",{},{"id":26,"text":4674,"url":26,"identifiers":4675},"Bowman D., 1990, Climatically triggered Gilbert‐type lacustrine fan deltas, the Dead Sea area, Israel, Spec. Publs int. Ass. Sediment., 10, 273",{},{"id":26,"text":4677,"url":26,"identifiers":4678},"10.1130\u002F0091-7613(1989)017\u003C0926:ROSSTM>2.3.CO;2",{"doi":4677},{"id":26,"text":4680,"url":26,"identifiers":4681},"Brayshaw A.C., 1984, Characteristics and origin of cluster bedforms in coarse‐grained alluvial channels, Mem. Can. Soc. Petrol. Geol., Calgary, 10, 77",{},{"id":26,"text":4683,"url":26,"identifiers":4684},"10.1306\u002F212F7E37-2B24-11D7-8648000102C1865D",{"doi":4683},{"id":26,"text":4686,"url":26,"identifiers":4687},"Bristow C.S., 1987, Brahmaputra River:channel migration and deposition, Spec. Publs Soc. econ. Paleont. 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Geol., 57, 370",{},{"id":26,"text":5271,"url":26,"identifiers":5272},"10.1086\u002F628028",{"doi":5271},{"id":26,"text":5274,"url":26,"identifiers":5275},"10.1016\u002F0025-3227(84)90008-2",{"doi":5274},{"id":26,"text":5277,"url":26,"identifiers":5278},"10.1086\u002F627805",{"doi":5277},{"id":26,"text":5280,"url":26,"identifiers":5281},"10.1016\u002F0025-3227(79)90149-X",{"doi":5280},{"id":26,"text":5283,"url":26,"identifiers":5284},"10.1016\u002FS0302-3524(80)80083-1",{"doi":5283},{"id":26,"text":5286,"url":26,"identifiers":5287},"Wright L.D., 1986, Hyperpycnal plumes and plume fronts over the Huanghe (Yellow River) delta front, Geomarine Lett., 6, 97",{},{"id":26,"text":5289,"url":26,"identifiers":5290},"Wright L.D., 1986, Short period internal waves over the Huanghe (Yellow River) delta front, Geomarine Lett., 6, 115",{},{"id":26,"text":5292,"url":26,"identifiers":5293},"10.1016\u002F0025-3227(89)90135-7",{"doi":5292},{"id":26,"text":5295,"url":26,"identifiers":5296},"10.1029\u002FTR036i004p00655",{"doi":5295},{"id":5298,"createTime":5299,"updateTime":5299,"relativeEntities":5300,"slug":5301,"properties":5302,"entityType":859,"verifyStatus":25,"verifyTime":5299,"verifyNote":861,"syncStatus":28,"languages":5313,"translateLanguages":26,"viewCount":36,"primaryUrl":5314,"fullTextUrl":26,"authors":5315,"publicationType":902,"publisherRelationship":5355,"citationCount":5392,"citationInfo":5393,"publishDate":5395,"publishYear":5396,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":5397,"isForceReanalyzing":1431},"5c952fa9-be1c-4f1d-9fc8-6a181a64937b","2024-10-01T02:56:53.561+00:00",[],"A-simulation-model-of-alluvial-stratigraphy",{"mag":5303,"keywords":5305,"openalex":5306,"abstract":5308,"title":5310,"doi":5312},{"VOID":5304},"2091350509",{},{"VOID":5307},"W2091350509",{"EN":5309},"\u003Cjats:title>ABSTRACT\u003C\u002Fjats:title>\u003Cjats:p>The quantitative model presented simulates the development of a two‐dimensional alluvial sedimentary succession beneath a floodplain traversed by a single major river. Several inter‐related effects which influence the distribution of channel‐belt sand and gravel bodies within overbank fines are accounted for. These are (a) laterally variable aggradation, (b) compaction of fine sediment, (c) tectonic movement at floodplain margins, and (d) channel avulsion. Selected experiments with the model show how the interconnectedness and areal density of channel‐belt deposits decrease with increasing floodplain width\u002Fchannel‐belt size, mean avulsion period, and channel‐belt aggradation rate. Separation of stream patterns based on interconnectedness and channel deposit density is difficult. Tectonic movements do not have a significant influence upon the successions unless a preferred direction of tilting is maintained (half‐graben). Then channel‐belt deposits showing offlap tendencies tend to cluster adjacent to the active floodplain margin, leaving dominantly fine‐grained alluvium to accumulate on the inactive side. Individual channel‐belt deposits thicken during aggradation, although a self‐regulating limit to such thickening is likely to operate. ‘Multistorey’features resulting from aggradation may be difficult to tell apart from those arising through superposition of distinct channel‐belt deposits of avulsive origin.