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Journal of Medicine and Pharmacy","Tạp chí Y Dược học Cần Thơ",{"EN":487,"VI":488},"\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">04\u002F10\u002F2015 Ministry of Information and Communications allowed Can Tho journal of medicine and pharmacy to operate (102 \u002FGP-BTTTT)\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">07\u002F16\u002F2015 Can Tho journal of medicine and pharmacy is internationally recognized: ISSN 2354-1210\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">In 2016, The journal has been included in the list of medical science journals by The State Council for professorship which is awarded a work score of 0-0.5 points for a published article.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Can Tho Journal of Medicine and Pharmacy welcome original works that haven’t been submitted or published in other medical journals. Posts must contain content related to one of the journal’s categories.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The content published\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The journal is divided into 3 categories:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Scientific research article: are valuable scientific works, which have been researched and accepted.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Overview of medicine, biology and pharmacy: serving the objective of continuing training in the fields of medicine, biology and pharmacy; to systematize classical and modern knowledge.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Update information on new knowledge about medicine, biology, pharmacy in the country and in the world.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Scope\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Publication and introduction of scientific research in the fields:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Medicine (internal medicine, surgery, pediatrics, obstetrics and gynecology, odonto-stomatology, laboratory, oncology, traditional medicine, nursing).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Biology (genetics, biotechnology).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Pharmacology (pharmaceutics, drug quality analysis-control, synthetic pharmaceutical chemistry, biochemistry, pharmacognosy, botany, clinical pharmacy).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- To enhance the quality of undergraduate, postgraduate education, scientifically researching and meet the necessary treatment in hospital.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Introducing the updated domestic and oversea information about science technology to promote scientific research and exchanging technology in local, other universities.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Exchanging pharmaceutical and medical information for social health developing in the Mekong Delta and Vietnam.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The object\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Postgraduate students, student of Can Tho University of Medicine and Pharmacy, scientists from schools, research institutes, hospitals, health centers, pharmaceutical companies of the Mekong Delta; 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. Danh sách bài báo theo số Tạp chí được in ấn và phát hành trong năm định kỳ được công bố chính thức trên website: https:\u002F\u002Ftapchi.ctump.edu.vn\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>",{"VOID":490},"wcQ1uqwAAAAJ","2023-05-30T08:17:21.868+00:00",[],[494],{"id":495,"createTime":28,"updateTime":28,"relativeEntities":496,"slug":28,"properties":497,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":507,"parentIds":508,"statistic":28},"6413896b-eca9-442b-a73f-182a58a0ce40",[],{"title":498,"address":501,"country":504,"abbreviation":505},{"EN":499,"VI":500},"Can Tho University of Medicine and Pharmacy","Trường Đại học Y Dược Cần Thơ",{"EN":502,"VI":503},"No 179, Nguyen Van Cu street, An Khanh ward, Ninh Kieu district, Can Tho city, Vietnam","Số 179, đường Nguyễn Văn Cừ, phường An Khánh, quận Ninh Kiều, thành phố Cần Thơ, Việt Nam",{"VOID":15},{"VOID":506},"ctump","http:\u002F\u002Fwww.ctump.edu.vn\u002F",[],[],"https:\u002F\u002Ftapchi.ctump.edu.vn\u002Findex.php\u002Fctump",{"impactFactor":32,"impactFactorByYear":512,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":514,"totalPublicationByYear":515,"totalCitation":520,"totalCitationByYear":521,"totalCitationPerPublication":108,"totalCitationPerPublicationByYear":523,"hindexLast5Year":45,"hindex":45},{"2022":513,"2023":111,"2024":106},0.01,1556,{"2020":47,"2021":516,"2022":517,"2023":518,"2024":519,"2025":122},57,306,801,358,161,{"2021":146,"2022":280,"2023":522},99,{"2021":524,"2022":318,"2023":104},0.23,{"impactFactor":28,"impactFactorByYear":28,"i10Index":123,"i10IndexLast5Year":123,"totalPublication":526,"totalPublicationByYear":527,"totalCitation":526,"totalCitationByYear":528,"totalCitationPerPublication":40,"totalCitationPerPublicationByYear":531,"hindexLast5Year":49,"hindex":49},476,{"0":205,"2019":123,"2021":139,"2022":459,"2023":451,"2024":357,"2025":49,"2026":48},{"2021":42,"2022":123,"2023":161,"2024":529,"2025":360,"2026":530},136,83,{"2021":105,"2022":513,"2023":532,"2024":127,"2025":533,"2026":534},0.62,25.43,13.83,{"id":536,"createTime":537,"updateTime":382,"relativeEntities":538,"slug":539,"properties":540,"entityType":25,"verifyStatus":26,"verifyTime":28,"verifyNote":28,"languages":552,"translateLanguages":28,"viewCount":133,"subjectFields":553,"manageAffiliations":554,"indexDatabases":555,"url":556,"thumbnailPath":557,"statistic":558,"gsStatistic":594,"type":55,"analyzePriority":28},"6984a56a-db70-403b-9cc4-4013e1ceaffa","2023-05-09T06:47:40.346+00:00",[],"T%E1%BA%A1p%20ch%C3%AD%20Nghi%C3%AAn%20c%E1%BB%A9u%20n%C6%B0%E1%BB%9Bc%20ngo%C3%A0i",{"country":541,"issn":542,"title":544,"introduce":547,"gsId":550},{"VOID":15},{"VOID":543},"25252445",{"EN":545,"VI":546},"VNU Journal of Foreign Studies","Tạp chí Nghiên cứu nước ngoài",{"EN":548,"VI":549},"{\"ops\":[{\"insert\":\"\\n\\nThe \\n\"},{\"attributes\":{\"italic\":true},\"insert\":\"VNU Journal of Science\"},{\"insert\":\"\\n was established in 1985 for the publication of national and international research papers in all fields of natural sciences and technology, social sciences and humanities. 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Palaeomagnetic and palaeofloral data indicate that early accretion (Vendian–Ordovician) took place when Baltica and Siberia were separated by a wide ocean. Island arcs and Precambrian microcontinents accreted to the active margins of the two continents or amalgamated in an oceanic setting (as in Kazakhstan) by roll-back and collision, forming a huge accretionary collage. The Palaeo-Asian Ocean closed in the Permian with formation of the Solonker suture. We evaluate contrasting tectonic models for the evolution of the orogenic belt. Current information provides little support for the main tenets of the one- or three-arc Kipchak model; current data suggest that an archipelago-type (Indonesian) model is more viable. Some diagnostic features of ridge–trench interaction are present in the Central Asian orogen (e.g. granites, adakites, boninites, near-trench magmatism, Alaskan-type mafic–ultramafic complexes, high-temperature metamorphic belts that prograde rapidly from low-grade belts, rhyolitic ash-fall tuffs). They offer a promising perspective for future investigations.\n          \u003C\u002Fjats:p>",{"EN":953},"Tectonic models for accretion of the Central Asian Orogenic Belt",{"VOID":955},"10.1144\u002F0016-76492006-022","PUBLICATION","2024-09-02T10:49:44.969+00:00","Auto Verify",[31],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002F0016-76492006-022",[962,979,998,1017,1036],{"id":963,"sortIndex":32,"researcher":28,"roles":964,"affiliations":965,"properties":974,"displayName":976,"givenName":28,"familyName":28},"78420795-32b1-459a-8075-c2ee36808e41",[],[966],{"id":967,"sortIndex":32,"affiliation":968,"properties":28},"4f671255-ad69-4519-aef6-f1b58690be7d",{"id":967,"createTime":28,"updateTime":28,"relativeEntities":969,"slug":28,"properties":970,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":973,"statistic":28},[],{"title":971},{"EN":972},"1Department of Geology, University of Leicester, Leicester LE1 7RH, UK (e-mail: brian.windley@btinternet.com)",[],{"title":975,"openalex":977},{"EN":976},"Brian F. 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Zaitsev Yu.A. (eds) 1976. Tectonic map of the Paleozoic folded belts of Kazakhstan and adjacent territories. Scale 1:1 500 000 . Aerogeologiya MinGeo of USSR Leningrad [in Russian].",{},{"id":28,"text":1118,"url":28,"identifiers":1119},"Alexeiev D.V. Cook H.E. Mikolaichuk A.V. & Djenchuraeva A.V. 2000. Upper Devonian through Lower Permian carbonates in the Middle Tian-Shan of Kyrgyzstan: new data on the evolution of passive margin carbonate platforms of the Kazakhstania paleocontinent. 