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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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global set of present plate boundaries on the Earth is presented in digital form. Most come from sources in the literature. A few boundaries are newly interpreted from topography, volcanism, and\u002For seismicity, taking into account relative plate velocities from magnetic anomalies, moment tensor solutions, and\u002For geodesy. In addition to the 14 large plates whose motion was described by the NUVEL‐1A poles (Africa, Antarctica, Arabia, Australia, Caribbean, Cocos, Eurasia, India, Juan de Fuca, Nazca, North America, Pacific, Philippine Sea, South America), model PB2002 includes 38 small plates (Okhotsk, Amur, Yangtze, Okinawa, Sunda, Burma, Molucca Sea, Banda Sea, Timor, Birds Head, Maoke, Caroline, Mariana, North Bismarck, Manus, South Bismarck, Solomon Sea, Woodlark, New Hebrides, Conway Reef, Balmoral Reef, Futuna, Niuafo'ou, Tonga, Kermadec, Rivera, Galapagos, Easter, Juan Fernandez, Panama, North Andes, Altiplano, Shetland, Scotia, Sandwich, Aegean Sea, Anatolia, Somalia), for a total of 52 plates. No attempt is made to divide the Alps‐Persia‐Tibet mountain belt, the Philippine Islands, the Peruvian Andes, the Sierras Pampeanas, or the California‐Nevada zone of dextral transtension into plates; instead, they are designated as “orogens” in which this plate model is not expected to be accurate. The cumulative‐number\u002Farea distribution for this model follows a power law for plates with areas between 0.002 and 1 steradian. Departure from this scaling at the small‐plate end suggests that future work is very likely to define more very small plates within the orogens. The model is presented in four digital files: a set of plate boundary segments; a set of plate outlines; a set of outlines of the orogens; and a table of characteristics of each digitization step along plate boundaries, including estimated relative velocity vector and classification into one of 7 types (continental convergence zone, continental transform fault, continental rift, oceanic spreading ridge, oceanic transform fault, oceanic convergent boundary, subduction zone). Total length, mean velocity, and total rate of area production\u002Fdestruction are computed for each class; the global rate of area production and destruction is 0.108 m\u003Cjats:sup>2\u003C\u002Fjats:sup>\u002Fs, which is higher than in previous models because of the incorporation of back‐arc spreading.\u003C\u002Fjats:p>",{"EN":980},"An updated digital model of plate boundaries",{"VOID":982},"10.1029\u002F2001gc000252","PUBLICATION","Auto 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Z.Zhengguo andL.Xiang Terrane accretion and continent collision between Sino‐Korean plate and South China plate during Hercynian‐Indosinian orogeny paper presented atthe International Tectonostratigraphic Terrane Conference 4 58 Nonjing China 1998.",{},{"id":28,"text":1124,"url":28,"identifiers":1125},"Bevis M., 1999, Crustal motion north and south of the Arica deflection; comparing recent geodetic results from the Central Andes, Geochem. Geophys. Geosyst., 1",{},{"id":28,"text":1127,"url":28,"identifiers":1128},"Bevis M., 2001, On the strength of interplate coupling and the rate of back arc convergence in the Central Andes: An analysis of the interseismic velocity field, Geochem. Geophys. 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T.Halboutyet al. 5 sheets at 1:10 000 000 Am. Assoc. Petrol. Geol. Tulsa Okla. 1981.",{},{"id":28,"text":1167,"url":28,"identifiers":1168},"Circum‐Pacific Map Project Plate‐Tectonic Map of the Circum‐Pacific Region edited byM. T.Halboutyet al. 5 sheets at 1:10 000 000 and 1 sheet at 1:20 000 000 Amer. Assoc. Petr. Geol. Tulsa Okla. 1986.",{},{"id":28,"text":1170,"url":28,"identifiers":1171},"10.1029\u002F2002EO000120",{"doi":1170},{"id":28,"text":1173,"url":28,"identifiers":1174},"10.1016\u002F0264-3707(86)90031-1",{"doi":1173},{"id":28,"text":1176,"url":28,"identifiers":1177},"Craig H., 1983, Active ridge crest mapping on the Juan Fernandez micro‐plate: The use of Sea Beam‐controlled hydrothermal plume surveys (abstract), Eos Trans. 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G.Grunthal K.Shedlock andP.Zhang Global Seismic Hazard Map 1:35 000 000 Global Seismic Hazard Assessment Program UN\u002FInternational Decade of Natural Disaster Reduction International Lithosphere Program 1999. (Available athttp:\u002F\u002Fseismo.ethz.ch\u002FGSHAP).",{},{"id":28,"text":1242,"url":28,"identifiers":1243},"10.1130\u002F0091-7613(2000)28\u003C1043:BBAPNA>2.0.CO;2",{"doi":1242},{"id":28,"text":1245,"url":28,"identifiers":1246},"10.1016\u002FS0012-821X(96)00227-0",{"doi":1245},{"id":28,"text":1248,"url":28,"identifiers":1249},"10.1029\u002FRF001p0066",{"doi":1248},{"id":28,"text":1251,"url":28,"identifiers":1252},"10.1029\u002F1999TC001152",{"doi":1251},{"id":28,"text":1254,"url":28,"identifiers":1255},"10.1029\u002F93JB00892",{"doi":1254},{"id":28,"text":1257,"url":28,"identifiers":1258},"Hamilton W., 1979, Tectonics of the Indonesian region, U.S. Geol. Surv. 