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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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Papers published involve various aspects of research concerning geosciences and related disciplines, such as stratigraphy, palaeontology, origin and history of the Earth, structural geology, tectonics, mineralogy, petrology, geochemistry, geophysics, geology of mineral deposits, hydrogeology, engineering geology, environmental geology, regional geology and new theories and technologies of geological exploration.","PENDING",[886],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":888,"label":889,"description":891,"parentId":28,"standard":28,"scholarHubFieldId":28},"4cb4a523-c417-4606-9969-2d1fe12ec173",[],{"EN":890},"Geology",{},[893,900],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":895,"slug":28,"properties":896,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":899,"statistic":28},"43d4a537-d044-4372-8544-ca45c3bea38f",[],{"title":897},{"EN":898},"WILEY",[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":902,"slug":28,"properties":903,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":906,"statistic":28},"3ee06008-4db7-4279-a843-ba360bf26e00",[],{"title":904},{"EN":905},"Science Press",[],[908,923],{"id":909,"indexDatabase":910,"url":921,"indexYears":28,"academicFieldIds":922,"indexDatabaseRanking":28},"dc644243-8084-4080-9603-29b2e8c2f413",{"id":911,"createTime":28,"updateTime":28,"relativeEntities":912,"label":913,"description":915,"key":918,"publicationTags":919,"standard":28},"a4921856-b128-4d9f-8f1f-e80813d3bbd4",[],{"EN":914,"VI":914},"ISI\u002FSCIE - Science Citation Index Expanded",{"EN":916,"VI":917},"SCIE database","Cơ sở dữ liệu SCIE","scie",[920,813],"SCIE","https:\u002F\u002Fmjl.clarivate.com\u002Fsearch-results?issn=1000-9515",[816],{"id":924,"indexDatabase":925,"url":930,"indexYears":931,"academicFieldIds":932,"indexDatabaseRanking":934},"f2818393-71b4-4d37-8678-48a3c420e75e",{"id":775,"createTime":28,"updateTime":28,"relativeEntities":926,"label":927,"description":928,"key":781,"publicationTags":929,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],"https:\u002F\u002Fwww.scopus.com\u002Fsourceid\u002F25750","1988-2025",[933],"daacc282-927f-40f0-915e-161403c1fcb7","SCOPUS__Q2","https:\u002F\u002Fonlinelibrary.wiley.com\u002Fjournal\u002F17556724",{"meta":937,"data":939},{"total":938},"19",[940,1108,1436,1832,2337,2600,2825,3025,3302,3619],{"id":941,"createTime":942,"updateTime":942,"relativeEntities":943,"slug":944,"properties":945,"entityType":956,"verifyStatus":884,"verifyTime":957,"verifyNote":958,"languages":959,"translateLanguages":28,"viewCount":32,"primaryUrl":960,"fullTextUrl":28,"authors":961,"publicationType":989,"publisherRelationship":990,"citationCount":826,"citationInfo":1036,"publishDate":1039,"publishYear":1037,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1040,"openAccess":28,"references":1041,"isForceReanalyzing":1107},"770c01ad-5e75-425b-9c93-d092c485a926","2024-12-03T08:34:30.915+00:00",[],"REE-Geochemistry-in-the-Weathered-Crust-of-Granites-Longnan-Area-Jiangxi-Province",{"openalex":946,"mag":948,"abstract":950,"title":952,"doi":954},{"VOID":947},"W1583041281",{"VOID":949},"1583041281",{"EN":951},"\u003Cjats:p>\u003Cjats:bold>Abstract\u003C\u002Fjats:bold> Warm and humid climate and gentle hilly topography have provided favourable conditions for the development of the weathering crust of the granite intrusions in the Longnan area, Jiangxi Province. REE is mostly concentrated in an adsorption state in clay in the wholly weathered zone. The rare‐earth minerals enriched in the parent rocks provided the source material for the REE enrichment. Exchangeable REE accounts for 48‐86%. Extraction experiments and stable isotopic study of clay minerals suggest that the downward infiltration of meteoric water and increasing gradient of pH values have played an important role in the enrichment of REE during the progressive weathering. Slight fractionation of individual REE can not change their distribution patterns in the profiles, which are inherited from the parent rocks.