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St. Peterburg University Publishing St. Peterburg [in Russian].",{},{"id":28,"text":1139,"url":28,"identifiers":1140},"Brown M. 1998. Ridge–trench interactions and high- T –low- P metamorphism with particular reference to the Cretaceous evolution of the Japanese Islands. In: Treloar P.J. O'Brien P.J. (eds) What Drives Metamorphism and Metamorphic Reactions? . Geological Society London Special Publications 138 137–169.",{"doi":1141},"10.1144\u002FGSL.SP.1996.138.01.09",{"id":28,"text":1143,"url":28,"identifiers":1144},"Bryan S.E. Riley T.R. Jerram D.A. Stephens C.J. & Leat P.T. 2002. Silicic volcanism: an undervalued component of large igneous provinces and volcanic rifted margins. In: Menzies M.A. Klemperer S.L. Ebinger C.J. & Baker J. (eds) Volcanic Rifted Margins . Geological Society of America Special Papers 362 99–120.",{"doi":1145},"10.1130\u002F0-8137-2362-0.97",{"id":28,"text":1147,"url":28,"identifiers":1148},"10.1144\u002Fjgs.158.3.445",{"doi":1147},{"id":28,"text":1150,"url":28,"identifiers":1151},"10.1016\u002FS0009-2541(02)00138-9",{"doi":1150},{"id":28,"text":1153,"url":28,"identifiers":1154},"10.1007\u002FBF02910304",{"doi":1153},{"id":28,"text":1156,"url":28,"identifiers":1157},"Buslov, M.M., Watanabe, T., Smirnova, L.V. , et al., 2003. Role of strike-slip faults in Paleozoic–Early Mesozoic tectonics and geodynamics of the Altai–Sayan and East Kazakhstan folded zone. Russian Geology and Geophysics, 44, 49–75.",{},{"id":28,"text":1159,"url":28,"identifiers":1160},"10.1016\u002FS1342-937X(05)71064-9",{"doi":1159},{"id":28,"text":1162,"url":28,"identifiers":1163},"10.1111\u002Fj.1747-5457.2003.tb00033.x",{"doi":1162},{"id":28,"text":1165,"url":28,"identifiers":1166},"10.1017\u002FS0016756801006100",{"doi":1165},{"id":28,"text":1168,"url":28,"identifiers":1169},"10.1016\u002Fj.earscirev.2005.04.001",{"doi":1168},{"id":28,"text":1171,"url":28,"identifiers":1172},"10.1016\u002Fj.tecto.2003.09.003",{"doi":1171},{"id":28,"text":1174,"url":28,"identifiers":1175},"Cook H.E. Zhemchuzhnikov V.G. Zempolich W.G. et al. 2002. Devonian and Carboniferous carbonate platform facies in the Bolshoi Karatau Southern Kazakhstan: outcrop analogs for coeval carbonate oil and gas fields in the North Caspian Basin Western Kazakhstan. In: Zempolich W.G. & Cook H.E. (eds) et al. Paleozoic Carbonates of the Commonwealth of the Independent States (CIS): Subsurface Reservoirs and Outcrop Analogs . SEPM Special Publications N74 81–122.",{"doi":1176},"10.2110\u002Fpec.02.74.0081",{"id":28,"text":1178,"url":28,"identifiers":1179},"10.2747\u002F0020-6814.47.3.270",{"doi":1178},{"id":28,"text":1181,"url":28,"identifiers":1182},"Daukeev S.Zh. Uzhkenov B.S. Miletenko N.V. et al. 2002. Atlas of the Lithology–Paleogeographical Structural Palinspastic and Geoenvironmental Maps of Central Eurasia . Scientific Research Institute of Natural Resources Almaty Kazakhstan.",{},{"id":28,"text":1184,"url":28,"identifiers":1185},"Degtyarev, K.Ye., 1999. Tectonic evolution of the Early Paleozoic active margin in Kazakhstan. Transactions of GIN, 513, 1–124 [in Russian].",{},{"id":28,"text":1187,"url":28,"identifiers":1188},"10.1144\u002F0016-764904-156",{"doi":1187},{"id":28,"text":1190,"url":28,"identifiers":1191},"Dobretsov, N.L., Simonov, V.A., Buslov, M.M. & Kurenkov, S.A. 1992. Oceanic and island arc ophiolites of Gorny Altai. Russian Geology and Geophysics, 12, 3–14.",{},{"id":28,"text":1193,"url":28,"identifiers":1194},"10.1016\u002FS1342-937X(05)70966-7",{"doi":1193},{"id":28,"text":1196,"url":28,"identifiers":1197},"10.1016\u002FS1367-9120(03)00132-9",{"doi":1196},{"id":28,"text":1199,"url":28,"identifiers":1200},"Dobretsov, N.L., Simonov, V.A., Buslov, M.M. & Kotlyarov, A.V. 2005. Magmatism and geodynamics of the Paleoasian ocean at the Vendian–Cambrian stage of its evolution. Russian Geology and Geophysics, 46, 952–967.",{},{"id":28,"text":1202,"url":28,"identifiers":1203},"Eganov, E.A., Sovetov, Yu.K. 1979. Karatau—a model for phosphorite deposition. Transactions of the Institute of Geology and Geophysics, Siberian Branch, USSR Academy of Sciences, 427, 1–192 [in Russian with English abstract].",{},{"id":28,"text":1205,"url":28,"identifiers":1206},"Fedorovskii, V.S., Khain, E.E., Vladimirov, A.G., Kargopolov, S.A., Gibsher, A.S. & Izokh, A.E. 1995. Tectonics, metamorphism, and magmatism of collisional zones of the Central Asian Caledonides. 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American Geophysical Union Geodynamic Series 21 .",{"doi":1496},"10.1029\u002FGD021",false,{"id":1499,"createTime":1500,"updateTime":1500,"relativeEntities":1501,"slug":1502,"properties":1503,"entityType":956,"verifyStatus":884,"verifyTime":1500,"verifyNote":1514,"languages":1515,"translateLanguages":28,"viewCount":32,"primaryUrl":1516,"fullTextUrl":28,"authors":1517,"publicationType":1053,"publisherRelationship":1529,"citationCount":1575,"citationInfo":1576,"publishDate":1581,"publishYear":1577,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1582,"openAccess":28,"references":1583,"isForceReanalyzing":1497},"a0464a74-a5f5-49cd-b30a-297b25ca856c","2024-09-19T22:11:39.921+00:00",[],"Fault-rocks-and-fault-mechanisms",{"openalex":1504,"mag":1506,"abstract":1508,"title":1510,"doi":1512},{"VOID":1505},"W2155128667",{"VOID":1507},"2155128667",{"EN":1509},"\u003Cjats:p>Physical factors likely to affect the genesis of the various fault rocks—frictional properties, temperature, effective stress normal to the fault and differential stress—are examined in relation to the energy budget of fault zones, the main velocity modes of faulting and the type of faulting, whether thrust, wrench, or normal. In a conceptual model of a major fault zone cutting crystalline quartzo-feldspathic crust, a zone of elastico-frictional (EF) behaviour generating random-fabric fault rocks (gouge—breccia—cataclasite series—pseudotachylyte) overlies a region where quasi-plastic (QP) processes of rock deformation operate in ductile shear zones with the production of mylonite series rocks possessing strong tectonite fabrics. In some cases, fault rocks developed by transient seismic faulting can be distinguished from those generated by slow aseismic shear. Random-fabric fault rocks may form as a result of seismic faulting within the ductile shear zones from time to time, but tend to be obliterated by continued shearing. Resistance to shear within the fault zone reaches a peak value (greatest for thrusts and least for normal faults) around the EF\u002FQP transition level, which for normal geothermal gradients and an adequate supply of water, occurs at depths of 10–15 km.\u003C\u002Fjats:p>",{"EN":1511},"Fault rocks and fault mechanisms",{"VOID":1513},"10.1144\u002Fgsjgs.133.3.0191","Author affiliation is blank",[31],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fgsjgs.133.3.0191",[1518],{"id":1519,"sortIndex":32,"researcher":28,"roles":1520,"affiliations":1521,"properties":1522,"displayName":1526,"givenName":28,"familyName":28},"ba2aa92a-43ae-4054-afaf-32c44d2a24c9",[],[],{"orcid":1523,"title":1525,"openalex":1527},{"VOID":1524},"https:\u002F\u002Forcid.org\u002F0000-0003-3509-7079",{"EN":1526},"Richard H. 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N.Maximum intensity of ground movements caused by faultingProc. 4th Wld. Conf Earthq Engng1969115471Santiago",{},{"id":28,"text":1588,"url":28,"identifiers":1589},"Anderson E. M.The dynamics of faulting19512nd edEdinburghOliver & Boyd",{},{"id":28,"text":1591,"url":28,"identifiers":1592},"10.1038\u002F254566a0",{"doi":1591},{"id":28,"text":1594,"url":28,"identifiers":1595},"10.1007\u002FBF00371429",{"doi":1594},{"id":28,"text":1597,"url":28,"identifiers":1598},"10.1016\u002F0024-4937(73)90052-2",{"doi":1597},{"id":28,"text":1600,"url":28,"identifiers":1601},"Berry F. A. F.High fluid potentials in the California Coast Ranges and their tectonic significanceBull Am Assoc Petrol Geol197357121949",{},{"id":28,"text":1603,"url":28,"identifiers":1604},"Birch F., Judd W. R.Megageological considerations in rock mechanicsState of stress in the earth’s crust1964New YorkElsevier5580",{},{"id":28,"text":1606,"url":28,"identifiers":1607},"10.1126\u002Fscience.153.3739.990",{"doi":1606},{"id":28,"text":1609,"url":28,"identifiers":1610},"10.1029\u002FJB075i026p04997",{"doi":1609},{"id":28,"text":1612,"url":28,"identifiers":1613},"10.1029\u002FJB074i015p03821",{"doi":1612},{"id":28,"text":1615,"url":28,"identifiers":1616},"10.1029\u002FJB073i014p04741",{"doi":1615},{"id":28,"text":1618,"url":28,"identifiers":1619},"10.1029\u002FJB073i018p06031",{"doi":1618},{"id":28,"text":1621,"url":28,"identifiers":1622},"10.1126\u002Fscience.164.3880.713",{"doi":1621},{"id":28,"text":1624,"url":28,"identifiers":1625},"Carslaw H. S., Jaeger J. C.Conduction of heat in solids19592nd edOxfordClarendon Press",{},{"id":28,"text":1627,"url":28,"identifiers":1628},"10.1144\u002Ftransed.18.1.79",{"doi":1627},{"id":28,"text":1630,"url":28,"identifiers":1631},"Christie J. M.The Moine Thrust in the Assynt region, north-west ScotlandUniv Calif Publs geol Sci196340345419",{},{"id":28,"text":1633,"url":28,"identifiers":1634},"10.1016\u002F0040-1951(70)90120-4",{"doi":1633},{"id":28,"text":1636,"url":28,"identifiers":1637},"Dieterich J. H., Donath F. A.Earthquake mechanisms and modellingAnnual review of earth and planetary science19742Palo Alto, CalifAnnual Reviews Inc275301",{},{"id":28,"text":1639,"url":28,"identifiers":1640},"10.1086\u002F627630",{"doi":1639},{"id":28,"text":1642,"url":28,"identifiers":1643},"10.1016\u002F0148-9062(72)90019-8",{"doi":1642},{"id":28,"text":1645,"url":28,"identifiers":1646},"10.1130\u002F0016-7606(1973)84\u003C2645:DFLIMR>2.0.CO;2",{"doi":1645},{"id":28,"text":1648,"url":28,"identifiers":1649},"10.1007\u002FBF01592900",{"doi":1648},{"id":28,"text":1651,"url":28,"identifiers":1652},"Francis P. W., Sibson R. H., Park R. G., Tarney J.The Outer Hebrides ThrustThe early Precambrian of Scotland and related rocks of Greenland1973Univ. of Keele95104",{},{"id":28,"text":1654,"url":28,"identifiers":1655},"Griffith A. A. 1924. Theory of rupture. Proc. 1st Int. Congr. appl. Mech. Delft 55–63.",{},{"id":28,"text":1657,"url":28,"identifiers":1658},"10.1111\u002Fj.1365-246X.1967.tb06218.x",{"doi":1657},{"id":28,"text":1660,"url":28,"identifiers":1661},"Griggs D. T., Baker D. W.The origin of deep-focus earthquakesProperties of matter under unusual conditions1969New YorkInterscience2342",{},{"id":28,"text":1663,"url":28,"identifiers":1664},"Griggs D. T., Handin J.Observations on fracture and an hypothesis for earthquakesMem geol Soc Am19607934764",{},{"id":28,"text":1666,"url":28,"identifiers":1667},"Heard H. C.Comparison of flow properties of rocks at crustal conditionsPhil. Trans. R. Soc. Lond1976A28317386",{"doi":1668},"10.1098\u002Frsta.1976.0077",{"id":28,"text":1670,"url":28,"identifiers":1671},"Higgins M. W.Cataclastic rocksProf. Pap. U.S. geol. Surv1971687",{},{"id":28,"text":1673,"url":28,"identifiers":1674},"Hsu K. J.Granulites and mylonites of the region about Cucamonga and San Antonio Canyons, San Gabriel Mountains, CaliforniaUniv Calif Publs, geol Sci195530223352",{},{"id":28,"text":1676,"url":28,"identifiers":1677},"10.1130\u002F0016-7606(1959)70[115:ROFPIM]2.0.CO;2",{"doi":1676},{"id":28,"text":1679,"url":28,"identifiers":1680},"Jaeger J. C., Cook N. G. W.Fundamentals of Rock Mechanics1969LondonMethuen",{},{"id":28,"text":1682,"url":28,"identifiers":1683},"10.1016\u002F0148-9062(74)91759-8",{"doi":1682},{"id":28,"text":1685,"url":28,"identifiers":1686},"10.1017\u002FS0016756800076019",{"doi":1685},{"id":28,"text":1688,"url":28,"identifiers":1689},"Jeffreys H.The Earth19594th edCambridge Univ. Press",{},{"id":28,"text":1691,"url":28,"identifiers":1692},"10.1144\u002Fgsjgs.131.4.0429",{"doi":1691},{"id":28,"text":1694,"url":28,"identifiers":1695},"Kerrich