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Project, 60, 909",{},{"id":28,"text":1284,"url":28,"identifiers":1285},"Ishihara T., 2001, Seafloor spreading in the southern Mariana Trough inferred from 3‐component magnetometer data, Eos Trans. AGU, 82, F1202",{},{"id":28,"text":1287,"url":28,"identifiers":1288},"10.1029\u002F92JB00944",{"doi":1287},{"id":28,"text":1290,"url":28,"identifiers":1291},"10.1029\u002F95JB01294",{"doi":1290},{"id":28,"text":1293,"url":28,"identifiers":1294},"10.1111\u002Fj.1365-246X.1994.tb03286.x",{"doi":1293},{"id":28,"text":1296,"url":28,"identifiers":1297},"Johnson R. W., 1979, Geotectonics and volcanism in Papua New Guinea: A review of the late Cainozoic, BMR J. Aust. Geol. 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A., 1982, Holocene plate tectonics of the Sea of Okhotsk region, Dokl. Acad. Sci. USSR, Earth Sci. Ser., Engl. 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AGU, 77",{},{"id":28,"text":1603,"url":28,"identifiers":1604},"10.1130\u002F0091-7613(1994)022\u003C0451:TIOTIO>2.3.CO;2",{"doi":1603},{"id":28,"text":1606,"url":28,"identifiers":1607},"10.1130\u002F0091-7613(2001)029\u003C0075:GEORMB>2.0.CO;2",{"doi":1606},{"id":28,"text":1609,"url":28,"identifiers":1610},"10.1029\u002FGD027p0337",{"doi":1609},{"id":28,"text":1612,"url":28,"identifiers":1613},"10.1016\u002FS0040-1951(99)00259-0",{"doi":1612},{"id":28,"text":1615,"url":28,"identifiers":1616},"10.1016\u002F0012-821X(78)90004-3",{"doi":1615},{"id":28,"text":1618,"url":28,"identifiers":1619},"10.1016\u002F0040-1951(82)90229-3",{"doi":1618},{"id":28,"text":1621,"url":28,"identifiers":1622},"10.1029\u002F94JB00692",{"doi":1621},{"id":28,"text":1624,"url":28,"identifiers":1625},"10.1029\u002F94JB00335",{"doi":1624},{"id":28,"text":1627,"url":28,"identifiers":1628},"10.1130\u002FSPE295-p91",{"doi":1627},{"id":28,"text":1630,"url":28,"identifiers":1631},"10.1029\u002FJB093iB10p11863",{"doi":1630},{"id":28,"text":1633,"url":28,"identifiers":1634},"10.1016\u002F0025-3227(93)90017-P",{"doi":1633},{"id":28,"text":1636,"url":28,"identifiers":1637},"Wright D. J., 1986, Plate boundary structures and processes at the northerm terminus of the Tonga trench (abstract), Eos Trans. AGU, 67, 1238",{},{"id":28,"text":1639,"url":28,"identifiers":1640},"Yamazaki T. F.Murakami E.Saito andM.Yuasa Opening of the northern Mariana Trough (abstract) paper presented atTectonics of Eastern Asia and Western Pacific Continental Margin 1988 DELP Tokyo International Symposium 6th Japan‐U.S.S.R. Geotectonic Symposium 25–26 1988.",{},{"id":28,"text":1642,"url":28,"identifiers":1643},"10.1016\u002F0040-1951(93)90333-F",{"doi":1642},{"id":28,"text":1645,"url":28,"identifiers":1646},"10.1029\u002F2000GC000106",{"doi":1645},{"id":28,"text":1648,"url":28,"identifiers":1649},"10.1029\u002F92JB00132",{"doi":1648},false,{"id":1652,"createTime":1653,"updateTime":1653,"relativeEntities":1654,"slug":1655,"properties":1656,"entityType":983,"verifyStatus":26,"verifyTime":1653,"verifyNote":984,"languages":1667,"translateLanguages":28,"viewCount":32,"primaryUrl":1668,"fullTextUrl":28,"authors":1669,"publicationType":1007,"publisherRelationship":1689,"citationCount":1740,"citationInfo":1741,"publishDate":1749,"publishYear":1742,"citationAnalyzeStatus":879,"lastCitationAnalyze":28,"indexDatabases":1750,"openAccess":28,"references":1751,"isForceReanalyzing":1650},"61316076-a0ff-4ae0-b3b0-6dcea642a6a6","2024-10-11T09:20:33.287+00:00",[],"Relationships-between-the-trace-element-composition-of-sedimentary-rocks-and-upper-continental-crust",{"openalex":1657,"mag":1659,"abstract":1661,"title":1663,"doi":1665},{"VOID":1658},"W1880555926",{"VOID":1660},"1880555926",{"EN":1662},"\u003Cjats:p>Estimates of the average composition of various Precambrian shields and a variety of estimates of the average composition of upper continental crust show considerable disagreement for a number of trace elements, including Ti, Nb, Ta, Cs, Cr, Ni, V, and Co. For these elements and others that are carried predominantly in terrigenous sediment, rather than in solution (and ultimately into chemical sediment), during the erosion of continents the La\u002Felement ratio is relatively uniform in clastic sediments. Since the average rare earth element (REE) pattern of terrigenous sediment is widely accepted to reflect the upper continental crust, such correlations provide robust estimates of upper crustal abundances for these trace elements directly from the sedimentary data. Suggested revisions to the upper crustal