\u003C\u002Fjats:p>",{"EN":953},"REE Geochemistry in the Weathered Crust of Granites, Longnan Area, Jiangxi Province",{"VOID":955},"10.1111\u002Fj.1755-6724.1990.mp3002006.x","PUBLICATION","2024-12-03T08:34:30.914+00:00","Author affiliation is blank",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1755-6724.1990.mp3002006.x",[962,971,980],{"id":963,"sortIndex":32,"researcher":28,"roles":964,"affiliations":965,"properties":966,"displayName":968,"givenName":28,"familyName":28},"4d6e75b9-3591-4ba4-8980-deb0053ff8cf",[],[],{"title":967,"openalex":969},{"EN":968},"Wu Chengyu",{"VOID":970},"A5111859256",{"id":972,"sortIndex":40,"researcher":28,"roles":973,"affiliations":974,"properties":975,"displayName":977,"givenName":28,"familyName":28},"d9151247-b3c0-4fa6-b65d-abac5c4f4c45",[],[],{"title":976,"openalex":978},{"EN":977},"Huang Dianhao",{"VOID":979},"A5085689253",{"id":981,"sortIndex":123,"researcher":28,"roles":982,"affiliations":983,"properties":984,"displayName":986,"givenName":28,"familyName":28},"850c15c6-e24d-4a48-89be-629b1255b215",[],[],{"title":985,"openalex":987},{"EN":986},"Guo Zhongxun",{"VOID":988},"A5037869387","ARTICLE",{"url":28,"publisher":991,"properties":1029},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":992,"slug":872,"properties":993,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":998,"manageAffiliations":1003,"indexDatabases":1014,"url":935,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":994,"eissn":995,"issn":996,"title":997},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[999],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1000,"label":1001,"description":1002,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1004,1009],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1005,"slug":28,"properties":1006,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1008,"statistic":28},[],{"title":1007},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1010,"slug":28,"properties":1011,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1013,"statistic":28},[],{"title":1012},{"EN":905},[],[1015,1022],{"id":909,"indexDatabase":1016,"url":921,"indexYears":28,"academicFieldIds":1021,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1017,"label":1018,"description":1019,"key":918,"publicationTags":1020,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[816],{"id":924,"indexDatabase":1023,"url":930,"indexYears":931,"academicFieldIds":1028,"indexDatabaseRanking":934},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1024,"label":1025,"description":1026,"key":781,"publicationTags":1027,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[933],{"issue":1030,"pages":1032,"volume":1034},{"VOID":1031},"2",{"VOID":1033},"193-209",{"VOID":1035},"3",{"total":826,"publishYear":1037,"statisticByYear":1038},1990,{"2012":40,"2013":42,"2014":46,"2015":45,"2016":49,"2017":45,"2018":48,"2019":48,"2020":49,"2021":46,"2022":48,"2023":46,"2024":48},"1990-06-01",[934,920],[1042,1045,1048,1051,1054,1057,1060,1063,1066,1069,1072,1075,1078,1081,1084,1087,1090,1093,1096,1099,1102,1105],{"id":28,"text":1043,"url":28,"identifiers":1044},"Anderson M., 1981, Adsorptrion of inorganics at the solid‐liquid interface, 357",{},{"id":28,"text":1046,"url":28,"identifiers":1047},"10.1016\u002F0022-1902(79)80145-1",{"doi":1046},{"id":28,"text":1049,"url":28,"identifiers":1050},"Department of Sciences and Technology, Ministry of Geology and Mineral Resources, 1984, Determination of physical and chemical properties of bentonites‐ Tentative standardized methods, 15",{},{"id":28,"text":1052,"url":28,"identifiers":1053},"Drever J. I., 1982, The geochemistry of natural waters, 388",{},{"id":28,"text":1055,"url":28,"identifiers":1056},"10.1016\u002F0009-2541(80)90102-3",{"doi":1055},{"id":28,"text":1058,"url":28,"identifiers":1059},"Fleet A. J., 1984, Aqueous and sedimentary geochemistry of the rare earth elements, in Rare elements geochemistry: developments in geochemistry 2, 343",{},{"id":28,"text":1061,"url":28,"identifiers":1062},"Henderson P, 1984, Rare earth elements geochemistry: developments in geochemistry 2, 