R. F. 1974. Aspects of pressure solution as a deformation mechanism. Thesis Ph.D. Univ. London (unpubl.).",{},{"id":28,"text":1697,"url":28,"identifiers":1698},"10.1029\u002FJB074i006p01702",{"doi":1697},{"id":28,"text":1700,"url":28,"identifiers":1701},"Lapworth C.The highland controversy in British geology; its causes, course and consequenceNature, Lond1885325589",{},{"id":28,"text":1703,"url":28,"identifiers":1704},"McClintock F. A. & Walsh J. B. 1962. Friction on Griffith cracks under pressure. Proc. 4th US. Natl. Congr. appl. Mech. 1015–21.",{},{"id":28,"text":1706,"url":28,"identifiers":1707},"10.1111\u002Fj.1365-246X.1972.tb06152.x",{"doi":1706},{"id":28,"text":1709,"url":28,"identifiers":1710},"10.1086\u002F623241",{"doi":1709},{"id":28,"text":1712,"url":28,"identifiers":1713},"10.1016\u002F0040-1951(72)90037-6",{"doi":1712},{"id":28,"text":1715,"url":28,"identifiers":1716},"Mogi K., Donath F. A.Rock fractureAnnual review of earth and planetary science19731Palo Alto. CalifAnnual Reviews Inc6384",{},{"id":28,"text":1718,"url":28,"identifiers":1719},"Orowan E.Mechanism of seismic faultingMem geol Soc Am19607932345",{},{"id":28,"text":1721,"url":28,"identifiers":1722},"Press F., Brace W. F.Earthquake predictionScience NT1966152157584",{},{"id":28,"text":1724,"url":28,"identifiers":1725},"Price N. J.Fault and joint development in brittle and semi-brittle rock1966LondonPergamon",{},{"id":28,"text":1727,"url":28,"identifiers":1728},"Price N. J., Hancock P. L.Development of fracture cleavage and kindred structuresInt geol Congr1972358492",{},{"id":28,"text":1730,"url":28,"identifiers":1731},"Pshennikov K. B.The energy balance in the focal region of a strong earthquakeIzv Acad Sci USSR, Phys Solid Earth1965101724",{},{"id":28,"text":1733,"url":28,"identifiers":1734},"10.1139\u002Fe70-078",{"doi":1733},{"id":28,"text":1736,"url":28,"identifiers":1737},"10.1080\u002F00288306.1964.10428124",{"doi":1736},{"id":28,"text":1739,"url":28,"identifiers":1740},"Reid H. F.The mechanics of the earthquakeIn, The California earthquake of April 18, 19061910Washington D.CCarnegie Institution of WashingtonReport of the State Investigation Commission, Part 2, 16–28",{},{"id":28,"text":1742,"url":28,"identifiers":1743},"Righter C. F.Elementary Seismology1958San FranciscoFreeman",{},{"id":28,"text":1745,"url":28,"identifiers":1746},"10.1016\u002F0148-9062(74)91111-5",{"doi":1745},{"id":28,"text":1748,"url":28,"identifiers":1749},"10.1016\u002F0040-1951(72)90003-0",{"doi":1748},{"id":28,"text":1751,"url":28,"identifiers":1752},"Rutter E. H.The kinetics of rock deformation by pressure solutionPhil. Trans. R. Soc. Lond1976A28320319",{"doi":1753},"10.1098\u002Frsta.1976.0079",{"id":28,"text":1755,"url":28,"identifiers":1756},"10.1029\u002FJB074i008p02049",{"doi":1755},{"id":28,"text":1755,"url":28,"identifiers":1758},{"doi":1755},{"id":28,"text":1760,"url":28,"identifiers":1761},"10.2475\u002Fajs.263.8.633",{"doi":1760},{"id":28,"text":1763,"url":28,"identifiers":1764},"10.1038\u002Fphysci243066a0",{"doi":1763},{"id":28,"text":1766,"url":28,"identifiers":1767},"10.1038\u002F249542a0",{"doi":1766},{"id":28,"text":1769,"url":28,"identifiers":1770},"10.1111\u002Fj.1365-246X.1975.tb06195.x",{"doi":1769},{"id":28,"text":1772,"url":28,"identifiers":1773},"Spry A.Metamorphic Textures1969LondonPergamon",{},{"id":28,"text":1775,"url":28,"identifiers":1776},"10.1016\u002F0040-1951(74)90119-X",{"doi":1775},{"id":28,"text":1778,"url":28,"identifiers":1779},"10.1029\u002FGL001i006p00261",{"doi":1778},{"id":28,"text":1781,"url":28,"identifiers":1782},"10.1038\u002F245298a0",{"doi":1781},{"id":28,"text":1784,"url":28,"identifiers":1785},"10.1016\u002FS0016-7878(18)80015-3",{"doi":1784},{"id":28,"text":1787,"url":28,"identifiers":1788},"Turner F.J.Metamorphic petrology1968New YorkMcGraw-Hill",{},{"id":28,"text":1790,"url":28,"identifiers":1791},"10.2475\u002Fajs.s5-29.174.473",{"doi":1790},{"id":28,"text":1793,"url":28,"identifiers":1794},"10.1007\u002FBF00550453",{"doi":1793},{"id":28,"text":1796,"url":28,"identifiers":1797},"White S.The effects of strain on the microstructures, fabrics and deformation mechanisms in quartzitePhil. Trans. R. Soc. Lond1976A2836986",{"doi":1798},"10.1098\u002Frsta.1976.0070",{"id":28,"text":1800,"url":28,"identifiers":1801},"10.1029\u002FTR037i004p00393",{"doi":1800},{"id":28,"text":1803,"url":28,"identifiers":1804},"10.1016\u002F0040-1951(73)90142-X",{"doi":1803},{"id":28,"text":1806,"url":28,"identifiers":1807},"10.1130\u002F0016-7606(1975)86\u003C968:POIQRM>2.0.CO;2",{"doi":1806},{"id":1809,"createTime":1810,"updateTime":1810,"relativeEntities":1811,"slug":1812,"properties":1813,"entityType":956,"verifyStatus":26,"verifyTime":1824,"verifyNote":958,"languages":1825,"translateLanguages":28,"viewCount":32,"primaryUrl":1826,"fullTextUrl":28,"authors":1827,"publicationType":1053,"publisherRelationship":1915,"citationCount":1961,"citationInfo":1962,"publishDate":1965,"publishYear":1963,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1966,"openAccess":28,"references":1967,"isForceReanalyzing":1497},"e5311793-9966-41a9-849c-71553674529c","2024-09-11T14:51:22.760+00:00",[],"Zircon-U-Pb-ages-for-the-Early-Cambrian-time-scale",{"openalex":1814,"mag":1816,"abstract":1818,"title":1820,"doi":1822},{"VOID":1815},"W2080522683",{"VOID":1817},"2080522683",{"EN":1819},"\u003Cjats:p>\n            Single zircons from two Early Cambrian volcanic horizons have been analysed using the SHRIMP ion microprobe. Full details of the analytical procedures and data reduction are given. Zircons from tuff within the Lie de Vin Formation, near Tiout, Morocco, show little spread in U-Pb age and have a mean value of 521 ± 7 Ma (2σ). Those from a bentonite within unit 5 of the Meishucun section near Kunming, southern China, show relatively dispersed U-Pb ages, revealing the presence of both detrital or xenocrystic grains as well as areas within grains that have lost radiogenic Pb. The main population has a mean age of 525 ± 7 Ma, but a mean\n            \u003Cjats:sup>207\u003C\u002Fjats:sup>\n            Pb\u002F\n            \u003Cjats:sup>206\u003C\u002Fjats:sup>\n            Pb age of 539 ± 34 Ma which is a maximum estimate for the bentonite age. These results conflict with previous Rb-Sr whole rock ages of\n            \u003Cjats:italic>c.\u003C\u002Fjats:italic>\n            580 Ma for overlying Cambrian shales at Meishucun, and\n            \u003Cjats:italic>c.\u003C\u002Fjats:italic>\n            570 Ma for Atdabanian shales from the E. Yangtse Gorges area.\n          \u003C\u002Fjats:p>",{"EN":1821},"Zircon U-Pb ages for the Early Cambrian time-scale",{"VOID":1823},"10.1144\u002Fgsjgs.149.2.0171","2024-09-11T14:51:22.759+00:00",[31],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fgsjgs.149.2.0171",[1828,1845,1864,1881,1900],{"id":1829,"sortIndex":32,"researcher":28,"roles":1830,"affiliations":1831,"properties":1840,"displayName":1842,"givenName":28,"familyName":28},"27cebf44-698f-4a4c-96f0-fcbd9e39c10e",[],[1832],{"id":1833,"sortIndex":32,"affiliation":1834,"properties":28},"597abe79-37e5-43d2-b638-ebcfcdaea8fe",{"id":1833,"createTime":28,"updateTime":28,"relativeEntities":1835,"slug":28,"properties":1836,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1839,"statistic":28},[],{"title":1837},{"VI":1838},"Yichang Institute of Geology and Mineral Resources, Yichang 443003, China",[],{"title":1841,"openalex":1843},{"EN":1842},"W. 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P., Andrews J. R., Badham J. P. N.Preliminary investigations of south Cornish mélangesProceedings of the Ussher Society197942628",{},{"id":28,"text":2239,"url":28,"identifiers":2240},"10.1086\u002F628815",{"doi":2239},{"id":28,"text":2242,"url":28,"identifiers":2243},"10.1016\u002F0037-0738(84)90065-4",{"doi":2242},{"id":28,"text":2245,"url":28,"identifiers":2246},"10.1016\u002F0009-2541(81)90089-9",{"doi":2245},{"id":28,"text":2248,"url":28,"identifiers":2249},"Blatt H., Middleton G., Murray R.Origin of Sedimentary Rocks19802nd ednNew JerseyPrentice-Hall Inc",{},{"id":28,"text":2251,"url":28,"identifiers":2252},"Bouma A. H.Sedimentology of some Flysch Deposits1962AmsterdamElsevier",{},{"id":28,"text":2254,"url":28,"identifiers":2255},"10.1017\u002FS0016756800042771",{"doi":2254},{"id":28,"text":2257,"url":28,"identifiers":2258},"10.1016\u002F0301-9268(77)90034-1",{"doi":2257},{"id":28,"text":2260,"url":28,"identifiers":2261},"10.1080\u002F00288306.1979.10422555",{"doi":2260},{"id":28,"text":2263,"url":28,"identifiers":2264},"10.1144\u002Fgsjgs.139.4.0465",{"doi":2263},{"id":28,"text":2266,"url":28,"identifiers":2267},"10.1130\u002F0016-7606(1970)81[2759:PAGOEP]2.0.CO;2",{"doi":2266},{"id":28,"text":2269,"url":28,"identifiers":2270},"Crook K. A. W.Lithogenesis and geotectonics: the significance of compositional variation in fiysch arenites (greywackes)Society of Economic Palaeontologists and Mineralogists, Special Publication19741930410",{},{"id":28,"text":2272,"url":28,"identifiers":2273},"10.1130\u002F0016-7606(1957)68[993:OOPM]2.0.CO;2",{"doi":2272},{"id":28,"text":2275,"url":28,"identifiers":2276},"10.1002\u002Fgj.3350030105",{"doi":2275},{"id":28,"text":2278,"url":28,"identifiers":2279},"10.1144\u002Fgsjgs.141.1.0003",{"doi":2278},{"id":28,"text":2281,"url":28,"identifiers":2282},"Dearman W. R.A general view of the structure of CornubiaProceedings of the Ussher Society1971222036",{},{"id":28,"text":2284,"url":28,"identifiers":2285},"Dearman W. R., Leveridge B. E., Turner R. G.Structural sequences and the ages of slates and phyllites from southwest EnglandProceedings of the Geological Society of London19691654415",{},{"id":28,"text":2287,"url":28,"identifiers":2288},"Dickinson W. R.Compositions of sandstones in circum-Pacific subduction complexes and fore-arc basinsBulletin of the American Association of Petroleum Geologists19826612137",{},{"id":28,"text":2290,"url":28,"identifiers":2291},"Dickinson W. R., Suczek C. A.Plate tectonics and sandstone compositionsBulletin of the American Association of Petroleum Geologists197963216482",{},{"id":28,"text":2293,"url":28,"identifiers":2294},"10.1130\u002F0091-7613(1980)8\u003C82:PSAPOS>2.0.CO;2",{"doi":2293},{"id":28,"text":2296,"url":28,"identifiers":2297},"10.1007\u002FBF02519780",{"doi":2296},{"id":28,"text":2299,"url":28,"identifiers":2300},"Edwards R. P.Aspects