abundances of \u003Cjats:italic>Taylor and McLennan\u003C\u002Fjats:italic> [1985] are as follows (all in parts per million): Sc = 13.6, Ti = 4100, V = 107, Cr = 83, Co = 17, Ni = 44, Nb = 12, Cs = 4.6, Ta = 1.0, and Pb = 17. The upper crustal abundances of Rb, Zr, Ba, Hf, and Th were also directly reevaluated and K, U, and Rb indirectly evaluated (by assuming Th\u002FU, K\u002FU, and K\u002FRb ratios), and no revisions are warranted for these elements. In the models of crustal composition proposed by \u003Cjats:italic>Taylor and McLennan\u003C\u002Fjats:italic> [1985] the lower continental crust (75% of the entire crust) is determined by subtraction of the upper crust (25%) from a model composition for the bulk crust, and accordingly, these changes also necessitate revisions to lower crustal abundances for these elements.\u003C\u002Fjats:p>",{"EN":1664},"Relationships between the trace element composition of sedimentary rocks and upper continental crust",{"VOID":1666},"10.1029\u002F2000gc000109",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F2000GC000109",[1670],{"id":1671,"sortIndex":32,"researcher":28,"roles":1672,"affiliations":1673,"properties":1682},"34b74c15-a449-4eae-9405-db245b250ce2",[],[1674],{"id":1675,"sortIndex":32,"affiliation":1676,"properties":28},"49a4ab81-7410-4b00-8d1f-bbc4bf2667d0",{"id":1675,"createTime":28,"updateTime":28,"relativeEntities":1677,"slug":28,"properties":1678,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1681,"statistic":28},[],{"title":1679},{"EN":1680},"Department of Geosciences, State University of New York at Stony Brook, Stony Brook, New York, 11794‐2100",[],{"orcid":1683,"title":1685,"openalex":1687},{"VOID":1684},"https:\u002F\u002Forcid.org\u002F0000-0003-4259-7178",{"EN":1686},"S. 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A combination of approaches is required to estimate the major and trace element abundances in DM. Absolute concentrations of few elements can be estimated directly, and the bulk of the estimates is derived using elemental ratios. The isotopic composition of MORB allows calculation of parent‐daughter ratios. These estimates form the “backbone” of the abundances of the trace elements that make up the Coryell‐Masuda diagram (spider diagram). The remaining elements of the Coryell‐Masuda diagram are estimated through the composition of MORB. A third group of estimates is derived from the elemental and isotopic composition of peridotites. The major element composition is obtained by subtraction of a low‐degree melt from a bulk silicate Earth (BSE) composition. The continental crust (CC) is thought to be complementary to the DM, and ratios that are chondritic in the CC are expected to also be chondritic in the DM. Thus some of the remaining elements are estimated using the composition of CC and chondrites. Volatile element and noble gas concentrations are estimated using constraints from the composition of MORBs and ocean island basalts (OIBs). 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It is shown that the removal of silicate contamination is the most important step for the measurement of Mg\u002FCa ratios. In an example, bulk sample Mg\u002FCa decreases from 10.5 to 2.5 mmol mol\u003Cjats:sup>−1\u003C\u002Fjats:sup> during clay removal. Oxidation of organic material causes a lowering of sample Mg\u002FCa in the order of 10% or approximately 1°C when converted to temperature. Use of dilute acid leaching to remove adsorbed contaminants causes partial dissolution of the sample carbonate and a corresponding decrease in Mg\u002FCa. Reductive treatment also causes dissolution of the sample and a decrease in the Mg\u002FCa ratio of up to 10–15%. Sample preparation for Sr\u002FCa analysis does not require the same degree of rigor as is necessary for Mg\u002FCa work. The “within‐run” reproducibility of the method described here for \u003Cjats:italic>G. ruber\u003C\u002Fjats:italic> in a core‐top sample from the Arabian Sea was ±1.8% (mean sample ratio was 4.72 mmol mol\u003Cjats:sup>−1\u003C\u002Fjats:sup>). When converted to temperature, this becomes 28 ± 0.2°C. The equivalent result for Sr\u002FCa was ±0.5% (mean ratio = 1.44 mmol mol\u003Cjats:sup>−1\u003C\u002Fjats:sup>).\u003C\u002Fjats:p>",{"EN":3282},"A study of cleaning procedures used for foraminiferal Mg\u002FCa paleothermometry",{"VOID":3284},"10.1029\u002F2003gc000559",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F2003GC000559",[3288,3307,3324],{"id":3289,"sortIndex":32,"researcher":28,"roles":3290,"affiliations":3291,"properties":3300},"6607e0b8-15e2-439d-a074-a74e92889df5",[],[3292],{"id":3293,"sortIndex":32,"affiliation":3294,"properties":28},"6e5237ed-57b0-45f6-908a-66df2d3c04ac",{"id":3293,"createTime":28,"updateTime":28,"relativeEntities":3295,"slug":28,"properties":3296,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3299,"statistic":28},[],{"title":3297},{"VI":3298},"Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ U.K.",[],{"orcid":3301,"title":3303,"openalex":3305},{"VOID":3302},"https:\u002F\u002Forcid.org\u002F0000-0001-7870-6431",{"EN":3304},"S. 