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other provinces and regions in Vietnam and other country.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Address\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Headquarters of Can Tho Journal of Medicine and Pharmacy, located Scientific Research and International Cooperation Office: 179 Nguyen Van Cu Street, An Khanh Ward, Ninh Kieu District, Can Tho City, Vietnam.\u003C\u002Fspan>\u003C\u002Fp>","\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Ngày 16\u002F7\u002F2015, Tạp chí Y Dược học Cần Thơ được cấp chỉ số quốc tế: ISSN 2354-1210.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 4\u002F2016, Tạp chí đã được Hội đồng Giáo sư ngành Y đưa vào danh sách các tạp chí khoa học Y học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Năm 2020 Tạp chí Y Dược học Cần Thơ đã được phê duyệt vào danh mục của các Hội đồng Giáo sư ngành Dược học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ ra 12 số\u002Fnăm, 180-200 trang\u002Fsố.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 12\u002F2022 Tạp chí Y Dược học Cần Thơ là thành viên của hệ thống Crossref và từ tháng 01\u002F2023 tạp chí thực hiện bình duyệt online kín 2 chiều nhằm tăng tính minh bạch, tin cậy của các công trình nghiên cứu khoa học và đảm bảo tốt nhất chất lượng khoa học của bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ, mục đích và phạm vi của tạp chí\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ và mục đích hoạt động của tạp chí: xuất bản nhằm mục đích phổ biến kết quả từ các đề tài nghiên cứu khoa học; giao lưu trao đổi khoa học, chia sẻ kinh nghiệm, học tập, đồng thời cập nhật thông tin khoa học mới trong các lĩnh vực y, sinh, dược học trong và ngoài nước.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phạm vi của tạp chí: Tạp chí xuất bản được chia thành 3 chuyên mục: (i) Bài báo nghiên cứu khoa học là kết quả công trình nghiên cứu khoa học có giá trị đã được triển khai nghiên cứu, (ii) Bài tổng quan y, sinh, dược học: phục vụ mục tiêu đào tạo liên tục trong lĩnh vực y, sinh, dược học; nhằm hệ thống hóa những kiến thức kinh điển và hiện đại; (iii) Thông tin cập nhật kiến thức mới về y, sinh, dược học trong nước và trên thế giới.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Chính sách truy cập mở\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ áp dụng chính sách truy cập mở đối với các bài báo đã xuất bản đến với độc giả, nhằm mở rộng cơ hội tiếp cận các kết quả nghiên cứu chất lượng cao và tăng cường trao đổi kiến thức. Tạp chí đăng tải trực tuyến (miễn phí) toàn văn các bài báo được công bố trên website của Tạp chí (https:\u002F\u002Ftapchi.ctump.edu.vn).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đạo đức xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ cam kết tuân thủ đạo đức xuất bản phù hợp với các hướng dẫn và tiêu chuẩn của the Committee on Publication Ethics (COPE), tuân thủ các nguyên tắc của COPE’s Core Practices, Best Practices Guidelines for Journal Editors và Guidelines on Good Publication Practices.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Bản thảo bài báo chỉ được chấp nhận khi được tác giả chịu trách nhiệm chính cam kết các nội dung sau: Các nội dung của bản thảo chưa được đăng tải toàn bộ hoặc một phần ở các tạp chí khác; Tất cả các tác giả đều có đóng góp một cách đáng kể vào quá trình nghiên cứu hoặc chuẩn bị bản thảo và cùng chịu trách nhiệm về các nội dung của bản thảo; Tuân thủ các biện pháp đảm bảo đạo đức nghiên cứu (ví dụ thỏa thuận đồng ý tham gia nghiên cứu).