of trace metal and ore distribution in CornwallTransactions of the Institution of Mining & Metallurgy (Applied Earth Science)197685138390",{},{"id":28,"text":2302,"url":28,"identifiers":2303},"10.1007\u002FBF00371987",{"doi":2302},{"id":28,"text":2305,"url":28,"identifiers":2306},"10.1016\u002FB978-0-444-42148-7.50015-0",{"doi":2305},{"id":28,"text":2308,"url":28,"identifiers":2309},"Flett J. S.The geology of the MeneageMemoirs of the Geological Survey of Great Britain, Summary of Progress for 193219332114",{},{"id":28,"text":2311,"url":28,"identifiers":2312},"10.1016\u002F0016-7037(68)90101-4",{"doi":2311},{"id":28,"text":2314,"url":28,"identifiers":2315},"10.1144\u002Fgsjgs.139.4.0505",{"doi":2314},{"id":28,"text":2317,"url":28,"identifiers":2318},"10.1144\u002Fgsjgs.141.1.0061",{"doi":2317},{"id":28,"text":2320,"url":28,"identifiers":2321},"Floyd P. A. 1986. Geochemistry and provenance of basaltic clasts within volcaniclastic debris flows S Mariana Basin DSDP 585. In : Schlanger S. O. & Moberly R. (eds) Initial Reports DSDP 89 . Washington (US Printing Office) 449–58",{"doi":2322},"10.2973\u002Fdsdp.proc.89.115.1986",{"id":28,"text":2324,"url":28,"identifiers":2325},"10.1130\u002F0016-7606(1974)85\u003C379:DADAOS>2.0.CO;2",{"doi":2324},{"id":28,"text":2327,"url":28,"identifiers":2328},"Graham S. A., Ingersoll R. V., Dickinson W. R.Common provenance for lithic grains in Carboniferous sandstones from Ouachita Mountains and Blade Warrior BasinJournal of Sedimentary Petrology19764662032",{},{"id":28,"text":2330,"url":28,"identifiers":2331},"Halliday A. N., Mitchell J. G.K-Ar ages of basaltic dykes from the Lizard Complex (Abstr.)Proceedings of the Ussher Society1977424",{},{"id":28,"text":2333,"url":28,"identifiers":2334},"Henderson P.Inorganic Geochemistry1982OxfordPergamon Press",{},{"id":28,"text":2336,"url":28,"identifiers":2337},"10.1144\u002FGSL.JGS.1937.093.01-04.13",{"doi":2336},{"id":28,"text":2339,"url":28,"identifiers":2340},"10.1017\u002FS0016756800072320",{"doi":2339},{"id":28,"text":2342,"url":28,"identifiers":2343},"10.1144\u002Fgsjgs.143.1.0125",{"doi":2342},{"id":28,"text":2345,"url":28,"identifiers":2346},"House M. R., Selwood E. B., Hosking K. F. G., Shrimpron G. J.Palaeozoic palaeontology in Devon and CornwallPresent Views of Some Aspects of the Geology of Cornwall and Devon1964TruroRoyal Geological Society of Cornwall4586",{},{"id":28,"text":2348,"url":28,"identifiers":2349},"Ingersoll R. V., Suczek C. A.Petrology & provenance of Neogene sand from Nicobar and Bengal Fans, D.S.D.P. Sites 211 and 218Journal of Sedimentary Petrology197949121728",{},{"id":28,"text":2351,"url":28,"identifiers":2352},"10.1130\u002F0016-7606(1972)83[29:MATEAI]2.0.CO;2",{"doi":2351},{"id":28,"text":2354,"url":28,"identifiers":2355},"10.1139\u002Fe68-134",{"doi":2354},{"id":28,"text":2357,"url":28,"identifiers":2358},"10.1086\u002F628188",{"doi":2357},{"id":28,"text":2360,"url":28,"identifiers":2361},"10.1038\u002F282058a0",{"doi":2360},{"id":28,"text":2363,"url":28,"identifiers":2364},"Kuenan P. H., Migliorini C.Turbidity currents as a cause of graded beddingJournal of Geology19505890126",{},{"id":28,"text":2366,"url":28,"identifiers":2367},"10.1144\u002Fgsjgs.121.1.0339",{"doi":2366},{"id":28,"text":2369,"url":28,"identifiers":2370},"10.1144\u002Fgsjgs.139.4.0479",{"doi":2369},{"id":28,"text":2372,"url":28,"identifiers":2373},"10.1016\u002FS0016-7878(85)80006-7",{"doi":2372},{"id":28,"text":2375,"url":28,"identifiers":2376},"Levinson A. A.Introduction to Exploration Geochemistry1974IllinoisApplied Publishing Ltd",{},{"id":28,"text":2378,"url":28,"identifiers":2379},"Mack G. H.Exceptions to the relationship between plate tectonics and sandstone compositionJournal of Sedimentary Petrology19845421220",{},{"id":28,"text":2381,"url":28,"identifiers":2382},"Mason B., Moore C. B.Principles of Geochemistry1982New YorkWiley & Sons",{},{"id":28,"text":2384,"url":28,"identifiers":2385},"Maynard J. B., Valloni R., Yu H., Leggett J. K.Composition of modern deep sea sands from arc related basinsTrench-Forearc Geology198210LondonSpecial Publication of the Geological Society55161",{},{"id":28,"text":2387,"url":28,"identifiers":2388},"10.1016\u002F0016-7037(80)90232-X",{"doi":2387},{"id":28,"text":2390,"url":28,"identifiers":2391},"10.1016\u002F0016-7037(84)90345-4",{"doi":2390},{"id":28,"text":2393,"url":28,"identifiers":2394},"Mitchell A. H. G.Southwest England granites: magmatism and tin mineralization in a post-collision tectonic settingTransactions of the Insititution of Mining and Metallurgy (Applied Earth Science)197483957",{},{"id":28,"text":2396,"url":28,"identifiers":2397},"Mutti E., Ricci-Lucchi F.Le turbiditi dell'Appennino settentrionale: introduzione all'analisi di faciesMemorie della Societa Geologica Italiana19721116199",{},{"id":28,"text":2399,"url":28,"identifiers":2400},"10.1016\u002F0016-7037(76)90093-4",{"doi":2399},{"id":28,"text":2402,"url":28,"identifiers":2403},"10.1016\u002F0016-7037(69)90126-4",{"doi":2402},{"id":28,"text":2405,"url":28,"identifiers":2406},"10.1086\u002F628359",{"doi":2405},{"id":28,"text":2408,"url":28,"identifiers":2409},"Sadler P. M.An interpretation of new stratigraphic evidence from South CornwallProceedings of the Ussher Society1973353550",{},{"id":28,"text":2411,"url":28,"identifiers":2412},"10.1144\u002Fgsjgs.139.6.0691",{"doi":2411},{"id":28,"text":2414,"url":28,"identifiers":2415},"Sanderson D. J., Hutton D. H. W., Sanderson D. J.Structural variation across the northern margin of the Variscides in NW EuropeVariscan Tectonics of the North Atlantic Region198414LondonSpecial Publication of the Geological Society14965",{},{"id":28,"text":2417,"url":28,"identifiers":2418},"10.1130\u002F0091-7613(1975)3\u003C487:FMACCO>2.0.CO;2",{"doi":2417},{"id":28,"text":2420,"url":28,"identifiers":2421},"10.1086\u002F628416",{"doi":2420},{"id":28,"text":2423,"url":28,"identifiers":2424},"10.1016\u002F0016-7037(68)90050-1",{"doi":2423},{"id":28,"text":2426,"url":28,"identifiers":2427},"Stauffer P. H.Grain-flow deposits and their implications, Santa Ynez Mountains, CaliforniaJournal of Sedimentary Petrology196737487508",{},{"id":28,"text":2429,"url":28,"identifiers":2430},"Strong D. F., Stevens R. K., Malpas J. G., Badham J. P. N.A new tale for the LizardProceedings of the Ussher Society19753265(abstr.)",{},{"id":28,"text":2432,"url":28,"identifiers":2433},"Tarling D. H.Palaeomagnetic reconstructions and the Variscan orogenyProceedings of the Ussher Society1979423361",{},{"id":28,"text":2435,"url":28,"identifiers":2436},"10.1016\u002FS0024-4937(68)80008-8",{"doi":2435},{"id":28,"text":2438,"url":28,"identifiers":2439},"Taylor S. R., McLennan S. M.The composition and evolution of the continental crust: rare earth element evidence from sedimentary rocksPhilosophical Transactions of the Royal Society, London1981A30138199",{},{"id":28,"text":2441,"url":28,"identifiers":2442},"Taylor S. R., McLennan S. M.The Continental Crust: its Composition and Evolution1985OxfordBlackwell Scientific Publications",{},{"id":28,"text":2444,"url":28,"identifiers":2445},"10.1007\u002FBF00370873",{"doi":2444},{"id":28,"text":2447,"url":28,"identifiers":2448},"Turner R. E., Taylor R. T., Goode A. J. J., Owens B.Palynological evidence for the age of the Mylor slates, Mount Wellington, CornwallProceedings of the Ussher Society1979427483",{},{"id":28,"text":2450,"url":28,"identifiers":2451},"Walker R. G.Deep water sandstone facies and ancient submarine fans: models for exploration for stratigraphic trapsBulletin of the American Association of Petroleum Geologists19786293266",{},{"id":28,"text":2453,"url":28,"identifiers":2454},"Walker R. G., Wilker R. G.Turbidites and associated coarse clastic depositsFacies Models19791Geological Association of Canada91103Reprint Series",{},{"id":28,"text":2456,"url":28,"identifiers":2457},"10.1016\u002F0009-2541(81)90091-7",{"doi":2456},{"id":2459,"createTime":2460,"updateTime":2460,"relativeEntities":2461,"slug":2462,"properties":2463,"entityType":956,"verifyStatus":884,"verifyTime":2460,"verifyNote":1514,"languages":2474,"translateLanguages":28,"viewCount":32,"primaryUrl":2475,"fullTextUrl":28,"authors":2476,"publicationType":1053,"publisherRelationship":2503,"citationCount":2549,"citationInfo":2550,"publishDate":2553,"publishYear":2551,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":2554,"openAccess":28,"references":2555,"isForceReanalyzing":1497},"54bbf954-5345-4a02-bafc-4bbb2fc2e7c0","2024-09-05T19:42:55.968+00:00",[],"Seismic-pumping-a-hydrothermal-fluid-transport-mechanism",{"openalex":2464,"mag":2466,"abstract":2468,"title":2470,"doi":2472},{"VOID":2465},"W2028299312",{"VOID":2467},"2028299312",{"EN":2469},"\u003Cjats:p>A consequence of the dilatancy\u002Ffluid-diffusion mechanism for shallow earthquakes is that considerable volumes of fluid are rapidly redistributed in the crust following seismic faulting. This is borne out by the outpourings of warm groundwater which have been observed along fault traces following some moderate (M5–M7) earthquakes. The quantities of fluid involved are such that significant hydrothermal mineralisation may result from each seismically induced fluid pulse, and the mechanism provides an explanation for the textures of hydrothermal vein deposits associated with ancient faults, which almost invariably indicate that mineralisation was episodic.