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AGU, 82",{},{"id":28,"text":3402,"url":28,"identifiers":3403},"10.1029\u002F2002GC000312",{"doi":3402},{"id":28,"text":3405,"url":28,"identifiers":3406},"10.1016\u002F0012-821X(81)90022-4",{"doi":3405},{"id":28,"text":3408,"url":28,"identifiers":3409},"10.1016\u002F0016-7037(83)90029-7",{"doi":3408},{"id":28,"text":3411,"url":28,"identifiers":3412},"10.1016\u002F0012-821X(85)90154-2",{"doi":3411},{"id":28,"text":3414,"url":28,"identifiers":3415},"10.1029\u002F96PA01491",{"doi":3414},{"id":28,"text":3417,"url":28,"identifiers":3418},"Deer W. A. R. A.Howie andJ.Zussman An Introduction to the Rock Forming Minerals 2 ed. Addison‐Wesley‐Longman Reading Mass. 1992.",{},{"id":28,"text":3420,"url":28,"identifiers":3421},"10.1029\u002F2001GC000200",{"doi":3420},{"id":28,"text":3423,"url":28,"identifiers":3424},"10.1016\u002F0025-3227(92)90227-9",{"doi":3423},{"id":28,"text":3426,"url":28,"identifiers":3427},"10.1029\u002F2001GC000169",{"doi":3426},{"id":28,"text":3429,"url":28,"identifiers":3430},"10.1038\u002F35013033",{"doi":3429},{"id":28,"text":3432,"url":28,"identifiers":3433},"10.2307\u002F1484483",{"doi":3432},{"id":28,"text":3435,"url":28,"identifiers":3436},"10.1016\u002FS0009-2541(01)00399-0",{"doi":3435},{"id":28,"text":3438,"url":28,"identifiers":3439},"10.1016\u002F0016-7037(96)00196-2",{"doi":3438},{"id":28,"text":3441,"url":28,"identifiers":3442},"10.1016\u002F0016-7037(91)90491-M",{"doi":3441},{"id":28,"text":3444,"url":28,"identifiers":3445},"10.1016\u002F0009-2541(93)90292-Q",{"doi":3444},{"id":28,"text":3447,"url":28,"identifiers":3448},"10.1126\u002Fscience.289.5485.1719",{"doi":3447},{"id":28,"text":3450,"url":28,"identifiers":3451},"10.1016\u002FS0277-3791(01)00081-6",{"doi":3450},{"id":28,"text":3453,"url":28,"identifiers":3454},"10.1029\u002F2001GC000280",{"doi":3453},{"id":28,"text":3456,"url":28,"identifiers":3457},"McCave I. N. North East Atlantic palaeoceanography and climate change community research project of NERC cruise report Univ. of Cambridge Cambridge 1984.",{},{"id":28,"text":3459,"url":28,"identifiers":3460},"10.1016\u002F0025-3227(93)90026-R",{"doi":3459},{"id":28,"text":3462,"url":28,"identifiers":3463},"10.1016\u002F0016-7037(82)90290-3",{"doi":3462},{"id":28,"text":3465,"url":28,"identifiers":3466},"10.1016\u002FS0377-8398(97)00028-5",{"doi":3465},{"id":28,"text":3468,"url":28,"identifiers":3469},"Riley J. P. andR.Chester Introduction to Marine Chemistry Academic San Diego Calif. 1971.",{},{"id":28,"text":3471,"url":28,"identifiers":3472},"10.1029\u002F1999PA000415",{"doi":3471},{"id":28,"text":3474,"url":28,"identifiers":3475},"10.1016\u002F0016-7037(94)90497-9",{"doi":3474},{"id":28,"text":3477,"url":28,"identifiers":3478},"Sirocko F. Abrupt change in monsoonal climate: Evidence from the geochemical composition of Arabian Sea sediments Habilitation thesis Christian‐Albrechts‐Univ. Kiel 1994.",{},{"id":28,"text":3480,"url":28,"identifiers":3481},"10.1016\u002FS0016-7037(99)00129-5",{"doi":3480},{"id":3483,"createTime":3484,"updateTime":3485,"relativeEntities":3486,"slug":3487,"properties":3488,"entityType":983,"verifyStatus":26,"verifyTime":3503,"verifyNote":984,"languages":3504,"translateLanguages":3505,"viewCount":32,"primaryUrl":3506,"fullTextUrl":28,"authors":3507,"publicationType":1007,"publisherRelationship":3725,"citationCount":3777,"citationInfo":3778,"publishDate":3783,"publishYear":3779,"citationAnalyzeStatus":879,"lastCitationAnalyze":28,"indexDatabases":3784,"openAccess":28,"references":3785,"isForceReanalyzing":1650},"3de23f1f-cb5f-4ee9-8740-a76e08d36734","2024-10-06T03:23:26.762+00:00","2024-12-30T00:42:49.826+00:00",[],"High-precision-isotopic-characterization-of-USGS-reference-materials-by-TIMS-and-MC-ICP-MS",{"openalex":3489,"mag":3491,"abstract":3493,"title":3496,"keywords":3499,"doi":3501},{"VOID":3490},"W2117683602",{"VOID":3492},"2117683602",{"EN":3494,"VI":3495},"\u003Cjats:p>The Pacific Centre for Isotopic and Geochemical Research (PCIGR) at the University of British Columbia has undertaken a systematic analysis of the isotopic (Sr, Nd, and Pb) compositions and concentrations of a broad compositional range of U.S. Geological Survey (USGS) reference materials, including basalt (BCR‐1, 2; BHVO‐1, 2), andesite (AGV‐1, 2), rhyolite (RGM‐1, 2), syenite (STM‐1, 2), granodiorite (GSP‐2), and granite (G‐2, 3). USGS rock reference materials are geochemically well characterized, but there is neither a systematic methodology nor a database for radiogenic isotopic compositions, even for the widely used BCR‐1. This