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Cam kết bảo mật\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí cam kết thực hiện và tuân thủ các quy định của luật và các văn bản hướng dẫn liên quan đến bảo mật thông tin cá nhân trên không gian mạng. Các thông tin mà người dùng (tác giả, độc giả, biên tập viên, người phản biện) nhập vào các biểu mẫu trên Hệ thống Quản lý xuất bản trực tuyến của tạp chí chỉ được sử dụng vào các mục đích đã được tuyên bố rõ ràng và sẽ không được cung cấp cho bất kỳ bên thứ ba nào khác, hay dùng vào bất kỳ mục đích nào khác.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phí gửi bài\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng bài: 1.000.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng nhanh: 1.500.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với tác giả là cán bộ viên chức thuộc Trường Đại học Y Dược Cần Thơ thì được hỗ trợ 50% lệ phí gửi đăng bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với sinh viên thực hiện đề tài nghiên cứu khoa học cấp trường được hỗ trợ 100% lệ phí đăng bài ( Tác giả gửi đính kèm “ Quyết định về việc giao tổ chức thực hiện đề tài nghiên cứu khoa học cấp Trường của sinh viên”).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Hình thức nộp lệ phí:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Tiền mặt:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Nộp trực tiếp tại Phòng Tài chính - Kế toán, Trường Đại học Y Dược Cần Thơ, số 179 Nguyễn Văn Cừ, P. An Khánh, Q. Ninh Kiều, thành phố Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Chuyển khoản:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tên Tài khoản: Trường ĐHYD Cần Thơ, Số TK: 0111000115668, tại ngân hàng Vietcombank chi nhánh Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Thời gian: Áp dụng từ ngày 01\u002F02\u002F2023.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">* Phí gửi bài không được hoàn trả khi bài viết bị từ chối hoặc tác giả xin rút bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Quy trình phản biện bài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ thực hiện quy trình phản biện kín hai chiều nghiêm ngặt. Danh tính của những người phản biện không được tiết lộ cho các tác giả và ngược lại. Quy trình thẩm định bài báo đăng gồm các bước sau:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tiếp nhận bản thảo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tác giả liên hệ gửi bản thảo đến Tạp chí qua hệ thống trực tuyến tại website: https:\u002F\u002Ftapchi.ctump.edu.vn. Hướng dẫn về cách đăng ký, gửi bài và chuẩn bị bản thảo được cung cấp trên website của Tạp chí.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sàng lọc sơ bộ\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sau khi Tòa soạn nhận được bài báo của tác giả, Ban Thư ký sẽ tiến hành kiểm tra sơ bộ bài báo (các yêu cầu về nội dung và hình thức). Những bài báo không đúng quy cách hoặc có nội dung không phù hợp hoặc vi phạm bản quyền sẽ bị từ chối (Ban Thư ký thông báo phản hồi đến tác giả trong vòng 1 tuần). Những bài báo đủ điều kiện, được Ban Thư ký tòa soạn chuyển đến Ban Biên tập có cùng chuyên môn với nội dung bài báo để đề xuất người phản biện. Thời gian kể từ khi Ban Biên tập nhận bài báo đến khi đề xuất người phản biện bài báo chậm nhất là 5 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Vòng phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký gửi bài và yêu cầu phản biện đến 02 phản biện độc lập.