510",{},{"id":28,"text":1064,"url":28,"identifiers":1065},"10.1111\u002Fj.1755-6724.1989.mp2002004.x",{"doi":1064},{"id":28,"text":1067,"url":28,"identifiers":1068},"10.1038\u002F279206a0",{"doi":1067},{"id":28,"text":1070,"url":28,"identifiers":1071},"10.1016\u002F0009-2541(74)90066-7",{"doi":1070},{"id":28,"text":1073,"url":28,"identifiers":1074},"10.1016\u002F0016-7037(70)90149-3",{"doi":1073},{"id":28,"text":1076,"url":28,"identifiers":1077},"10.1071\u002FSR9760043",{"doi":1076},{"id":28,"text":1079,"url":28,"identifiers":1080},"Yunhu Song, 1982, Discussion on clay minerais occurring in the weathering crust of a certain acid volcanic rock in Jiangxi Province and their formation conditions, Acta Mineralogica Sinica, 207",{},{"id":28,"text":1082,"url":28,"identifiers":1083},"Yunhu Song, 1986, REE geochemistry of the weathered crust of acid volcanic rocks‐ an experimental study, Geochimica, 225",{},{"id":28,"text":1085,"url":28,"identifiers":1086},"Sudo Toshio, 1981, Clay Mineralogy, 532",{},{"id":28,"text":1088,"url":28,"identifiers":1089},"Xianjue Wang, 1980, An experimental investigation on the REE weathering crust of granites in South China, Scientific Papers on Geology for International Exchange (2), Prepared for 26th International Congress, 139",{},{"id":28,"text":1091,"url":28,"identifiers":1092},"10.1007\u002F978-3-642-67041-1",{"doi":1091},{"id":28,"text":1094,"url":28,"identifiers":1095},"Yueqing Yang, 1981, Geological characteristics of mineralization of rare earth deposits of the iron‐ adsorption type and their prospecting direction, Bulletin of Institute of Mineral Deposits, Chinese Academy of Geological Sciences, 2, 102",{},{"id":28,"text":1097,"url":28,"identifiers":1098},"Zhuming Yang, 1987, A study on clay minerals from the REE‐rich weathered crust developed on the Longnan granite, Jiangxi Province, Scientia Geologica Sinica, 70",{},{"id":28,"text":1100,"url":28,"identifiers":1101},"Shuhui Zheng, 1983, Study on hydrogen and oxygen stable isotopes of meteoric waters, China, Kexue Tongbao, 28, 801",{},{"id":28,"text":1103,"url":28,"identifiers":1104},"",{},{"id":28,"text":1103,"url":28,"identifiers":1106},{},false,{"id":1109,"createTime":1110,"updateTime":1110,"relativeEntities":1111,"slug":1112,"properties":1113,"entityType":956,"verifyStatus":26,"verifyTime":1124,"verifyNote":1125,"languages":1126,"translateLanguages":28,"viewCount":32,"primaryUrl":1127,"fullTextUrl":28,"authors":1128,"publicationType":989,"publisherRelationship":1261,"citationCount":599,"citationInfo":1307,"publishDate":1310,"publishYear":1308,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1311,"openAccess":28,"references":1312,"isForceReanalyzing":1107},"1caec2ac-35e2-4c9d-bc3a-b5992dddfe5f","2024-09-12T05:44:13.483+00:00",[],"Current-Knowledge-of-Mesozoic-Coleoptera-from-Daohugou-and-Liaoning-Northeast-China-",{"openalex":1114,"mag":1116,"abstract":1118,"title":1120,"doi":1122},{"VOID":1115},"W1963498212",{"VOID":1117},"1963498212",{"EN":1119},"\u003Cjats:title>Abstract:\u003C\u002Fjats:title>\u003Cjats:p>The present paper is devoted to an overview on fossil Coleoptera studied from Inner Mongolia, Daohugou (Middle Jurassic, Jiulongshan Formation) and Liaoning (Upper Jurassic‐Lower Cretaceous, Yixian Formation) deposited in Chinese collections. As a result, species of the tribe Sperchopsini and Hydrophilini from Hydrophilidae, families and subfamilies Silphidae, Syndesinae from Lucanidae, Pleocomidae, Trogidae, Trogissitidae, Pyrochroidae, Diaperinae from Tenebrionidae, and Cerambycidae were first registered in the Mesozoic and some families were defined as new. It was shown that many superfamilies represented in the Recent Fauna were formed within the Middle Jurassic and Lower Cretaceous. The materials examined confirm the hypothesis that Cucujiformian beetles are a younger group than other infraordera of Polyphaga (Staphyliniformia and Elateriformia) and, therefore, they appeared in the fossil record only in the late Mesozoic. It was shown and confirmed that most superfamilies appeared in the fossil records before Cucujoidea. The synonymy of \u003Cjats:italic>Notocupes\u003C\u002Fjats:italic> Ponomarenko, 1964; \u003Cjats:italic>Sinocupes\u003C\u002Fjats:italic> Lin, 1976, syn. nov.; \u003Cjats:italic>Amblomma\u003C\u002Fjats:italic> Tan, Ren et Liu 2005, syn. nov.; \u003Cjats:italic>Euryomma\u003C\u002Fjats:italic> Tan, Ren