investigation represents the first comprehensive, systematic analysis of the isotopic composition and concentration of USGS reference materials and provides an important database for the isotopic community. In addition, the range of equipment at the PCIGR, including a Nu Instruments Plasma MC‐ICP‐MS, a Thermo Finnigan Triton TIMS, and a Thermo Finnigan Element2 HR‐ICP‐MS, permits an assessment and comparison of the precision and accuracy of isotopic analyses determined by both the TIMS and MC‐ICP‐MS methods (e.g., Nd isotopic compositions). For each of the reference materials, 5 to 10 complete replicate analyses provide coherent isotopic results, all with external precision below 30 ppm (2 SD) for Sr and Nd isotopic compositions (27 and 24 ppm for TIMS and MC‐ICP‐MS, respectively). Our results also show that the first‐ and second‐generation USGS reference materials have homogeneous Sr and Nd isotopic compositions. Nd isotopic compositions by MC‐ICP‐MS and TIMS agree to within 15 ppm for all reference materials. Interlaboratory MC‐ICP‐MS comparisons show excellent agreement for Pb isotopic compositions; however, the reproducibility is not as good as for Sr and Nd. A careful, sequential leaching experiment of three first‐ and second‐generation reference materials (BCR, BHVO, AGV) indicates that the heterogeneity in Pb isotopic compositions, and concentrations, could be directly related to contamination by the steel (mortar\u002Fpestle) used to process the materials. Contamination also accounts for the high concentrations of certain other trace elements (e.g., Li, Mo, Cd, Sn, Sb, W) in various USGS reference materials.\u003C\u002Fjats:p>","\u003Cjats:p>Trung tâm Nghiên cứu Đồng vị và Địa hóa Thái Bình Dương (PCIGR) tại Đại học British Columbia đã tiến hành phân tích có hệ thống các thành phần và nồng độ đồng vị (Sr, Nd, và Pb) của một loạt vật liệu tham khảo của Cục Khảo sát Địa chất Hoa Kỳ (USGS), bao gồm basalt (BCR‐1, 2; BHVO‐1, 2), andesite (AGV‐1, 2), rhyolite (RGM‐1, 2), syenite (STM‐1, 2), granodiorite (GSP‐2), và granite (G‐2, 3). Các vật liệu tham khảo đá của USGS đã được đặc trưng hóa địa hóa tốt, nhưng không có phương pháp hệ thống hay cơ sở dữ liệu cho các thành phần đồng vị phóng xạ, ngay cả đối với BCR‐1 thường được sử dụng. Cuộc điều tra này đại diện cho phân tích có hệ thống đầu tiên về thành phần và nồng độ đồng vị của các vật liệu tham khảo USGS và cung cấp một cơ sở dữ liệu quan trọng cho cộng đồng đồng vị. Thêm vào đó, dải thiết bị tại PCIGR, bao gồm máy Plasma MC‐ICP‐MS của Nu Instruments, Triton TIMS của Thermo Finnigan, và Element2 HR‐ICP‐MS của Thermo Finnigan, cho phép đánh giá và so sánh độ chính xác và độ chính xác của các phân tích đồng vị được xác định bởi cả phương pháp TIMS và MC‐ICP‐MS (ví dụ, các thành phần đồng vị Nd). Đối với mỗi vật liệu tham khảo, 5 đến 10 phân tích hoàn toàn lặp lại cung cấp các kết quả đồng vị nhất quán, tất cả với độ chính xác bên ngoài dưới 30 ppm (2 SD) cho các thành phần đồng vị Sr và Nd (27 và 24 ppm đối với TIMS và MC‐ICP‐MS, tương ứng). Kết quả của chúng tôi cũng cho thấy rằng các vật liệu tham khảo thế hệ đầu tiên và thứ hai của USGS có các thành phần đồng vị Sr và Nd đồng nhất. Các thành phần đồng vị Nd bằng MC‐ICP‐MS và TIMS đồng ý trong phạm vi 15 ppm cho tất cả các vật liệu tham khảo. Các so sánh giữa các phòng thí nghiệm MC‐ICP‐MS cho thấy sự đồng nhất tuyệt vời cho các thành phần đồng vị Pb; tuy nhiên, độ tái tạo không tốt bằng cho Sr và Nd. Một thí nghiệm rửa tỉ mỉ, tuần tự ba vật liệu tham khảo thế hệ đầu tiên và thứ hai (BCR, BHVO, AGV) cho thấy tính không đồng nhất trong các thành phần đồng vị Pb và nồng độ có thể liên quan trực tiếp đến ô nhiễm bởi thép (cối\u002F chày) sử dụng để xử lý các vật liệu. Ô nhiễm cũng là nguyên nhân cho nồng độ cao của một số nguyên tố vi lượng khác (ví dụ, Li, Mo, Cd, Sn, Sb, W) trong các vật liệu tham khảo USGS khác nhau.\u003C\u002Fjats:p>",{"EN":3497,"VI":3498},"High‐precision isotopic characterization of USGS reference materials by TIMS and MC‐ICP‐MS","Đặc trưng đồng vị chính xác cao của các vật liệu tham khảo USGS bằng TIMS và MC‐ICP‐MS",{"VI":3500},"",{"VOID":3502},"10.1029\u002F2006gc001283","2024-10-06T03:23:26.761+00:00",[31],[30],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F2006GC001283",[3508,3527,3544,3561,3578,3595,3610,3627,3642,3659,3676,3691,3706],{"id":3509,"sortIndex":32,"researcher":28,"roles":3510,"affiliations":3511,"properties":3520},"5ad14bd4-569f-4733-94dd-1f49503a4f14",[],[3512],{"id":3513,"sortIndex":32,"affiliation":3514,"properties":28},"78c4538f-a608-4886-b94f-7b04f030189e",{"id":3513,"createTime":28,"updateTime":28,"relativeEntities":3515,"slug":28,"properties":3516,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3519,"statistic":28},[],{"title":3517},{"EN":3518},"Pacific Centre for Isotopic and Geochemical Research, Department of