\u003C\u002Fjats:p>",{"EN":5311},"A simulation model of alluvial stratigraphy",{"VOID":1697},[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-3091.1979.tb00935.x",[5316,5335],{"id":5317,"sortIndex":115,"researcher":26,"roles":5318,"affiliations":5319,"properties":5330},"2934c873-8039-4748-a841-65865172bc26",[],[5320],{"id":5321,"sortIndex":36,"affiliation":5322,"properties":26},"d8945cf6-3666-41c4-9d49-5c8f0432f620",{"id":5323,"createTime":5324,"updateTime":5324,"relativeEntities":5325,"slug":5326,"properties":5327,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"a2353a56-4211-4a64-97b4-2847496dafb8","2024-10-01T02:56:53.581+00:00",[],"Department-of-Earth-Sciences-University-of-Leeds-Leeds-LS-2-9-JT-U-K-",{"title":5328},{"EN":5329},"Department of Earth Sciences, University of Leeds, Leeds LS 2 9 JT, U.K.",{"openalex":5331,"title":5333},{"VOID":5332},"A5090704729",{"EN":5334},"M. 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Geol., 53, 30",{},{"id":26,"text":5468,"url":26,"identifiers":5469},"Fisk H.N., 1944, Geological Investigation of the Alluvial Valley of the Lower Mississippi River",{},{"id":26,"text":5471,"url":26,"identifiers":5472},"Fisk H.N., 1947, Fine Grained Alluvial Deposits and their Effects on Mississippi River Activity",{},{"id":26,"text":5474,"url":26,"identifiers":5475},"Fisk H.N., 1952, Mississippi River Valley geology: relation to river regime, Trans. Am. Soc. civ. Engs, 117, 667, 10.1061\u002FTACEAT.0006733",{"doi":2822},{"id":26,"text":5477,"url":26,"identifiers":5478},"Friend P.F., 1972, Sedimentation of the Wood Bay Formation (Devonian) of Spitsbergen: regional analysis of a late orogenic basin, Norsk. Pol. Skr, 157",{},{"id":26,"text":5480,"url":26,"identifiers":5481},"10.1680\u002Fiicep.1975.3641",{"doi":5480},{"id":26,"text":5483,"url":26,"identifiers":5484},"Gole C.V., 1966, Inland delta building activity of Kosi River, J. Hydraul. Div. Am. Soc. Civ. Engrs, 92, 111",{},{"id":26,"text":5486,"url":26,"identifiers":5487},"10.1016\u002F0040-1951(74)90067-5",{"doi":5486},{"id":26,"text":5489,"url":26,"identifiers":5490},"10.1016\u002F0040-1951(74)90030-4",{"doi":5489},{"id":26,"text":5492,"url":26,"identifiers":5493},"10.2475\u002Fajs.243.3.113",{"doi":5492},{"id":26,"text":5495,"url":26,"identifiers":5496},"Harbaugh J.W., 1970, Computer Simulation in Geology",{},{"id":26,"text":5498,"url":26,"identifiers":5499},"Harms J.C., 1966, Stratigraphic traps in a valley fill, western Nebraska, Bull. Am. Ass. Petrol. Geol., 50, 2119",{},{"id":26,"text":5501,"url":26,"identifiers":5502},"Inglis C.C., 1938, Relationship between meander belts, distance between meanders, width and discharge of rivers",{},{"id":26,"text":5504,"url":26,"identifiers":5505},"Jahns R.H., 1947, Geological features of the Connecticut Valley, Massachusetts, as related to recent floods, Wat. Supply Irrig. Pap. U.S. geol. Surv, 996",{},{"id":26,"text":5507,"url":26,"identifiers":5508},"Johnson N.L.&Kotz S.