et Shih, 2006, syn. nov., non Stein, 1899 and \u003Cjats:italic>Ovatocupes\u003C\u002Fjats:italic> Tan et Ren, 2006, syn. nov.; synonymy of \u003Cjats:italic>Tetraphalerus\u003C\u002Fjats:italic> Waterhouse, 1901 and \u003Cjats:italic>Odontomma\u003C\u002Fjats:italic> Tan, Ren et Ge 2006, syn. nov.; and synonymy of \u003Cjats:italic>Priacmopsis\u003C\u002Fjats:italic> Ponomarenko, 1966 and \u003Cjats:italic>Latocupes\u003C\u002Fjats:italic> Tan et Ren, 2006, syn. nov. are proposed. \u003Cjats:italic>Sinorhombocoleus papposus\u003C\u002Fjats:italic> Tan et Ren, 2009 is transferred from the family Rhombocoleidae to Schizophoridae. \u003Cjats:italic>Cervicatinius complanus\u003C\u002Fjats:italic> Tan, Ren et Shih, 2007 and \u003Cjats:italic>Forticatinius elegans\u003C\u002Fjats:italic> Tan, Ren et Shih, 2007 are transferred from the family Catiniidae (suborder Archostemata) to superfamily Cleroidea (suborder Polyphaga: first among the family Peltidae and second as a closely related group to the latter family). The family Parandrexidae is transferred from the superfamily Cucujoidea to Cleroidea. The ecological circumstances of the past ecosystems and hypotheses of historical development of the order Coleoptera are discussed. The age of faunas examined is considered. The list of the taxa described from Daohugou and Liaoning is compiled.\u003C\u002Fjats:p>",{"EN":1121},"Current Knowledge of Mesozoic Coleoptera from Daohugou and Liaoning (Northeast China)",{"VOID":1123},"10.1111\u002Fj.1755-6724.2010.00253.x","2024-09-12T05:44:13.480+00:00","Auto Verify",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1755-6724.2010.00253.x",[1129,1156,1179,1204,1221,1244],{"id":1130,"sortIndex":32,"researcher":28,"roles":1131,"affiliations":1132,"properties":1149,"displayName":1153,"givenName":28,"familyName":28},"028116d8-402a-4966-912d-bb1588cffc8e",[],[1133,1141],{"id":1134,"sortIndex":32,"affiliation":1135,"properties":28},"1441a838-911f-4dba-9919-85096e90706a",{"id":1134,"createTime":28,"updateTime":28,"relativeEntities":1136,"slug":28,"properties":1137,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1140,"statistic":28},[],{"title":1138},{"VI":1139},"College of Life Science, Capital Normal University, Beijing, 100048, China",[],{"id":1142,"sortIndex":40,"affiliation":1143,"properties":28},"8e12f9f2-92e7-4073-859a-0e5db9d117be",{"id":1142,"createTime":28,"updateTime":28,"relativeEntities":1144,"slug":28,"properties":1145,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1148,"statistic":28},[],{"title":1146},{"VI":1147},"Zoological Institute of the Russian Academy of Sciences, St. Petersburg 199034, Russia",[],{"orcid":1150,"title":1152,"openalex":1154},{"VOID":1151},"https:\u002F\u002Forcid.org\u002F0000-0002-8826-0258",{"EN":1153},"Alexander G. 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The complex is composed of various high‐grade and multiply deformed rocks, including gray gneiss, basic granulite, amphibolite, fine‐grained gneiss and marble, metamorphosed to upper amphibolite or granulite facies. It can be divided into four rock units: the Fuping TTG gneisses, Longquanguan augen gneisses, Wanzi supracrustals, and Nanying granitic gneisses. U‐Pb age and Hf isotope compositions of about 200 detrital zircons from the Wanzi supracrustals of the Fuping Complex have been analyzed. The data on metamorphic zircon rims give ages of 1.82‐1.84 Ga, corresponding to the final amalgamation event of the NCC, whereas the data for igneous zircon cores yield two age populations at ∼2.10 and ∼2.51 Ga, with some inherited ages scattering between 2.5 and 2.9 Ga. These results suggest that the Wanzi supracrustals were derived from the Fuping TTG gneisses (∼2.5 Ga) and the Nanying granitic gneisses (2.0–2.1 Ga) and deposited between 2.10 and 1.84 Ga. All zircons with ∼2.51 Ga age have positive initial ∍\u003Cjats:sub>Hf\u003C\u002Fjats:sub> values from +1.4 to +10.9, suggesting an important crustal growth event at ∼2.5 Ga through the addition of juvenile materials from the mantle. The Hf isotope data for the detrital zircons further imply that the 2.8 Ga rocks are important components in the lower crust, which is consistent with a suggestion from Nd isotope data for the Eastern Block. The zircons of 2.10 Ga population have initial ∍\u003Cjats:sub>Hf\u003C\u002Fjats:sub> values of −4.9 to +6.1, interpreted as mixing of crustal re‐melt with minor juvenile material contribution at 2.1 Ga. 