Earth and Ocean Sciences University of British Columbia 6339 Stores Road Vancouver, British Columbia Canada V6T 1Z4",[],{"orcid":3521,"title":3523,"openalex":3525},{"VOID":3522},"https:\u002F\u002Forcid.org\u002F0000-0002-6638-5543",{"EN":3524},"Dominique Weis",{"VOID":3526},"A5086662700",{"id":3528,"sortIndex":40,"researcher":28,"roles":3529,"affiliations":3530,"properties":3537},"d18c4496-f48b-4215-886f-ed8eab03acef",[],[3531],{"id":3513,"sortIndex":32,"affiliation":3532,"properties":28},{"id":3513,"createTime":28,"updateTime":28,"relativeEntities":3533,"slug":28,"properties":3534,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3536,"statistic":28},[],{"title":3535},{"EN":3518},[],{"orcid":3538,"title":3540,"openalex":3542},{"VOID":3539},"https:\u002F\u002Forcid.org\u002F0000-0002-2033-4679",{"EN":3541},"Bruno Kieffer",{"VOID":3543},"A5089366249",{"id":3545,"sortIndex":123,"researcher":28,"roles":3546,"affiliations":3547,"properties":3556},"cb7aed2a-292a-43f0-a1af-fa574ac4db36",[],[3548],{"id":3549,"sortIndex":32,"affiliation":3550,"properties":28},"012bd651-bae0-44c8-8b0e-88bca221fef6",{"id":3549,"createTime":28,"updateTime":28,"relativeEntities":3551,"slug":28,"properties":3552,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3555,"statistic":28},[],{"title":3553},{"EN":3554},"Department of Earth and Environmental Sciences UniversitéLibre de Bruxelles  CP 160\u002F02, Avenue F.D. 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One leads to the conclusion that mantle potential temperature (i.e., T\u003Cjats:sub>P\u003C\u002Fjats:sub>) of ambient mantle below oceanic ridges is 1430°C, the same as Hawaii. Another has ridges with a large range in ambient mantle potential temperature (i.e., T\u003Cjats:sub>P\u003C\u002Fjats:sub> = 1300–1570°C), comparable in some cases to hot spots (Klein and Langmuir, 1987; Langmuir et al., 1992). A third has uniformly low temperatures for ambient mantle below ridges, ∼1300°C, with localized 250°C anomalies associated with mantle plumes. All methods involve assumptions and uncertainties that we critically evaluate. A new evaluation is made of parental magma compositions that would crystallize olivines with the maximum forsterite contents observed in lava flows. These are generally in good agreement with primary magma compositions calculated using the mass balance method of Herzberg and O'Hara (2002), and differences reflect the well‐known effects of fractional crystallization. Results of primary magma compositions we obtain for mid‐ocean ridge basalts and various oceanic islands and plateaus generally favor the third type of model but with ambient mantle potential temperatures in the range 1280–1400°C and thermal anomalies that can be 200–300°C above this background. Our results are consistent with the plume model.\u003C\u002Fjats:p>","\u003Cjats:p>Nhiều phương pháp đã được phát triển để đánh giá trạng thái nhiệt của manti dưới các sống núi đại dương, đảo, và cao nguyên, dựa trên thạch học và hóa địa chất của dung nham phun trào. Một phương pháp dẫn đến kết luận rằng nhiệt độ tiềm năng của manti (gọi là T\u003Cjats:sub>P\u003C\u002Fjats:sub>) của manti môi trường dưới các sống núi đại dương là 1430°C, giống như Hawaii. Phương pháp khác cho thấy các sống núi có một phạm vi lớn về nhiệt độ tiềm năng của manti môi trường (gọi là T\u003Cjats:sub>P\u003C\u002Fjats:sub> = 1300–1570°C), so sánh trong một số trường hợp với các điểm nóng (Klein và Langmuir, 1987; Langmuir et al., 1992). Phương pháp thứ ba cho thấy nhiệt độ thấp đồng nhất cho manti môi trường dưới các sống núi, khoảng 1300°C, với các dị thường 250°C có tính điểm liên quan đến các cột manti. Tất cả các phương pháp đều có các giả định và không chắc chắn mà chúng tôi đánh giá phê phán. Một đánh giá mới được thực hiện về thành phần dung nham mẹ có thể kết tinh olivin với hàm lượng forsterit tối đa quan sát thấy ở các dòng chảy dung nham. Những điều này nhìn chung phù hợp với các thành phần dung nham chính được tính bằng phương pháp cân bằng khối lượng của Herzberg và O'Hara (2002), và sự khác biệt phản ánh các hiệu ứng nổi tiếng của sự kết tinh phân đoạn. Kết quả về thành phần dung nham chính mà chúng tôi thu được cho bazan sống núi giữa đại dương và các đảo, cao nguyên đại dương khác nhau nói chung ủng hộ loại mô hình thứ ba nhưng với nhiệt độ tiềm năng của manti môi trường trong phạm vi 1280–1400°C và các dị thường nhiệt có thể vượt trên khoảng nền này từ 200–300°C. Kết quả của chúng tôi phù hợp với mô hình cột manti.