\u003C\u002Fjats:p>",{"EN":2471},"Seismic pumping—a hydrothermal fluid transport mechanism",{"VOID":2473},"10.1144\u002Fgsjgs.131.6.0653",[31],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fgsjgs.131.6.0653",[2477,2485,2494],{"id":2478,"sortIndex":32,"researcher":28,"roles":2479,"affiliations":2480,"properties":2481,"displayName":1526,"givenName":28,"familyName":28},"1267a3a9-1dc5-47cb-9fc8-9022bd40ab62",[],[],{"orcid":2482,"title":2483,"openalex":2484},{"VOID":1524},{"EN":1526},{"VOID":1528},{"id":2486,"sortIndex":40,"researcher":28,"roles":2487,"affiliations":2488,"properties":2489,"displayName":2491,"givenName":28,"familyName":28},"c2cdafed-4b5f-431f-9bb7-30b760a7b4ff",[],[],{"title":2490,"openalex":2492},{"EN":2491},"J. Mc. M. MOORE",{"VOID":2493},"A5103456674",{"id":2495,"sortIndex":123,"researcher":28,"roles":2496,"affiliations":2497,"properties":2498,"displayName":2500,"givenName":28,"familyName":28},"a8f5cc40-2073-4d65-9b49-4c7778ba7ed8",[],[],{"title":2499,"openalex":2501},{"EN":2500},"Andrew H. Rankin",{"VOID":2502},"A5015097681",{"url":28,"publisher":2504,"properties":2542},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":2505,"slug":872,"properties":2506,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":2511,"manageAffiliations":2516,"indexDatabases":2527,"url":935,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":2507,"eissn":2508,"issn":2509,"title":2510},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[2512],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":2513,"label":2514,"description":2515,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[2517,2522],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":2518,"slug":28,"properties":2519,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2521,"statistic":28},[],{"title":2520},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":2523,"slug":28,"properties":2524,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2526,"statistic":28},[],{"title":2525},{"EN":905},[],[2528,2535],{"id":924,"indexDatabase":2529,"url":930,"indexYears":931,"academicFieldIds":2534,"indexDatabaseRanking":934},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":2530,"label":2531,"description":2532,"key":781,"publicationTags":2533,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[933],{"id":909,"indexDatabase":2536,"url":921,"indexYears":28,"academicFieldIds":2541,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":2537,"label":2538,"description":2539,"key":918,"publicationTags":2540,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[816],{"issue":2543,"pages":2545,"volume":2547},{"VOID":2544},"6",{"VOID":2546},"653-659",{"VOID":2548},"131",654,{"total":2549,"publishYear":2551,"statisticByYear":2552},1975,{"2012":130,"2013":129,"2014":131,"2015":323,"2016":134,"2017":134,"2018":199,"2019":140,"2020":150,"2021":69,"2022":69,"2023":128,"2024":199},"1975-11-01",[920,934],[2556,2559,2562,2565,2568,2571,2574,2577,2580,2583,2586,2590,2593,2596,2598,2601,2604,2607],{"id":28,"text":2557,"url":28,"identifiers":2558},"Bateman A. M.Economic mineral deposits19502nd edNew YorkWiley916",{},{"id":28,"text":2560,"url":28,"identifiers":2561},"Bignell R. D.Timing, distribution and origin of submarine mineralization in the Red SeaTrans. Inst. Mining Metallurgy1975B84B16",{},{"id":28,"text":2563,"url":28,"identifiers":2564},"Briggs R. C., Troxell H. C.Effect of Arvin-Techapi earthquake on spring and stream flowEarthquakes in Kern County, California, during 1952 Calif Div Mines Bull19551718198",{},{"id":28,"text":2566,"url":28,"identifiers":2567},"10.1029\u002FRG003i004p00485",{"doi":2566},{"id":28,"text":2569,"url":28,"identifiers":2570},"10.1016\u002F0031-9201(72)90008-8",{"doi":2569},{"id":28,"text":2572,"url":28,"identifiers":2573},"Hagiwara T., Iwate T.Summary of the seismographic observation of Matsushiro swarm earthquakesBull Earthquake Res Inst Tokyo Univ19684665161",{},{"id":28,"text":2575,"url":28,"identifiers":2576},"Holland H. D., Barnes H. L.Gangue minerals in hydrothermal depositsGeochemistry of hydrothermal ore deposits1967New YorkHolt, Rinehart & Winston Inc382436",{},{"id":28,"text":2578,"url":28,"identifiers":2579},"Kasahara K.The source region of the Matsushiro swarm earthquakesBull Earthquake Res Inst Tokyo Univ197048581602",{},{"id":28,"text":2581,"url":28,"identifiers":2582},"10.1785\u002FBSSA0620051217",{"doi":2581},{"id":28,"text":2584,"url":28,"identifiers":2585},"10.1130\u002F0091-7613(1974)2\u003C217:MJESCO>2.0.CO;2",{"doi":2584},{"id":28,"text":2587,"url":28,"identifiers":2588},"Roedder E 1972. Composition of fluid inclusions. U.S. geol. Survey Prof. Paper 440-JJ",{"doi":2589},"10.3133\u002Fpp440JJ",{"id":28,"text":2591,"url":28,"identifiers":2592},"10.1029\u002FJB079i014p02132",{"doi":2591},{"id":28,"text":2594,"url":28,"identifiers":2595},"10.1126\u002Fscience.181.4102.803",{"doi":2594},{"id":28,"text":1766,"url":28,"identifiers":2597},{"doi":1766},{"id":28,"text":2599,"url":28,"identifiers":2600},"Tchalenko J. S.The Kashmar (Turshiz) 1903 and Torbat-e Heidariyeh (South) 1923 earthquakes in Central Khorassan (Iran)Ann Geofis1973262940",{},{"id":28,"text":2602,"url":28,"identifiers":2603},"Tsuneishi Y., Nakamura K.Faulting associated with the Matsushiro swarm earthquakesBull Earthquake Res Inst Tokyo Univ1970482951",{},{"id":28,"text":2605,"url":28,"identifiers":2606},"10.1126\u002Fscience.180.4086.632",{"doi":2605},{"id":28,"text":2608,"url":28,"identifiers":2609},"10.1029\u002FJB073i014p04681",{"doi":2608},{"id":2611,"createTime":2612,"updateTime":2612,"relativeEntities":2613,"slug":2614,"properties":2615,"entityType":956,"verifyStatus":884,"verifyTime":2612,"verifyNote":1514,"languages":2626,"translateLanguages":28,"viewCount":32,"primaryUrl":2627,"fullTextUrl":28,"authors":2628,"publicationType":1053,"publisherRelationship":2638,"citationCount":2683,"citationInfo":2684,"publishDate":2687,"publishYear":2685,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":2688,"openAccess":28,"references":2689,"isForceReanalyzing":1497},"ec7c436a-1c3b-48c3-91ab-20fa3b76dcdc","2024-09-30T19:30:37.163+00:00",[],"The-petrological-evolution-of-island-arc-systems",{"openalex":2616,"mag":2618,"abstract":2620,"title":2622,"doi":2624},{"VOID":2617},"W2018845940",{"VOID":2619},"2018845940",{"EN":2621},"\u003Cjats:p>The most important petrological problem relating to the development of island arc systems is the origin of the basalt-andesite-dacite-rhyolite volcanic suite. Characteristics of the suite are reviewed. They include distribution of active volcanoes relative to Benioff zones, chemical composition and fractionation trends of magmas, the evolutionary development of island arcs in time, often comprising an earlier tholeiitic stage followed by a later calcalkaline stage, and the trend of magmas to become richer in potassium and other incompatible elements, the greater the height of the volcano above the Benioff zone.\u003C\u002Fjats:p>\n          \u003Cjats:p>\n            Recent researches in experimental petrology suggest three fractionation controls which might be responsible for various characteristics of the suite; amphibole-controlled fractionation, eclogite-controlled fractionation and direct partial melting of mantle pyrolite under conditions of high water vapour pressure. The operation of these processes is reviewed. Amphibole-controlled fractionation is limited to depths smaller than 100 km and causes a calcalkaline trend among residual liquids but with little change in K\u002FNa and rare earth element abundances. Eclogite-controlled fractionation likewise causes a calcalkaline trend but is accompanied by increase of K\u002FNa ratios and fractionation of the rare earth elements. This process probably occurs in the 100–150 km depth interval. Partial melting of the mantle under high P\n            \u003Cjats:sub>\n              H\n              \u003Cjats:sub>2\u003C\u002Fjats:sub>\n              O\n            \u003C\u002Fjats:sub>\n            is shown to cause the formation of basaltic magmas in the depth interval, 70–100 km. Upon rising, these magmas fractionate towards basaltic andesite and andesite compositions via the crystallization mainly of olivine. Resulting liquids display a tholeiitic differentiation trend.\n          \u003C\u002Fjats:p>\n          \u003Cjats:p>\n            A model for the operation of these processes in the island arc environment is proposed. Amphibolite in the subducted oceanic crust becomes dehydrated at depths of 70–100 km under subsolidus conditions. The water produced causes partial melting to occur in the pyrolite wedge above the Benioff zone. Magmas thus produced differentiate under high P\n            \u003Cjats:sub>\n              H\n              \u003Cjats:sub>2\u003C\u002Fjats:sub>\n              O\n            \u003C\u002Fjats:sub>\n            to produce the early tholeiite stage of arc development. As the oceanic crust is sub-ducted to depths of 100–150 km, a high P\n            \u003Cjats:sub>\n              H\n              \u003Cjats:sub>2\u003C\u002Fjats:sub>\n              O\n            \u003C\u002Fjats:sub>\n            is maintained by the dehydration of serpentinite and derivative high pressure hydrated magnesium silicates. Partial melting of the quartz eclogite oceanic crust produces rhyodacite magmas. These react with overlying mantle pyrolite to form pyroxenite. Diapirs of pyroxenite rise upwards from the Benioff zone, partially melting to form magmas which fractionate by eclogite crystallization (80–150 km) and amphibole crystallization (30–100 km) thereby producing the calcalkaline phase of arc development.\n          \u003C\u002Fjats:p>\n          \u003Cjats:p>The residual, refractory eclogite and peridotite in the lithosphere plates which sink below about 150 km have become irreversibly differentiated and never again are able to participate in the formation of basaltic magmas at mid-oceanic ridges. The complementary differentiate is, ultimately, the continental crust, which grows through time by the accretion of island arcs and by the addition of the andesitic volcanic suite, derived as discussed above. It is estimated that about 30–60% of the volume of the mantle has passed through this process of irreversible differentiation.