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Based on the studies on the Lower Triassic of Chaohu, (1) a continuous conodont zonation is established, which has become an important reference for Lower Triassic stratigraphic correlation over the world; (2) the First Appearance Datum of conodont \u003Cjats:italic>Neospathodus waageni\u003C\u002Fjats:italic> was suggested and has been basically accepted as the primary marker to define the Induan‐Olenekian boundary; (3) a characteristic Lower Triassic excursion of carbon isotopes was brought to light and has been proven to be not only an excellent index for the stratigraphic correlation but also a unique indication for the perturbation of ecological environments in the aftermath of the end‐Permian mass extinction; (4) a magnetostratigraphic sequence is constituted with a certain biostratigraphic control in the low‐latitude region and it presents an important correlation to the Boreal sequence; (5) a cyclostratigraphic study provides an alternative method to constrain the age of the chronostratigraphic units; and (6) a scheme of the Olenekian subdivision is recently suggested to define the boundary between the Smithian and Spathian Substages. In addition, Chaohu is also the type locality of the Chaohuan Stage, the upper stage of the Lower Triassic in the China Chronostratigraphic System. Thus, the Lower Triassic of Chaohu is not only a classic sequence in South China, but also a key reference sequence to the investigation of the corresponding stratigraphy and geological events over the world. The recent achievements are viewed here for an overall understanding of the sequence. Then the current situation of the Induan‐Olenekian and Smithian‐Spathian boundaries is discussed to provide a reference for later works.\u003C\u002Fjats:p>",{"EN":2350},"Lower Triassic and Induan‐Olenekian Boundary in Chaohu, Anhui Province, South 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new tetrapod burrow casts from the Naobaogou Formation (Middle or Late Permian) of Nei Mongol, China are described. It marks the first pre‐Cenozoic tetrapod burrow from China, and one of the earliest records of tetrapod burrows. Comparison to other Permian and Triassic burrows suggests that these burrows were created by tetrapod slightly smaller than \u003Cjats:italic>Lystrosaurus\u003C\u002Fjats:italic>. Deduced from the morphology and sizes of two burrows and known tetrapods of the Naobaogou Formation, the burrow should be the production of a therapsid, most likely a dicynodon. These burrows indicate a seasonal climate and this area was semiarid or arid during that time.\u003C\u002Fjats:p>",{"EN":2838},"Large Tetrapod Burrows from the Permian Naobaogou Formation of the Daqingshan Area, Nei Mongol, China",{"VOID":2840},"10.1111\u002F1755-6724.12154","2024-09-21T18:26:08.306+00:00",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002F1755-6724.12154",[2845,2864],{"id":2846,"sortIndex":32,"researcher":28,"roles":2847,"affiliations":2848,"properties":2857,"displayName":2861,"givenName":28,"familyName":28},"413df424-c13b-4bf8-8a31-a14094cf8282",[],[2849],{"id":2850,"sortIndex":32,"affiliation":2851,"properties":28},"2ebd36f8-1de4-4464-ade5-29172a043753",{"id":2850,"createTime":28,"updateTime":28,"relativeEntities":2852,"slug":28,"properties":2853,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2856,"statistic":28},[],{"title":2854},{"VI":2855},"Key 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It contains the Yunmengshan batholith, which is dominated by two plutons: the Yunmengshan gneissic granite and the Shicheng gneissic diorite. Four samples of the Yunmengshan gneissic granite give SHRIMP zircon U–Pb ages from 145 to 141 Ma, whereas four samples of the Shicheng gneissic diorite have ages from 159 Ma to 151 Ma. Dikes that cut the Yunmengshan diorite record SHRIMP zircon U–Pb age of 162±2 and 156±4 Ma. The cumulative plots of zircons from the diorites show a peak age of 155 Ma, without inherited zircon cores, and the peak age of 142 Ma for granite is interpreted as the emplacement age of the Yunmengshan granitic pluton, whose igneous zircons contain inherited zircon cores. 