\u003C\u002Fjats:p>",{"EN":3904,"VI":3905},"Temperatures in ambient mantle and plumes: Constraints from basalts, picrites, and komatiites","Nhiệt độ trong lớp manti môi trường và các cột nhiệt: Các ràng buộc từ bazan, picrit, và komatiit",{"VI":3500},{"VOID":3908},"10.1029\u002F2006gc001390",[31],[30],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F2006GC001390",[3913,3932,3951,3968,3987,4006,4025,4044],{"id":3914,"sortIndex":32,"researcher":28,"roles":3915,"affiliations":3916,"properties":3925},"133c4709-1bc1-4366-824c-f9d4b99ebcd4",[],[3917],{"id":3918,"sortIndex":32,"affiliation":3919,"properties":28},"efa8f363-0d6a-46cc-95e5-648d33b51aaf",{"id":3918,"createTime":28,"updateTime":28,"relativeEntities":3920,"slug":28,"properties":3921,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3924,"statistic":28},[],{"title":3922},{"EN":3923},"Department of Geological Sciences Rutgers University Piscataway New Jersey USA",[],{"orcid":3926,"title":3928,"openalex":3930},{"VOID":3927},"https:\u002F\u002Forcid.org\u002F0000-0003-4568-826X",{"EN":3929},"Claude Herzberg",{"VOID":3931},"A5067905992",{"id":3933,"sortIndex":40,"researcher":28,"roles":3934,"affiliations":3935,"properties":3944},"e920ed3b-857b-46df-a926-e8071c55b44f",[],[3936],{"id":3937,"sortIndex":32,"affiliation":3938,"properties":28},"b83b1d5a-15b8-4bf9-9d10-0849973424b6",{"id":3937,"createTime":28,"updateTime":28,"relativeEntities":3939,"slug":28,"properties":3940,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3943,"statistic":28},[],{"title":3941},{"EN":3942},"Geological and Planetary Sciences, California Institute of Technology Pasadena California USA",[],{"orcid":3945,"title":3947,"openalex":3949},{"VOID":3946},"https:\u002F\u002Forcid.org\u002F0000-0001-6025-8925",{"EN":3948},"Paul D. 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Geol.in press.",{"doi":4460},"10.1016\u002Fj.chemgeo.2007.01.014",{"id":28,"text":4462,"url":28,"identifiers":4463},"10.1016\u002FS0024-4937(99)00038-9",{"doi":4462},{"id":28,"text":4465,"url":28,"identifiers":4466},"10.1093\u002Fpetrology\u002F41.7.1127",{"doi":4465},{"id":28,"text":4468,"url":28,"identifiers":4469},"10.1007\u002Fs00410-005-0662-y",{"doi":4468},{"id":28,"text":4471,"url":28,"identifiers":4472},"10.1016\u002F0040-1951(79)90334-2",{"doi":4471},{"id":28,"text":4474,"url":28,"identifiers":4475},"10.1016\u002F0012-821X(85)90084-6",{"doi":4474},{"id":28,"text":4477,"url":28,"identifiers":4478},"10.1016\u002F0012-821X(86)90144-5",{"doi":4477},{"id":28,"text":4480,"url":28,"identifiers":4481},"Roberge J., 2004, Origin and Evolution of the Ontong Java Plateau, 239",{},{"id":28,"text":4483,"url":28,"identifiers":4484},"10.1007\u002FBF00371276",{"doi":4483},{"id":28,"text":4486,"url":28,"identifiers":4487},"Sano T., 2004, Origin and Evolution of the Ontong Java Plateau, 185",{},{"id":28,"text":4489,"url":28,"identifiers":4490},"10.2113\u002Fgselements.1.5.259",{"doi":4489},{"id":28,"text":4492,"url":28,"identifiers":4493},"10.1029\u002FGM100p0045",{"doi":4492},{"id":28,"text":4495,"url":28,"identifiers":4496},"10.1038\u002F352397a0",{"doi":4495},{"id":28,"text":4498,"url":28,"identifiers":4499},"10.1016\u002Fj.pepi.2003.09.025",{"doi":4498},{"id":28,"text":4501,"url":28,"identifiers":4502},"10.1126\u002Fscience.1116349",{"doi":4501},{"id":28,"text":4504,"url":28,"identifiers":4505},"10.1016\u002F0016-7037(70)90009-8",{"doi":4504},{"id":28,"text":4507,"url":28,"identifiers":4508},"10.1029\u002F94JB02768",{"doi":4507},{"id":28,"text":4510,"url":28,"identifiers":4511},"10.1093\u002Fpetrology\u002F42.2.321",{"doi":4510},{"id":28,"text":4513,"url":28,"identifiers":4514},"10.1016\u002F0012-821X(95)00203-O",{"doi":4513},{"id":28,"text":4516,"url":28,"identifiers":4517},"Sobolev A. 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Bull., 84, 849, 10.1130\u002F0016-7606(1973)84\u003C849:MMAIBT>2.0.CO;2",{"doi":4563},"10.1130\u002F0016-7606(1973)84\u003C849:MMAIBT>2.0.CO;2",{"id":28,"text":4565,"url":28,"identifiers":4566},"10.1093\u002Fpetrology\u002F12.1.1",{"doi":4565},{"id":28,"text":4568,"url":28,"identifiers":4569},"10.1093\u002Fpetrology\u002F16.1.110",{"doi":4568},{"id":28,"text":4571,"url":28,"identifiers":4572},"10.1007\u002Fs004100050169",{"doi":4571},{"id":28,"text":4574,"url":28,"identifiers":4575},"10.1029\u002F93JB03205",{"doi":4574},{"id":28,"text":4577,"url":28,"identifiers":4578},"Yaxley G. M., 1998, Reactions between eclogite and peridotite: Mantle refertilisation by subduction of oceanic crust, Schweiz. Mineral. Petrogr. Mitt., 78, 243",{},{"id":4580,"createTime":4581,"updateTime":4581,"relativeEntities":4582,"slug":4583,"properties":4584,"entityType":983,"verifyStatus":26,"verifyTime":4581,"verifyNote":984,"languages":4595,"translateLanguages":28,"viewCount":32,"primaryUrl":4596,"fullTextUrl":28,"authors":4597,"publicationType":1007,"publisherRelationship":4670,"citationCount":4722,"citationInfo":4723,"publishDate":4726,"publishYear":4724,"citationAnalyzeStatus":879,"lastCitationAnalyze":28,"indexDatabases":4727,"openAccess":28,"references":4728,"isForceReanalyzing":1650},"808ec6a4-a8db-4a10-a5b2-059877186f59","2024-12-11T01:07:34.950+00:00",[],"The-pMELTS-A-revision-of-MELTS-for-improved-calculation-of-phase-relations-and-major-element-partitioning-related-to-partial-melting-of-the-mantle-to-3-GPa",{"openalex":4585,"mag":4587,"abstract":4589,"title":4591,"doi":4593},{"VOID":4586},"W2099914884",{"VOID":4588},"2099914884",{"EN":4590},"\u003Cjats:p>We