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Các phản biện gởi nhận xét cho Ban Thư ký. Thời gian từ khi gửi bài cho phản biện đến khi nhận ý kiến của phản biện tối đa là 20 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xử ký kết quả phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Nếu ý kiến đồng ý cho đăng và không cần chỉnh sửa, Ban Thư ký tiếp tục đăng bài theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Nếu ý kiến đồng ý đăng và cần chỉnh sửa, Ban Thư ký sẽ thông tin đến tác giả chỉnh sửa theo yêu cầu của người phản biện. Thời gian chỉnh sửa và gửi lại kéo dài không quá 2 tuần, từ khi tác giả bài báo nhận được thông tin (Quá trình này có thể lặp lại tối đa 2 lần\u002F1 bài báo). Khi có sự thống nhất, đồng ý của người phản biện; bài báo được tiếp tục đăng theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Những bài báo có chất lượng không đạt yêu cầu, cả 2 phản biện không đồng ý cho đăng sẽ bị Tòa soạn từ chối đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký tổng hợp các bản thảo đã được tác giả hoàn thiện sau thẩm định trình Ban Biên tập xem xét, Tổng Biên tập phê duyệt, quyết định bài đăng theo các tiêu chí: sự phù hợp nội dung với tôn chỉ và mục đích, thể loại bài viết (ưu tiên các bài có bài có nghiên cứu chuyên sâu, hàm lượng khoa học cao), đóng góp mới bài báo, bài báo được ưu tiên đăng trong số gần nhất của Tạp chí theo thứ tự: tính thời sự, chất lượng bài báo và thời gian gửi bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Ban Biên tập và Ban Thư ký biên tập bản thảo, chế bản, đọc rà soát lỗi. Thời gian hoàn thành từ 10-15 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Ban Thư ký có trách nhiệm thông báo cho tác giả bài báo (bằng e-mail) về tình hình phê duyệt bài báo, thời gian, số kỳ, tập xuất bản bài báo theo qui định.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">4. 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The main objectives of the journal include: providing an intellectual platform for Vietnamese and international scholars; promoting interdisciplinary studies in social sciences and humanities; becoming the leading journal in social sciences and humanities in Vietnam; being indexed by worldwide databases and having academic recognition internationally in the near future.\\nThe journal is currently indexed by Google Scholar, WorldCat, Open Archives, Cosmos Impact Factor, Advanced Sciences Index, Scientific Indexing Services, CrossRef, EBSCO Information Services and Vietnam National University’s digital archive.\\n\"},{\"attributes\":{\"bold\":true},\"insert\":\"Journal of Social Sciences and Humanities-Vietnam\"},{\"insert\":\"\\n\"},{\"attributes\":{\"bold\":true},\"insert\":\"ISSN 2354-1172, email: tapchikhxhnv@gmail.com, tckhxhnv@vnu.edu.vn\"},{\"insert\":\"\\n\"}]}","{\"ops\":[{\"insert\":\"Được thành lập ngày 31\u002F8\u002F2015 (giấy phép hoạt động số 155\u002FGP-BVHTT ngày 11 tháng 5 năm 2015 của Bộ Thông tin và Truyền thông, mã số tiêu chuẩn quốc tế ISSN 2354-1172), Tạp chí Khoa học Xã hội và Nhân văn (Journal of Social Sciences and Humanities) là ấn phẩm khoa học chính thức, duy nhất của Trường Đại học Khoa học Xã hội và Nhân văn, ĐHQG Hà Nội, phát triển và kế thừa Chuyên san Khoa học Xã hội và Nhân văn, Tạp chí Khoa học, ĐHQG Hà Nội.\\nTạp chí xuất bản định kỳ (04 số tiếng Việt\u002Fnăm và 02 số tiếng Anh\u002Fnăm), có nhiệm vụ \"},{\"attributes\":{\"italic\":true},\"insert\":\"công bố, giới thiệu các công trình nghiên cứu khoa học khoa học xã hội và nhân văn của các tác giả là các nhà khoa học trong và ngoài nước, phục vụ giảng dạy, học tập và nghiên cứu khoa học\"},{\"insert\":\". Hội đồng biên tập của Tạp chí hiện bao gồm 33 nhà khoa học có uy tín trong nước và quốc tế. Tạp chí tập trung và ưu tiên đăng tải những bài báo theo định hướng của tinh thần cởi mở, sáng tạo, nhanh chóng vươn lên để tiếp cận và sánh ngang với các tạp chí có uy tín hàng đầu của khu vực và trên thế giới. Nội dung chính của Tạp chí bao gồm các Bài nghiên cứu (khoảng 6000 đến 15000 từ), các bài điểm sách, thông tin khoa học (khoảng 300 đến 1500 từ) được trình bày theo đúng cấu trúc và chuẩn mực của một tạp chí khoa học.