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experimental data, this paper proposes that the generation of secondary biogenic gas (SBG) and its mixing of with the residual thermogenic gas at an early stage inevitably lead to secondary changes of the thermogenic gas and various geochemical additive effects. Experimental results also show that the fractionation of the carbon isotope of methane of coal core desorption gas changes very little; the δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sub>1\u003C\u002Fjats:sub> value of the mixed gas of biogenic and thermogenic gases is between the δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sub>1\u003C\u002Fjats:sub> values of the two “original” gases, and the value is determined by the carbon isotopic compositions and mixing proportions of the two “original” methanes. Therefore this paper proposes that the study on the secondary changes of the thermogenic gas and various additive effects is a new effective way to study and identify SBG. Herein, a systematic example of research on the coalbed gas (Huainan coalbed gas) is further conducted, revealing a series of secondary changes and additive effects, the main characteristics and markers of which are: (1) the contents of CO\u003Cjats:sub>2\u003C\u002Fjats:sub> and heavy‐hydrocarbons decrease significantly; (2) the content of CH\u003Cjats:sub>4\u003C\u002Fjats:sub> increases and the gas becomes drier; (3) the δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C and δD values of methane decrease significantly and tend to have biogenetic characteristics; and (4) the values of δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sub>2\u003C\u002Fjats:sub> and δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sc>co\u003C\u002Fjats:sc>\u003Cjats:sub>2\u003C\u002Fjats:sub> grow higher. These isotopic values also change with the degradation degrees by microbes and mixing proportions of the two kinds of gases in different locations. There exists a negative correlation between the δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sub>1\u003C\u002Fjats:sub>\u003Cjats:italic>vs\u003C\u002Fjats:italic>δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sc>co\u003C\u002Fjats:sc>\u003Cjats:sub>2\u003C\u002Fjats:sub> values. The Δδ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sc>c\u003C\u002Fjats:sc>\u003Cjats:sub>2\u003C\u002Fjats:sub>–\u003Cjats:sc>c\u003C\u002Fjats:sc>\u003Cjats:sub>1\u003C\u002Fjats:sub> values obviously become higher. The distributions of the Δδ\u003Cjats:sup>13\u003C\u002Fjats:sup>C\u003Cjats:sc>co\u003C\u002Fjats:sc>\u003Cjats:sub>2\u003C\u002Fjats:sub>–\u003Cjats:sc>c\u003C\u002Fjats:sc>\u003Cjats:sub>1\u003C\u002Fjats:sub> values are within certain limits and show regularity. There exist a positive correlation between the N\u003Cjats:sub>2\u003C\u002Fjats:sub> versus Ar contents, and a negative correlation between the N\u003Cjats:sub>2\u003C\u002Fjats:sub> versus CH\u003Cjats:sub>4\u003C\u002Fjats:sub> contents, indicating the down forward infiltration of the surface water containing air. These are important markers of the generation and existence of SBG.\u003C\u002Fjats:p>",{"EN":3315},"New Approaches and Markers for Identifying Secondary Biogenic Coalbed Gas",{"VOID":3317},"10.1111\u002Fj.1755-6724.2012.00622.x",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1755-6724.2012.00622.x",[3321,3340,3355,3380,3395,3412,3429,3444,3459],{"id":3322,"sortIndex":32,"researcher":28,"roles":3323,"affiliations":3324,"properties":3333,"displayName":3337,"givenName":28,"familyName":28},"7fa42e2f-9efa-4ab0-b0fa-e5f6e7e4b745",[],[3325],{"id":3326,"sortIndex":32,"affiliation":3327,"properties":28},"c38d1e44-2d84-4fe6-aa0f-8ee2b66904a4",{"id":3326,"createTime":28,"updateTime":28,"relativeEntities":3328,"slug":28,"properties":3329,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3332,"statistic":28},[],{"title":3330},{"EN":3331},"College of Resource Science and 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