(1970)Continuous Univariate Distributions.1.Houghton Mifflin Company Boston .",{},{"id":26,"text":5510,"url":26,"identifiers":5511},"10.1130\u002F0091-7613(1974)2\u003C461:LEAODO>2.0.CO;2",{"doi":5510},{"id":26,"text":5513,"url":26,"identifiers":5514},"10.1111\u002Fj.1467-8470.1975.tb00068.x",{"doi":5513},{"id":26,"text":5516,"url":26,"identifiers":5517},"10.1111\u002Fj.1467-8306.1972.tb00872.x",{"doi":5516},{"id":26,"text":5519,"url":26,"identifiers":5520},"10.1017\u002FS0016756800036098",{"doi":5519},{"id":26,"text":1949,"url":26,"identifiers":5522},{"doi":1949},{"id":26,"text":1952,"url":26,"identifiers":5524},{},{"id":26,"text":5526,"url":26,"identifiers":5527},"Leopold L.B., 1964, Fluvial Processes in Geomorphology",{},{"id":26,"text":5529,"url":26,"identifiers":5530},"Lomnitz C., 1974, Global Tectonics and Earthquake Risk. 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Geol., 38, 96",{},{"id":26,"text":5560,"url":26,"identifiers":5561},"10.1111\u002Fj.1467-8306.1966.tb00541.x",{"doi":5560},{"id":26,"text":5563,"url":26,"identifiers":5564},"Nijman W., 1978, Fluvial Sedimentology, 487",{},{"id":26,"text":5566,"url":26,"identifiers":5567},"Pavoni N., 1975, Recent crustal movements, Tectonophysics, 29, 1",{},{"id":26,"text":5569,"url":26,"identifiers":5570},"Perrier R., 1974, Thickness changes in sedimentary layers during compaction history; methods for quantitative evaluation, Bull. Am. Ass. Petrol. Geol., 58, 507",{},{"id":26,"text":2153,"url":26,"identifiers":5572},{"doi":2153},{"id":26,"text":5574,"url":26,"identifiers":5575},"10.1029\u002FWR010i002p00263",{"doi":5574},{"id":26,"text":5577,"url":26,"identifiers":5578},"10.1007\u002F978-3-642-66146-4_5",{"doi":5577},{"id":26,"text":5580,"url":26,"identifiers":5581},"Puigdefabregas C., 1978, Fluvial Sedimentology, 469",{},{"id":26,"text":5583,"url":26,"identifiers":5584},"10.1007\u002FBF00875187",{"doi":5583},{"id":26,"text":5586,"url":26,"identifiers":5587},"10.1007\u002F978-3-642-66146-4_7",{"doi":5586},{"id":26,"text":5589,"url":26,"identifiers":5590},"Rieke H.H., 1974, Compaction of Argillaceous Sediments. 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Surv., 352, 71",{},{"id":26,"text":5609,"url":26,"identifiers":5610},"10.1051\u002Flhb\u002F1964044",{"doi":5609},{"id":26,"text":5612,"url":26,"identifiers":5613},"Sestini G., 1972, Ores in Sediments, 275",{},{"id":26,"text":5615,"url":26,"identifiers":5616},"Sigafoos R.S., 1964, Botanical evidence of floods and floodplain deposition, Prof. Pap. U.S. geol. Surv, 485",{},{"id":26,"text":5618,"url":26,"identifiers":5619},"Teisseyre A.K., 1977, Recent fluvial processes in drainage‐basins of the Upper Bobr and Strzegomka Rivers in the Central Sudetes, Geologia Sudetica, 12, 107",{},{"id":26,"text":5621,"url":26,"identifiers":5622},"Toebes G.H., 1967, Hydraulics of meandering streams with flood plains, J. Wat. Ways Harb. Div. Am. Soc. civ. Engrs, 93, 213",{},{"id":26,"text":5624,"url":26,"identifiers":5625},"Velikanov Z.M., 1970, Field investigations of the hydraulics of a floodplain during a high flood, Soviet Hydrology: Selected Papers, 5, 426",{},{"id":26,"text":5627,"url":26,"identifiers":5628},"10.1007\u002F978-3-642-66146-4_11",{"doi":5627},{"id":26,"text":5630,"url":26,"identifiers":5631},"Wolf K.H., 1976, Compaction of Coarse‐Grained Sediments, 69",{},{"id":26,"text":3487,"url":26,"identifiers":5633},{"doi":3487},{"id":26,"text":5635,"url":26,"identifiers":5636},"Wolman M.G., 1957, River flood plains: some observations on their formation, Prof. Pap. U.S. geol. Surv., 282, 87",{},{"id":26,"text":5638,"url":26,"identifiers":5639},"Yen C.L., 1973, Shape effects on resistance in floodplain channels, J. Hydraul. Div. Amer. Soc. civ. Engrs, 99, 