\u003C\u002Fjats:p>",{"EN":2623},"The petrological evolution of island arc systems",{"VOID":2625},"10.1144\u002Fgsjgs.130.3.0183",[31],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fgsjgs.130.3.0183",[2629],{"id":2630,"sortIndex":32,"researcher":28,"roles":2631,"affiliations":2632,"properties":2633,"displayName":2635,"givenName":28,"familyName":28},"0efa6974-2663-43ab-a925-b2220b727852",[],[],{"title":2634,"openalex":2636},{"EN":2635},"A. E. Ringwood",{"VOID":2637},"A5045652400",{"url":28,"publisher":2639,"properties":2677},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":2640,"slug":872,"properties":2641,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":2646,"manageAffiliations":2651,"indexDatabases":2662,"url":935,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":2642,"eissn":2643,"issn":2644,"title":2645},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[2647],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":2648,"label":2649,"description":2650,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[2652,2657],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":2653,"slug":28,"properties":2654,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2656,"statistic":28},[],{"title":2655},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":2658,"slug":28,"properties":2659,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2661,"statistic":28},[],{"title":2660},{"EN":905},[],[2663,2670],{"id":924,"indexDatabase":2664,"url":930,"indexYears":931,"academicFieldIds":2669,"indexDatabaseRanking":934},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":2665,"label":2666,"description":2667,"key":781,"publicationTags":2668,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[933],{"id":909,"indexDatabase":2671,"url":921,"indexYears":28,"academicFieldIds":2676,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":2672,"label":2673,"description":2674,"key":918,"publicationTags":2675,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[816],{"issue":2678,"pages":2679,"volume":2681},{"VOID":1570},{"VOID":2680},"183-204",{"VOID":2682},"130",497,{"total":2683,"publishYear":2685,"statisticByYear":2686},1974,{"2012":42,"2013":328,"2014":146,"2015":205,"2016":48,"2017":145,"2018":48,"2019":357,"2020":323,"2021":126,"2022":45,"2023":357,"2024":42},"1974-05-01",[920,934],[2690,2693,2696,2699,2702,2705,2708,2711,2714,2717,2720,2723,2726,2730,2733,2736,2739,2742,2745,2748,2751,2754,2757,2760,2763,2766,2769,2772,2775,2778,2781,2784,2787,2790,2793,2796,2799,2802,2805,2808,2811,2814,2817,2820,2823,2826,2829,2832,2835,2839],{"id":28,"text":2691,"url":28,"identifiers":2692},"10.1007\u002FBF02596591",{"doi":2691},{"id":28,"text":2694,"url":28,"identifiers":2695},"10.1029\u002FJB076i035p08493",{"doi":2694},{"id":28,"text":2697,"url":28,"identifiers":2698},"10.1130\u002F0016-7606(1958)69[483:DOTM]2.0.CO;2",{"doi":2697},{"id":28,"text":2700,"url":28,"identifiers":2701},"Brown G. M., Schairer J. F.Melting relations of some calcalkaline volcanic rocksCarnegie Inst Washington Yearbook196866460467",{},{"id":28,"text":2703,"url":28,"identifiers":2704},"10.1038\u002F226928a0",{"doi":2703},{"id":28,"text":2706,"url":28,"identifiers":2707},"10.1093\u002Fpetrology\u002F5.3.435",{"doi":2706},{"id":28,"text":2709,"url":28,"identifiers":2710},"Daly R. A.Igneous Rocks and the Depths of the Earth1933New YorkMcGraw-Hill",{},{"id":28,"text":2712,"url":28,"identifiers":2713},"10.1130\u002F0016-7606(1962)73[1241:PSOGAV]2.0.CO;2",{"doi":2712},{"id":28,"text":2715,"url":28,"identifiers":2716},"10.1029\u002FJB073i006p02261",{"doi":2715},{"id":28,"text":2718,"url":28,"identifiers":2719},"10.1126\u002Fscience.157.3790.801",{"doi":2718},{"id":28,"text":2721,"url":28,"identifiers":2722},"10.1126\u002Fscience.174.4007.400",{"doi":2721},{"id":28,"text":2724,"url":28,"identifiers":2725},"10.1126\u002Fscience.140.3563.143",{"doi":2724},{"id":28,"text":2727,"url":28,"identifiers":2728},"Ewart A. Bryan W. B. Gill J.Mineralogy and geochemistry of the younger volcanic islands of Tonga1973S.W. PacificIn press",{"doi":2729},"10.1093\u002Fpetrology\u002F14.3.429",{"id":28,"text":2731,"url":28,"identifiers":2732},"10.1029\u002FJZ065i004p01287",{"doi":2731},{"id":28,"text":2734,"url":28,"identifiers":2735},"10.1007\u002FBF00385777",{"doi":2734},{"id":28,"text":2737,"url":28,"identifiers":2738},"Gorshkov G. S.Petrochemical features of volcanism in relation to the types of the earth's crustAm Geophys U Monograph19626110115",{},{"id":28,"text":2740,"url":28,"identifiers":2741},"10.1016\u002F0012-821X(73)90176-3",{"doi":2740},{"id":28,"text":2743,"url":28,"identifiers":2744},"10.1007\u002FBF00372052",{"doi":2743},{"id":28,"text":2746,"url":28,"identifiers":2747},"10.1007\u002FBF00373770",{"doi":2746},{"id":28,"text":2749,"url":28,"identifiers":2750},"10.1007\u002FBF00371806",{"doi":2749},{"id":28,"text":2752,"url":28,"identifiers":2753},"10.1080\u002F14400957208527881",{"doi":2752},{"id":28,"text":2755,"url":28,"identifiers":2756},"Griggs D. T., Robertson E. C.The sinking lithosphere and the focal mechanism of deep earthquakesThe Nature of the Solid Earth1972N.YMcGraw-Hill361384",{},{"id":28,"text":2758,"url":28,"identifiers":2759},"10.1126\u002Fscience.167.3920.980",{"doi":2758},{"id":28,"text":2761,"url":28,"identifiers":2762},"10.1093\u002Fpetrology\u002F13.1.1",{"doi":2761},{"id":28,"text":2764,"url":28,"identifiers":2765},"10.1029\u002FJZ067i013p05315",{"doi":2764},{"id":28,"text":2767,"url":28,"identifiers":2768},"10.1016\u002F0012-821X(70)90018-X",{"doi":2767},{"id":28,"text":2770,"url":28,"identifiers":2771},"10.1016\u002F0040-1951(69)90099-7",{"doi":2770},{"id":28,"text":2773,"url":28,"identifiers":2774},"10.1130\u002F0016-7606(1950)61[957:POHVAT]2.0.CO;2",{"doi":2773},{"id":28,"text":2776,"url":28,"identifiers":2777},"10.1093\u002Fpetrology\u002F13.2.311",{"doi":2776},{"id":28,"text":2779,"url":28,"identifiers":2780},"10.1016\u002F0012-821X(72)90073-8",{"doi":2779},{"id":28,"text":2782,"url":28,"identifiers":2783},"Kushiro I., Yoder H. S.Melting of forsterite and enstatite at high pressures under hydrous conditionsCarnegie Inst Washington Yearbook196967153158",{},{"id":28,"text":2785,"url":28,"identifiers":2786},"10.1038\u002F2191240a0",{"doi":2785},{"id":28,"text":2788,"url":28,"identifiers":2789},"Nicholls I. A. 1973. Manuscript",{},{"id":28,"text":2791,"url":28,"identifiers":2792},"10.1016\u002F0012-821X(72)90282-8",{"doi":2791},{"id":28,"text":2794,"url":28,"identifiers":2795},"10.1086\u002F627871",{"doi":2794},{"id":28,"text":2797,"url":28,"identifiers":2798},"O'Hara M. J.Melting of garnet peridotite and eclogite at 30 kilobarsCarnegie Inst Washington Yearbook1963627177",{},{"id":28,"text":2800,"url":28,"identifiers":2801},"10.1007\u002FBF00373068",{"doi":2800},{"id":28,"text":2803,"url":28,"identifiers":2804},"10.1130\u002F0016-7606(1970)81[1665:TSOIA]2.0.CO;2",{"doi":2803},{"id":28,"text":2806,"url":28,"identifiers":2807},"Ringwood A. E.Composition and evolution of the upper mantleAm Geophys U Monograph196913117",{},{"id":28,"text":2809,"url":28,"identifiers":2810},"10.1016\u002F0012-821X(72)90012-X",{"doi":2809},{"id":28,"text":2812,"url":28,"identifiers":2813},"Ringwood A. E.Composition and Petrology of the Earth's Mantle1973New YorkMcGraw-HillIn press",{},{"id":28,"text":2815,"url":28,"identifiers":2816},"10.1016\u002F0040-1951(66)90009-6",{"doi":2815},{"id":28,"text":2818,"url":28,"identifiers":2819},"Ringwood A. E., Major A.High pressure reconnaissance investigations in the system Mg2SiO4–MgO–H2O. Earth PlanetSci Letters19672130133",{},{"id":28,"text":2821,"url":28,"identifiers":2822},"Sclar C. B., Carrison L. C., Stewart O. M.High pressure synthesis of a new hydroxylated pyroxene in the system MgO–SiO2–H2O (abstract)Trans Am Geophys U196748226",{},{"id":28,"text":2824,"url":28,"identifiers":2825},"10.1016\u002F0040-1951(67)90056-X",{"doi":2824},{"id":28,"text":2827,"url":28,"identifiers":2828},"Taylor S. R.Trace elements chemistry of andesites and associated calcalkaline rocksBull Dept Geol Min Resources, State of Oregon1969654363",{},{"id":28,"text":2830,"url":28,"identifiers":2831},"Wager L. R., Deer W. A.Geological investigations in East Greenland III. The petrology of the Skaergaard Intrusion, Kangerdlugssaq, East GreenlandMed øm Grønland19391051352",{},{"id":28,"text":2833,"url":28,"identifiers":2834},"Wilson J. T., Kuiper G. P.The development and structure of the crustThe Earth as a Planet1954Chicago Univ. Press138214",{},{"id":28,"text":2836,"url":28,"identifiers":2837},"Yamamoto K. Akimoto S.High pressure and high temperature investigations in the system MgO–SiO 2 –H 2 O1973In press",{"doi":2838},"10.1016\u002F0022-4596(74)90073-5",{"id":28,"text":2840,"url":28,"identifiers":2841},"10.1093\u002Fpetrology\u002F3.3.342",{"doi":2840},{"id":2843,"createTime":2844,"updateTime":2844,"relativeEntities":2845,"slug":2846,"properties":2847,"entityType":956,"verifyStatus":26,"verifyTime":2844,"verifyNote":958,"languages":2858,"translateLanguages":28,"viewCount":32,"primaryUrl":2859,"fullTextUrl":28,"authors":2860,"publicationType":1053,"publisherRelationship":2899,"citationCount":2944,"citationInfo":2945,"publishDate":2948,"publishYear":2946,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":2949,"openAccess":28,"references":2950,"isForceReanalyzing":1497},"9c9f995d-9184-4411-ae56-0cc54c2e7cb7","2025-02-06T20:51:24.329+00:00",[],"Volcanism-CO-sub-2-sub-and-palaeoclimate-a-Late-Jurassic-Early-Cretaceous-carbon-and-oxygen-isotope-record",{"openalex":2848,"mag":2850,"abstract":2852,"title":2854,"doi":2856},{"VOID":2849},"W1985005684",{"VOID":2851},"1985005684",{"EN":2853},"\u003Cjats:p>\n            A composite Tethyan Late Jurassic–Early Cretaceous carbon and oxygen isotope curve is presented. C-isotope data provide information on the evolution and perturbation of the global carbon cycle. O-isotope data are used as a palaeotemperature proxy in combination with palaeontological information. The resulting trends in climate and in palaeoceanography are compared with biocalcification trends and oceanographic conditions favouring or inhibiting biocalcification. Positive C-isotope anomalies in the Valanginian and Aptian correlate with episodes of increased volcanic activity regarded as a source of excess atmospheric carbon dioxide. A major warming pulse accompanies the Aptian but not the Valanginian C-isotope event. The observed change in Early Aptian temperatures could have triggered the destabilization of sedimentary gas hydrates and the sudden release of methane to the biosphere as recorded as a distinct negative carbon isotope pulse preceding the positive excursion. Both C-isotope anomalies are accompanied by biocalcification crises that may have been triggered by\n            \u003Cjats:italic>p\u003C\u002Fjats:italic>\n            CO\n            \u003Cjats:sub>2\u003C\u002Fjats:sub>\n            -induced changes in climate and in surface water chemistry. Elevated nutrient levels in river-influenced coastal waters and in upwelling regions further weakened marine calcification. These conditions contrast with ‘normal’ trophic conditions prevailing in the latest Jurassic and favouring biocalcification. The C- and O-isotope curves record a stable mode of carbon cycling and stable temperatures. We conclude that biocalcification is mostly triggered (and inhibited) by CO\n            \u003Cjats:sub>2\u003C\u002Fjats:sub>\n            conditions in the atmosphere–ocean system.