\\nCác bài viết của Tạp chí hiện đang được trích dẫn bởi Google Scholar, WorldCat, Open Archives, Cosmos Impact Factor, Advanced Sciences Index, Scientific Indexing Services, CrossRef, EBSCO Information Services.\\nMọi thông tin xin liên hệ: \"},{\"attributes\":{\"italic\":true},\"insert\":\"Phòng Tạp chí, 701 - E, Trường Đại học Khoa học Xã hội và Nhân văn, 336 Nguyễn Trãi, Thanh Xuân, Hà Nội. ĐT: 024.35581984; email: tckhxhnv@vnu.edu.vn \"},{\"insert\":\"hoặc \"},{\"attributes\":{\"italic\":true},\"insert\":\"tapchikhxhnv@gmail.com \"},{\"insert\":\"\\n\"}]}",{"EN":494,"VI":495},"VNU Journal of Social Sciences and Humanities","Tạp chí Khoa học Xã hội và Nhân văn",[101,102],[],[499],{"id":500,"createTime":501,"updateTime":502,"relativeEntities":503,"slug":504,"properties":505,"entityType":98,"verifyStatus":25,"verifyTime":509,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":222,"url":26,"parentIds":510,"statistic":511},"8b6e349b-0daf-4895-9c3f-85f30f1bfd42","2023-07-31T12:55:58.430+00:00","2026-06-19T02:30:07.899+00:00",[],"Tr%C6%B0%E1%BB%9Dng-%C4%90%E1%BA%A1i-h%E1%BB%8Dc-Khoa-h%E1%BB%8Dc-X%C3%A3-h%E1%BB%99i-v%C3%A0-Nh%C3%A2n-v%C4%83n-%C4%90%E1%BA%A1i-h%E1%BB%8Dc-Qu%E1%BB%91c-gia-H%C3%A0-N%E1%BB%99i",{"title":506},{"EN":507,"VI":508},"VNU University of Social Sciences and Humanities","Trường Đại học Khoa học Xã hội và Nhân văn, Đại học Quốc gia Hà Nội","2023-08-02T15:28:49.057+00:00",[],{"impactFactor":36,"impactFactorByYear":512,"i10Index":59,"i10IndexLast5Year":115,"totalPublication":514,"totalPublicationByYear":515,"totalCitation":518,"totalCitationByYear":519,"totalCitationPerPublication":520,"totalCitationPerPublicationByYear":521,"hindexLast5Year":162,"hindex":162},{"2016":229,"2017":230,"2018":229,"2021":230,"2022":58,"2023":513,"2024":38},0.15,365,{"2013":115,"2014":158,"2015":125,"2016":252,"2017":44,"2018":516,"2019":286,"2020":396,"2021":259,"2022":517,"2023":396,"2024":115,"2025":59,"2026":115},21,42,169,{"2015":283,"2016":135,"2017":52,"2018":50,"2019":298,"2020":53,"2021":359,"2022":115,"2023":115},0.46,{"2015":266,"2016":57,"2017":57,"2018":522,"2019":523,"2020":524,"2021":368,"2022":229,"2023":39},0.38,0.32,0.37,[],"http:\u002F\u002Fjournal.ussh.vnu.edu.vn\u002Findex.php\u002Fvjossh","\u002Fapi\u002Fpublic\u002Ffile\u002Fpublisher\u002F2b8d7b12-2d20-4777-be98-077f44f03c69\u002F0bd0751202944a4b4165b482e6e623e4.png",{"impactFactor":36,"impactFactorByYear":529,"i10Index":162,"i10IndexLast5Year":115,"totalPublication":530,"totalPublicationByYear":531,"totalCitation":537,"totalCitationByYear":538,"totalCitationPerPublication":343,"totalCitationPerPublicationByYear":540,"hindexLast5Year":135,"hindex":135},{"2016":341,"2017":39,"2018":229,"2019":38,"2020":110,"2021":231,"2022":231,"2023":341,"2024":39},764,{"2015":255,"2016":245,"2017":532,"2018":259,"2019":533,"2020":534,"2021":535,"2022":536,"2023":534,"2024":254,"2025":50},111,106,68,92,89,265,{"2015":539,"2016":241,"2017":168,"2018":51,"2019":349,"2020":260,"2021":244,"2022":298,"2023":114},46,{"2015":541,"2016":523,"2017":524,"2018":290,"2019":542,"2020":522,"2021":523,"2022":57,"2023":39},1.48,0.63,{"id":544,"createTime":545,"updateTime":546,"relativeEntities":547,"slug":548,"properties":549,"entityType":24,"verifyStatus":25,"verifyTime":26,"verifyNote":558,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":50,"subjectFields":559,"manageAffiliations":560,"indexDatabases":561,"url":562,"thumbnailPath":563,"statistic":564,"gsStatistic":26,"type":26,"analyzePriority":26},"6ec01bd0-15c0-469a-86ac-41339076ae0a","2023-08-10T07:08:33.153+00:00","2026-01-31T21:19:06.362+00:00",[],"T%E1%BA%A1p-ch%C3%AD-Da-li%E1%BB%85u-h%E1%BB%8Dc-Vi%E1%BB%87t-Nam",{"country":550,"issn":551,"introduce":553,"title":555},{"VOID":15},{"VOID":552},"18594824",{"VI":554},"{\"ops\":[{\"insert\":\"Tạp chí “Da liễu học Việt Nam” (Tiếng Anh: Vietnamese Journal of Dermatology and Venereology) thuộc Hội Da liễu Việt Nam, xuất bản 4 số mỗi năm bằng tiếng Việt hoặc tiếng Anh.