219",{},{"id":5641,"createTime":5642,"updateTime":5642,"relativeEntities":5643,"slug":5644,"properties":5645,"entityType":859,"verifyStatus":25,"verifyTime":5642,"verifyNote":861,"syncStatus":28,"languages":5657,"translateLanguages":26,"viewCount":36,"primaryUrl":5658,"fullTextUrl":26,"authors":5659,"publicationType":902,"publisherRelationship":5716,"citationCount":5752,"citationInfo":5753,"publishDate":1531,"publishYear":1532,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":5755,"isForceReanalyzing":1431},"1d5d4073-5470-455d-be88-bd8d3b236af6","2024-10-01T02:56:25.945+00:00",[],"Spatial-and-temporal-distribution-of-diagenetic-alterations-in-siliciclastic-rocks-implications-for-mass-transfer-in-sedimentary-basins",{"mag":5646,"keywords":5648,"openalex":5649,"abstract":5651,"title":5653,"doi":5655},{"VOID":5647},"1849879787",{},{"VOID":5650},"W1849879787",{"EN":5652},"\u003Cjats:title>Summary\u003C\u002Fjats:title>\u003Cjats:p>The spatial and temporal distribution of diagenetic alterations in siliciclastic sequences is controlled by a complex array of interrelated parameters that prevail during eodiagenesis, mesodiagenesis and telodiagenesis. The spatial distribution of near‐surface eogenetic alteration is controlled by depositional facies, climate, detrital composition and relative changes in sea‐level. The most important eogenetic alterations in continental sediments include silicate dissolution and the formation of kaolinite, smectite, calcrete and dolocrete. In marine and transitional sediments, eogenetic alterations include the precipitation of carbonate, opal, microquartz, Fe‐silicates (glaucony, berthierine and nontronite), sulphides and zeolite. The eogenetic evolution of marine and transitional sediments can probably be developed within a predictable sequence stratigraphic context. Mesodiagenesis is strongly influenced by the induced eogenetic alterations, as well as by temperature, pressure and the composition of basinal brines. The residence time of sedimentary sequences under certain burial conditions is of key importance in determining the timing, extent and patterns of diagenetic modifications induced. The most important mesogenetic alterations include feldspar albitization, illitization and chloritization of smectite and kaolinite, dickitization of kaolinite, chemical compaction as well as quartz and carbonate cementation. Various aspects of deep‐burial mesodiagenesis are still poorly understood, such as: (i) whether reactions are accomplished by active fluid flow or by diffusion; (ii) the pattern and extent of mass transfer between mudrocks and sandstones; (iii) the role of hydrocarbon emplacement on sandstone diagenesis; and (iv) the importance and origin of fluids involved in the formation of secondary inter‐ and intragranular porosity during mesodiagenesis. Uplift and incursion of meteoric waters induce telogenetic alterations that include kaolinitization and carbonate‐cement dissolution down to depths of tens to a few hundred metres below the surface.\u003C\u002Fjats:p>",{"EN":5654},"Spatial and temporal distribution of diagenetic alterations in siliciclastic rocks: implications for mass transfer in sedimentary basins",{"VOID":5656},"10.1046\u002Fj.1365-3091.2000.00007.x",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1046\u002Fj.1365-3091.2000.00007.x",[5660,5682,5699],{"id":5661,"sortIndex":115,"researcher":26,"roles":5662,"affiliations":5663,"properties":5675},"a4d09b42-43d4-4c9a-a5a1-04f65c7f0245",[],[5664],{"id":5665,"sortIndex":36,"affiliation":5666,"properties":26},"12792898-c679-4eca-9960-0438414a6586",{"id":5667,"createTime":5668,"updateTime":5669,"relativeEntities":5670,"slug":5671,"properties":5672,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"bce12042-0398-40df-a171-993170b27f7e","2023-12-06T15:46:19.108+00:00","2024-10-15T20:58:51.305+00:00",[],"Department-of-Earth-Sciences-Uppsala-University-752-36-Uppsala-Sweden",{"title":5673},{"VI":5674},"Department