describe a newly calibrated model for the thermodynamic properties of magmatic silicate liquid. The new model, pMELTS, is based on MELTS [\u003Cjats:ext-link xmlns:xlink=\"http:\u002F\u002Fwww.w3.org\u002F1999\u002Fxlink\" xlink:href=\"#ggge167-bib-0022\">\u003Cjats:italic>Ghiorso and Sack\u003C\u002Fjats:italic>, 1995\u003C\u002Fjats:ext-link>] but has a number of improvements aimed at increasing the accuracy of calculations of partial melting of spinel peridotite. The pMELTS algorithm uses models of the thermodynamic properties of minerals and the phase equilibrium algorithms of MELTS, but the model for silicate liquid differs from MELTS in the following ways: (1) The new algorithm is calibrated from an expanded set of mineral‐liquid equilibrium constraints from 2439 experiments, 54% more than MELTS. (2) The new calibration includes mineral components not considered during calibration of MELTS and results in 11,394 individual mineral‐liquid calibration constraints (110% more than MELTS). Of these, 4924 statements of equilibrium are from experiments conducted at elevated pressure (200% more than MELTS). (3) The pMELTS model employs an improved liquid equation of state based on a third‐order Birch‐Murnaghan equation, calibrated from high‐pressure sink‐float and shockwave experiments to 10 GPa. (4) The new model employs a revised set of end‐member liquid components. The revised components were chosen to better span liquid composition‐space. Thermodynamic properties of these components are optimized as part of the mineral‐liquid calibration. Comparison of pMELTS to partial melting relations of spinel peridotite from experiments near 1 GPa indicates significant improvements relative to MELTS, but important outstanding problems remain. The pMELTS model accurately predicts oxide concentrations, including SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>, for liquids from partial melting of MM3 peridotite at 1 GPa from near the solidus up to ∼25% melting. Compared to experiments, the greatest discrepancy is for MgO, for which the calculations are between 1 and 4% high. Temperatures required to achieve a given melt fraction match those of the experiments near the solidus but are ∼60°C high over much of the spinel lherzolite melting interval at this pressure. Much of this discrepancy can probably be attributed to overstabilization of clinopyroxene in pMELTS under these conditions. Comparison of pMELTS calculations to the crystallization and partial melting experiments of \u003Cjats:ext-link xmlns:xlink=\"http:\u002F\u002Fwww.w3.org\u002F1999\u002Fxlink\" xlink:href=\"#ggge167-bib-0017\">\u003Cjats:italic>Falloon et al.\u003C\u002Fjats:italic> [1999]\u003C\u002Fjats:ext-link> shows excellent agreement but also suffers from exaggerated calculated stability of clinopyroxene. Finally, comparison of pMELTS calculations to the garnet peridotite experiments of \u003Cjats:ext-link xmlns:xlink=\"http:\u002F\u002Fwww.w3.org\u002F1999\u002Fxlink\" xlink:href=\"#ggge167-bib-0053\">\u003Cjats:italic>Walter\u003C\u002Fjats:italic> [1998]\u003C\u002Fjats:ext-link> at 3–7 GPa reveals disparities between calculations and experiments that increase with pressure. The most prominent of these disparities is manifest as overprediction of the stability of garnet and underprediction of that of olivine. Part of this problem may be attributed to inadequacies in the Birch‐Murnaghan equation of state in reproducing the behavior of highly compressible liquids at high pressures and temperatures.\u003C\u002Fjats:p>",{"EN":4592},"The pMELTS: A revision of MELTS for improved calculation of phase relations and major element partitioning related to partial melting of the mantle to 3 GPa",{"VOID":4594},"10.1029\u002F2001gc000217",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F2001GC000217",[4598,4617,4636,4655],{"id":4599,"sortIndex":32,"researcher":28,"roles":4600,"affiliations":4601,"properties":4610},"d93c1897-7574-4e85-9ba4-5dd80decaed6",[],[4602],{"id":4603,"sortIndex":32,"affiliation":4604,"properties":28},"9b5af69e-54bd-4e4a-983c-d5d953a14e6a",{"id":4603,"createTime":28,"updateTime":28,"relativeEntities":4605,"slug":28,"properties":4606,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4609,"statistic":28},[],{"title":4607},{"VI":4608},"Department of Earth and Space Sciences, University of Washington, Box 351310 Seattle, Washington 98195, USA",[],{"orcid":4611,"title":4613,"openalex":4615},{"VOID":4612},"https:\u002F\u002Forcid.org\u002F0000-0002-0489-0018",{"EN":4614},"M. 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