\n          \u003C\u002Fjats:p>",{"EN":2855},"Volcanism, CO\n            \u003Csub>2\u003C\u002Fsub>\n            and palaeoclimate: a Late Jurassic–Early Cretaceous carbon and oxygen isotope record",{"VOID":2857},"10.1144\u002F0016-764903-087",[31],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002F0016-764903-087",[2861,2880],{"id":2862,"sortIndex":32,"researcher":28,"roles":2863,"affiliations":2864,"properties":2873,"displayName":2877,"givenName":28,"familyName":28},"0ce496e4-9996-4822-866a-76a93e131df1",[],[2865],{"id":2866,"sortIndex":32,"affiliation":2867,"properties":28},"6c47c946-5c4f-436e-b55c-37f3a27db536",{"id":2866,"createTime":28,"updateTime":28,"relativeEntities":2868,"slug":28,"properties":2869,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2872,"statistic":28},[],{"title":2870},{"EN":2871},"1Department of Earth Science, ETH-Z, CH-8092 Zürich; Switzerland (e-mail: weissert@erdw.ethz.ch)",[],{"orcid":2874,"title":2876,"openalex":2878},{"VOID":2875},"https:\u002F\u002Forcid.org\u002F0000-0002-0738-927X",{"EN":2877},"Helmut Weissert",{"VOID":2879},"A5029448385",{"id":2881,"sortIndex":40,"researcher":28,"roles":2882,"affiliations":2883,"properties":2892,"displayName":2896,"givenName":28,"familyName":28},"26171aca-558e-4749-bf37-b43ff1e71ed7",[],[2884],{"id":2885,"sortIndex":32,"affiliation":2886,"properties":28},"cf3942af-46b6-4980-a431-be8be3a7ac93",{"id":2885,"createTime":28,"updateTime":28,"relativeEntities":2887,"slug":28,"properties":2888,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2891,"statistic":28},[],{"title":2889},{"EN":2890},"2Dipartimento di Scienze della Terra, ‘Ardito Desio’, via Mangiagalli, 34, 20133 Milano, Italy",[],{"orcid":2893,"title":2895,"openalex":2897},{"VOID":2894},"https:\u002F\u002Forcid.org\u002F0000-0001-6213-6550",{"EN":2896},"Elisabetta Erba",{"VOID":2898},"A5059153091",{"url":28,"publisher":2900,"properties":2938},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":2901,"slug":872,"properties":2902,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":2907,"manageAffiliations":2912,"indexDatabases":2923,"url":935,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":2903,"eissn":2904,"issn":2905,"title":2906},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[2908],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":2909,"label":2910,"description":2911,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[2913,2918],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":2914,"slug":28,"properties":2915,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2917,"statistic":28},[],{"title":2916},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":2919,"slug":28,"properties":2920,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2922,"statistic":28},[],{"title":2921},{"EN":905},[],[2924,2931],{"id":924,"indexDatabase":2925,"url":930,"indexYears":931,"academicFieldIds":2930,"indexDatabaseRanking":934},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":2926,"label":2927,"description":2928,"key":781,"publicationTags":2929,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[933],{"id":909,"indexDatabase":2932,"url":921,"indexYears":28,"academicFieldIds":2937,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":2933,"label":2934,"description":2935,"key":918,"publicationTags":2936,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[816],{"issue":2939,"pages":2940,"volume":2942},{"VOID":2210},{"VOID":2941},"695-702",{"VOID":2943},"161",485,{"total":2944,"publishYear":2946,"statisticByYear":2947},2004,{"2012":142,"2013":278,"2014":134,"2015":132,"2016":147,"2017":199,"2018":127,"2019":136,"2020":133,"2021":202,"2022":140,"2023":140,"2024":140,"2025":123},"2004-07-01",[920,934],[2951,2954,2958,2962,2965,2968,2971,2974,2978,2981,2984,2987,2991,2994,2997,3000,3003,3006,3010,3013,3016,3019,3022,3025,3028,3031,3034,3037,3040,3043,3046,3050,3053,3056,3059,3062,3065,3068,3071,3074,3077,3080,3083,3086,3089,3092,3095,3098,3101,3104,3107,3110,3113,3116,3119,3122,3125,3128,3131,3134,3138,3141,3144,3147,3150,3153,3156,3160,3163,3166,3169,3172,3175,3178,3181,3184],{"id":28,"text":2952,"url":28,"identifiers":2953},"10.1016\u002FS0921-8181(01)00101-1",{"doi":2952},{"id":28,"text":2955,"url":28,"identifiers":2956},"Arthur M.A. Jenkyns H.C. Brumsack H.J. & Schlanger S.O. 1990. Stratigraphy geochemistry and palaeogeography of organic carbon-rich Cretaceous sequences. In: Ginsburg R.N. & Beaudoin B. (eds) Cretaceous Resources Events and Rhythms . Kluwer Dordrecht 75–119.",{"doi":2957},"10.1007\u002F978-94-015-6861-6_6",{"id":28,"text":2959,"url":28,"identifiers":2960},"Bartolini A. 2003 Cretaceous radiolarian biochronology and carbon isotope stratigraphy of ODP Site 1149 (Northwestern Pacific Nadezhda Basin). http:\u002F\u002Fwww.odp.tamu.edu\u002Fpublications\u002F185 SR\u002FVOLUME\u002FCHAPTERS\u002F011.",{"doi":2961},"10.2973\u002Fodp.proc.sr.185.011.2003",{"id":28,"text":2963,"url":28,"identifiers":2964},"10.1016\u002FS0031-0182(01)00416-3",{"doi":2963},{"id":28,"text":2966,"url":28,"identifiers":2967},"Bown, P.R., Burnett, J.A. & Gallagher, L.T. 1992. Calcareous nannoplankton evolution. Memorie di Scienze Geologiche, 43, 1–17.",{},{"id":28,"text":2969,"url":28,"identifiers":2970},"10.1016\u002F0377-8398(89)90035-2",{"doi":2969},{"id":28,"text":2972,"url":28,"identifiers":2973},"Bralower, T.J., CoBabe, E., Clement, B., Sliter, W.V., Osburn, C.L. & Longoria, J. 1999. The record of global change in mid-Cretaceous (Barremian–Albian) sections from the Sierra Madre, Northeastern Mexico. Journal of Foraminiferal Research, 29, 418–437.",{},{"id":28,"text":2975,"url":28,"identifiers":2976},"Bralower T.J. Premoli Silva I. & Malone M.J. et al. (eds) 2002 Proceedings of the Ocean Drilling Program Initial Reports 198 . Ocean Drilling Program College Station TX.",{"doi":2977},"10.2973\u002Fodp.proc.ir.198.2002",{"id":28,"text":2979,"url":28,"identifiers":2980},"10.1038\u002F425365a",{"doi":2979},{"id":28,"text":2982,"url":28,"identifiers":2983},"10.1016\u002F0012-821X(87)90033-1",{"doi":2982},{"id":28,"text":2985,"url":28,"identifiers":2986},"10.1016\u002F0012-821X(93)90165-6",{"doi":2985},{"id":28,"text":2988,"url":28,"identifiers":2989},"Channell J.E.T. Erba E. Nakanishi M. & Tamaki K. 1995. Late Jurassic–Early Cretaceous time scales and oceanic magnetic anomaly block models. In: Berggren W.A. Kent D.V. Aubry M.P. & Hardenbol J. (eds) Geochronology Time Scales and Global Stratigraphic Correlations . SEPM Special Publications 54 51–63.",{"doi":2990},"10.2110\u002Fpec.95.04.0051",{"id":28,"text":2992,"url":28,"identifiers":2993},"Channell, J.E.T., Erba, E., Muttoni, G. & Tremolada, F. 2000. Early Cretaceous magnetic stratigraphy in the APTICORE drill core and adjacent outcrop in Cismon (southern Alps, Italy), and correlation to the proposed Barremian&Aptian boundary stratotype. Geological Society of America Bulletin, 112, 1430–1443.",{},{"id":28,"text":2995,"url":28,"identifiers":2996},"Clarke, L.J. & Jenkyns, H.C. 1999. New oxygen isotope evidence for long-term Cretaceous climatic change in the southern Hemisphere. Geology, 8, 699–702.",{},{"id":28,"text":2998,"url":28,"identifiers":2999},"D'Argenio, B., Ferreri, V., Ardillo, F. & Buonocunto, F.P. 1993. Microstratigrafia e stratigrafia sequenziale. Studi sui depositi di piattaforma carbonatica nel Cretaceo del Monte Maggiore (Appennino Meridionale). 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Terra Nova, 12, 289–294.",{},{"id":28,"text":3185,"url":28,"identifiers":3186},"Ziegler P. (ed.) 1988 Evolution of the Arctic North Atlantic and the Western Tethys . 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The Science of Climate Change1996CambridgeCambridge University Press",{},{"id":28,"text":3369,"url":28,"identifiers":3370},"Inoue J.Mass budget of Khumbu GlacierSeppyo197739Special Issue, 1519",{},{"id":28,"text":3372,"url":28,"identifiers":3373},"Inoue J.Gales over the Himalayas in 1976Seppyo197840Special Issue, 5659",{},{"id":28,"text":3375,"url":28,"identifiers":3376},"Kuhle M.Die Vergletscherung Tibets und die Entstehung von EiszeitenSpektrum der Wissenschaft1986September4254",{},{"id":28,"text":3378,"url":28,"identifiers":3379},"Kuhle M.Subtropical mountain and highland glaciation as Ice Age triggers and the waning of the glacial periods in the 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Hingham349366",{},{"id":28,"text":3453,"url":28,"identifiers":3454},"10.1029\u002FJD092iD07p08411",{"doi":3453},{"id":28,"text":3456,"url":28,"identifiers":3457},"10.1038\u002F360647a0",{"doi":3456},{"id":28,"text":3459,"url":28,"identifiers":3460},"10.1038\u002F323526a0",{"doi":3459},{"id":28,"text":3462,"url":28,"identifiers":3463},"10.1038\u002F359117a0",{"doi":3462},{"id":28,"text":3465,"url":28,"identifiers":3466},"10.1029\u002FJD094iD15p18409",{"doi":3465},{"id":28,"text":3468,"url":28,"identifiers":3469},"10.1016\u002F0033-5894(73)90057-4",{"doi":3468},{"id":28,"text":3471,"url":28,"identifiers":3472},"10.1038\u002F343549a0",{"doi":3471},{"id":28,"text":3474,"url":28,"identifiers":3475},"10.1016\u002F0277-3791(95)00061-5",{"doi":3474},{"id":28,"text":3477,"url":28,"identifiers":3478},"Shiraiwa T.Glacial fluctuations and cryogenic environments in the Langtang Valley, Nepal HimalayaContributions from the Institution of Low Temperature Science199338JapanHokkaido University198Series 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and ridges in Shorong and Khumbu HimalSeppyo1978402632",{},{"id":28,"text":3522,"url":28,"identifiers":3523},"Zheng BenxingThe influence of Himalayan uplift on the development of Quaternary glaciersZeitscrift für Geomorphologie1989a7689115",{},{"id":28,"text":3525,"url":28,"identifiers":3526},"10.1016\u002F0033-5894(89)90039-2",{"doi":3525},{"id":28,"text":3528,"url":28,"identifiers":3529},"10.1177\u002F095968369100100207",{"doi":3528},{"id":3531,"createTime":3532,"updateTime":3532,"relativeEntities":3533,"slug":3534,"properties":3535,"entityType":956,"verifyStatus":26,"verifyTime":3532,"verifyNote":958,"languages":3546,"translateLanguages":28,"viewCount":32,"primaryUrl":3547,"fullTextUrl":28,"authors":3548,"publicationType":1053,"publisherRelationship":3741,"citationCount":3785,"citationInfo":3786,"publishDate":2948,"publishYear":2946,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":3788,"openAccess":28,"references":3789,"isForceReanalyzing":1497},"07784a6a-ec53-4653-8f6f-b4080accfa84","2025-01-02T15:43:04.664+00:00",[],"Carbon-isotope-stratigraphy-recorded-by-the-Cenomanian-Turonian-Oceanic-Anoxic-Event-correlation-and-implications-based-on-three-key-localities",{"openalex":3536,"mag":3538,"abstract":3540,"title":3542,"doi":3544},{"VOID":3537},"W2151375251",{"VOID":3539},"2151375251",{"EN":3541},"\u003Cjats:p>\n            We present new, detailed carbon-isotope records for bulk carbonate, total organic carbon (TOC) and phytane from three key sections spanning the Cenomanian–Turonian boundary interval (Eastbourne, England; Gubbio, Italy; Tarfaya, Morocco), with the purpose of establishing a common chemostratigraphic framework for Oceanic Anoxic Event (OAE) 2. Isotope curves from all localities are characterized by a positive carbon-isotope excursion of\n            \u003Cjats:italic>c\u003C\u002Fjats:italic>\n            . 