of Earth Sciences, Uppsala University, 752 36 Uppsala, Sweden",{"openalex":5676,"orcid":5678,"title":5680},{"VOID":5677},"A5064080624",{"VOID":5679},"https:\u002F\u002Forcid.org\u002F0000-0003-4796-8177",{"EN":5681},"Marcelo Ketzer",{"id":5683,"sortIndex":36,"researcher":26,"roles":5684,"affiliations":5685,"properties":5692},"74bf61d0-f18a-42c5-8b5f-e707b4f4ef18",[],[5686],{"id":5687,"sortIndex":36,"affiliation":5688,"properties":26},"f56b90a3-28c2-4d32-b94b-6852d338b28c",{"id":5667,"createTime":5668,"updateTime":5669,"relativeEntities":5689,"slug":5671,"properties":5690,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":5691},{"VI":5674},{"openalex":5693,"orcid":5695,"title":5697},{"VOID":5694},"A5057027693",{"VOID":5696},"https:\u002F\u002Forcid.org\u002F0000-0002-8214-0896",{"EN":5698},"S. 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Miner., 83, 516, 10.2138\u002Fam-1998-5-611",{"doi":6321},"10.2138\u002Fam-1998-5-611",{"id":26,"text":6323,"url":26,"identifiers":6324},"10.1086\u002F629763",{"doi":6323},{"id":6326,"createTime":6327,"updateTime":6327,"relativeEntities":6328,"slug":6329,"properties":6330,"entityType":859,"verifyStatus":25,"verifyTime":6327,"verifyNote":861,"syncStatus":28,"languages":6342,"translateLanguages":26,"viewCount":36,"primaryUrl":6343,"fullTextUrl":26,"authors":6344,"publicationType":902,"publisherRelationship":6374,"citationCount":6412,"citationInfo":6413,"publishDate":6415,"publishYear":6416,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":6417,"isForceReanalyzing":1431},"d67ac0c8-9f51-44ac-9c8e-252a4bfdb264","2024-10-01T02:56:06.266+00:00",[],"Rhizoliths-in-terrestrial-carbonates-classification-recognition-genesis-and-significance",{"mag":6331,"keywords":6333,"openalex":6334,"abstract":6336,"title":6338,"doi":6340},{"VOID":6332},"2104772988",{},{"VOID":6335},"W2104772988",{"EN":6337},"\u003Cjats:title>ABSTRACT\u003C\u002Fjats:title>\u003Cjats:p>Rhizoliths are defined as organosedimentary structures resulting in the preservation of roots of higher plants, or remains thereof, in mineral matter. They are abundant and characteristic features of Quaternary terrestrial carbonates (calcretes and aeolianites) from coastal regions of the western Mediterranean. Field and petrographic observations indicate that five basic types of rhizoliths can be recognized: (1) root moulds, which are tubular voids that outline positions of former, now decayed roots; (2) root casts, which are sediment‐ and\u002For cement‐filled root moulds; (3) root tubules, which are cemented cylinders around root moulds; (4) rhizocretions \u003Cjats:italic>s.s.,\u003C\u002Fjats:italic> which are pedodiagenetic mineral accumulations (here low magnesian calcite) around living or dead plant roots; and (5) root petrifactions, which are mineral impregnations or mineral replacements of organic matter whereby anatomical features of roots have been preserved partially or totally. Apart from rhizoliths themselves, roots of higher plants are responsible for the formation of numerous and characteristic features of pedogenetically affected terrestrial carbonates. Plant roots are responsible for, or contribute to, the formation of alveolar textures, \u003Cjats:italic>in situ\u003C\u002Fjats:italic> brecciation (rhizobrecciation) textures, horizontal sheet cracks, vertically elongate glaebules (concretionary soil structures) and micritization (rhizomicritization) within terrestrial carbonates. Rhizoliths, together with the above features, are products of pedodiagenesis. 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