4‰ for TOC and phytane and\n            \u003Cjats:italic>c\u003C\u002Fjats:italic>\n            . 2.5‰ for carbonate, although diagenetic overprinting appears to have obliterated the primary carbonate carbon-isotope signal in at least part of the Tarfaya section. Stratigraphically, peak\n            \u003Cjats:italic>δ\u003C\u002Fjats:italic>\n            \u003Cjats:sup>13\u003C\u002Fjats:sup>\n            C values for all components are followed by intervals of high, near-constant\n            \u003Cjats:italic>δ\u003C\u002Fjats:italic>\n            \u003Cjats:sup>13\u003C\u002Fjats:sup>\n            C in the form of an isotopic plateau. Recognition of an unambiguous return to background\n            \u003Cjats:italic>δ\u003C\u002Fjats:italic>\n            \u003Cjats:sup>13\u003C\u002Fjats:sup>\n            C values above the plateau is, however, contentious in all sections, hence no firm chemostratigraphic marker for the end-point of the positive isotopic excursion can be established. The stratigraphically consistent first appearance of the calcareous nannofossil\n            \u003Cjats:italic>Quadrum gartneri\u003C\u002Fjats:italic>\n            at or near the Cenomanian–Turonian boundary as established by ammonite stratigraphy, in conjunction with the end of the\n            \u003Cjats:italic>δ\u003C\u002Fjats:italic>\n            \u003Cjats:sup>13\u003C\u002Fjats:sup>\n            C maximum characteristic of the isotopic plateau, provides a potentially powerful tool for delimiting the stratigraphic extent and duration of OAE 2. This Oceanic Anoxic Event is demonstrated to be largely, if not wholly, confined to the latest part of the Cenomanian stage.\n          \u003C\u002Fjats:p>",{"EN":3543},"Carbon-isotope stratigraphy recorded by the Cenomanian–Turonian Oceanic Anoxic Event: correlation and implications based on three key localities",{"VOID":3545},"10.1144\u002F0016-764903-077",[31],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002F0016-764903-077",[3549,3576,3593,3610,3627,3644,3661,3675,3690,3707,3724],{"id":3550,"sortIndex":32,"researcher":28,"roles":3551,"affiliations":3552,"properties":3569,"displayName":3573,"givenName":28,"familyName":28},"d49be422-83a8-4a4f-9967-b94ff2364961",[],[3553,3561],{"id":3554,"sortIndex":32,"affiliation":3555,"properties":28},"c982ebae-49b1-4e51-a69a-d6267c406d3c",{"id":3554,"createTime":28,"updateTime":28,"relativeEntities":3556,"slug":28,"properties":3557,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3560,"statistic":28},[],{"title":3558},{"EN":3559},"1Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK",[],{"id":3562,"sortIndex":40,"affiliation":3563,"properties":28},"e1ae2320-7ce2-4afa-927a-19582b8408e7",{"id":3562,"createTime":28,"updateTime":28,"relativeEntities":3564,"slug":28,"properties":3565,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3568,"statistic":28},[],{"title":3566},{"EN":3567},"5Present address: Department of Geology & Petroleum Geology, University of Aberdeen, Aberdeen AB2 3UE, UK (e-mail: h.tsikos@abdn.ac.uk)",[],{"orcid":3570,"title":3572,"openalex":3574},{"VOID":3571},"https:\u002F\u002Forcid.org\u002F0000-0002-1352-2655",{"EN":3573},"Harilaos Tsikos",{"VOID":3575},"A5079709882",{"id":3577,"sortIndex":40,"researcher":28,"roles":3578,"affiliations":3579,"properties":3586,"displayName":3590,"givenName":28,"familyName":28},"7d4a7818-36e6-4877-a02f-d4bbefe427e4",[],[3580],{"id":3554,"sortIndex":32,"affiliation":3581,"properties":28},{"id":3554,"createTime":28,"updateTime":28,"relativeEntities":3582,"slug":28,"properties":3583,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3585,"statistic":28},[],{"title":3584},{"EN":3559},[],{"orcid":3587,"title":3589,"openalex":3591},{"VOID":3588},"https:\u002F\u002Forcid.org\u002F0000-0002-2728-0984",{"EN":3590},"Hugh C. 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Mangiagalli 34, 20133 Milan, Italy",[],{"title":3606,"openalex":3608},{"EN":3607},"Ben Walsworth‐Bell",{"VOID":3609},"A5059360780",{"id":3611,"sortIndex":42,"researcher":28,"roles":3612,"affiliations":3613,"properties":3620,"displayName":3624,"givenName":28,"familyName":28},"8395292d-439d-4cc7-ad00-7cf155c6475b",[],[3614],{"id":3598,"sortIndex":32,"affiliation":3615,"properties":28},{"id":3598,"createTime":28,"updateTime":28,"relativeEntities":3616,"slug":28,"properties":3617,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3619,"statistic":28},[],{"title":3618},{"EN":3603},[],{"orcid":3621,"title":3623,"openalex":3625},{"VOID":3622},"https:\u002F\u002Forcid.org\u002F0000-0002-9584-8471",{"EN":3624},"Maria Rose Petrizzo",{"VOID":3626},"A5013301552",{"id":3628,"sortIndex":45,"researcher":28,"roles":3629,"affiliations":3630,"properties":3639,"displayName":3641,"givenName":28,"familyName":28},"47f759a6-338b-43ba-ac97-a7c3c37ea14d",[],[3631],{"id":3632,"sortIndex":32,"affiliation":3633,"properties":28},"c4875ae0-3d3e-4a65-98a3-89e0ffe98d5c",{"id":3632,"createTime":28,"updateTime":28,"relativeEntities":3634,"slug":28,"properties":3635,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3638,"statistic":28},[],{"title":3636},{"EN":3637},"3Department of Marine Biogeochemistry and Toxicology, Royal Netherlands Institute of Sea Research (NIOZ), 1790 AB Den Burg, The Netherlands",[],{"title":3640,"openalex":3642},{"EN":3641},"A. 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Paleoceanography, 17, 1–13.",{},{"id":28,"text":3855,"url":28,"identifiers":3856},"Luderer, F. & Kuhnt, W. 1997. A high resolution record of the Rotalipora extinction in laminated organic-carbon rich limestones of the Tarfaya Atlantic coastal basin (Morocco). Annales de la Société Géologique du Nord, 5, 199–205.",{},{"id":28,"text":3858,"url":28,"identifiers":3859},"10.1016\u002FS0031-0182(99)00009-7",{"doi":3858},{"id":28,"text":3861,"url":28,"identifiers":3862},"Pratt L.M. & Threlkeld C.N. 1984. Stratigraphic significance of 13 C\u002F 12 C ratios in mid-Cretaceous rocks of the Western Interior U.S.AÒ. In: Stott D.F. & Glass D.J. (eds) The Mesozoic of Middle North America . Canadian Society of Petroleum Geologists Memoirs 9 305–312.",{},{"id":28,"text":3864,"url":28,"identifiers":3865},"Pratt L.M. Arthur M.A. Dean W.E. & Scholle P.A. 1993. Paleoceanographic cycles and events during the Late Cretaceous in the Western Interior Seaway of North America. 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In: Brooks J. & Fleet A.J. (eds) Marine Petroleum Source Rocks . Geological Society London Special Publications 26 371–399.",{"doi":3876},"10.1144\u002FGSL.SP.1987.026.01.24",{"id":28,"text":3878,"url":28,"identifiers":3879},"Scholle, P.A. & Arthur, M.A. 1980. Carbon-isotope fluctuations in Cretaceous pelagic limestones: potential stratigraphic and petroleum exploration tool. AAPG Bulletin, 64, 67–87.",{},{"id":28,"text":3881,"url":28,"identifiers":3882},"10.1130\u002F0016-7606(2000)112\u003C308:HSIRFT>2.0.CO;2",{"doi":3881},{"id":28,"text":3884,"url":28,"identifiers":3885},"Watkins D.K. 1985. Biostratigraphy and paleoecology of calcareous nannofossils in the Greenhorn marine cycle. In: Pratt L.M. Kauffman E.G. & Zelt F.B. (eds) Fine-grained Deposits and Biofacies of the Cretaceous Western Interior Seaway: Evidence of Cyclic Sedimentary Processes . SEPM Field Trip Guidebook 4 151–156.",{"doi":3886},"10.2110\u002Fsepmfg.04.151",{"id":3888,"createTime":3889,"updateTime":3889,"relativeEntities":3890,"slug":3891,"properties":3892,"entityType":956,"verifyStatus":26,"verifyTime":3903,"verifyNote":958,"languages":3904,"translateLanguages":28,"viewCount":32,"primaryUrl":3905,"fullTextUrl":28,"authors":3906,"publicationType":1053,"publisherRelationship":4041,"citationCount":458,"citationInfo":4085,"publishDate":4087,"publishYear":1963,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":4088,"openAccess":28,"references":4089,"isForceReanalyzing":1497},"f7686b94-65f3-4e1d-b919-826fba620e17","2024-10-16T02:01:47.952+00:00",[],"The-geochemistry-of-young-volcanism-throughout-western-Panama-and-southeastern-Costa-Rica-an-overview",{"openalex":3893,"mag":3895,"abstract":3897,"title":3899,"doi":3901},{"VOID":3894},"W1990327655",{"VOID":3896},"1990327655",{"EN":3898},"\u003Cjats:p>Oblique aseismic subduction below western Panama and southeastern Costa Rica has produced Recent arc-related volcanism. The aseismicity is probably related to the subduction of relatively hot oceanic lithosphere. The volcanism throughout this region over the past 2 Ma has been quite distinct, consisting of felsic magmas (andesites to rhyolites but mainly dacites) with geochemical signatures suggesting a metamorphosed basaltic source. It is believed that the subduction of young oceanic crust sets up conditions under which the slab melts rather than the overlying mantle wedge. Rocks with slab-melt geochemistries and associated with young subducted crust have been termed adakites elsewhere. The young adakite melts are sometimes associated with a few rare young high-Nb basalts, but there is no obvious genetic link between them through differentiation. High-Nb basalts may also be derived from the partial melting of the subducted oceanic crust. High-Nb basalt migmatites have been found with pegmatites of adakite compositions in the exposed subduction terrain of the Catalina Schist, California. Alternatively, the high-Nb basalts may be partial melts of phlogopite-rich mantle that has previously reacted with adakite magmas.\u003C\u002Fjats:p>\n          \u003Cjats:p>Eruption of adakites and high-Nb basalts was preceded by a 2-3 Ma period of relative quiescence. Prior to this, there was a 7 Ma period of calc-alkaline volcanism typical of the present-day magmatism (associated with a distinct Benioff zone) found throughout the Central American arc. 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