\\nTạp chí Da liễu học Việt Nam hoạt động với mục đích, tôn chỉ là phổ biến, trao đổi thông tin trong lĩnh vực chuyên ngành da liễu; đăng tải các công trình nghiên cứu khoa học; chuyển giao công nghệ - kinh tế và khoa học kỹ thuật liên quan đến lĩnh vực da liễu.\\nPhạm vi của tạp chí là tất cả các bài báo khoa học, bài tổng quan, giới thiệu ca lâm sàng, … có liên quan tới chuyên ngành da liễu trong và ngoài nước. 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Hội đồng biên tập tạp chí bao gồm các nhà khoa học có uy tín (Giáo sư, Phó Giáo sư, Tiến sĩ, Bác sĩ…) trong chuyên ngành da liễu nhằm đảm bảo chất lượng và tính khách quan, khoa học cho các bài viết đăng trên Tạp chí.\\n\"}]}",{"EN":556,"VI":557},"Vietnamese Journal of Dermatology and Venereology","Tạp chí Da liễu học Việt Nam","Admin Import",[],[],[],"https:\u002F\u002Fvjdv.vn\u002Findex.php\u002Fvjdv","\u002Fapi\u002Fpublic\u002Ffile\u002Fpublisher\u002F6ec01bd0-15c0-469a-86ac-41339076ae0a\u002F3cbc81720e58429dc7b1c4d7ab1935ca.jpg",{"impactFactor":36,"impactFactorByYear":565,"i10Index":36,"i10IndexLast5Year":36,"totalPublication":566,"totalPublicationByYear":567,"totalCitation":116,"totalCitationByYear":570,"totalCitationPerPublication":109,"totalCitationPerPublicationByYear":571,"hindexLast5Year":115,"hindex":115},{"2023":38,"2024":230},182,{"2022":568,"2023":45,"2024":569},69,56,{"2022":52,"2023":115},{"2022":40,"2023":229},{"id":573,"createTime":574,"updateTime":575,"relativeEntities":576,"slug":577,"properties":578,"entityType":24,"verifyStatus":25,"verifyTime":26,"verifyNote":27,"syncStatus":28,"languages":587,"translateLanguages":26,"viewCount":283,"subjectFields":588,"manageAffiliations":589,"indexDatabases":647,"url":648,"thumbnailPath":649,"statistic":650,"gsStatistic":26,"type":26,"analyzePriority":26},"19221551-7519-47ff-a892-331d1139c64b","2023-09-12T07:03:05.744+00:00","2026-01-24T20:54:40.144+00:00",[],"T%E1%BA%A1p-ch%C3%AD-Khoa-h%E1%BB%8Dc-S%E1%BB%A9c-kho%E1%BA%BB-%C4%90%E1%BA%A1i-h%E1%BB%8Dc-Qu%E1%BB%91c-gia-Th%C3%A0nh-ph%E1%BB%91-H%E1%BB%93-Ch%C3%AD-Minh",{"country":579,"issn":580,"introduce":582,"title":584},{"VOID":15},{"VOID":581},"27349446",{"EN":583},"{\"ops\":[{\"attributes\":{\"bold\":true},\"insert\":\"1. 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And the first issue was published in January 1998 with ISSN 1859-0128. Since then, STDJ has become the most important scientific forum of scientists from VNU-HCM as well as other universities. The magazine has undergone 20 years of development and has become a bridge for scientific exchanges, as well as enriching reference materials for the faculty, doctoral students, students of VNU-HCM in particular and other universities, institutes...\"},{\"attributes\":{\"align\":\"justify\"},\"insert\":\"\\n\"},{\"insert\":\"Science and Technology Development Journal - Health Sciences (STDJ-HS) is a subjournal of Science and Technology Development Journal since 2020.\"},{\"attributes\":{\"align\":\"justify\"},\"insert\":\"\\n\"},{\"insert\":\" \"},{\"attributes\":{\"align\":\"justify\"},\"insert\":\"\\n\"},{\"attributes\":{\"bold\":true},\"insert\":\"2. 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Precious Metal. Geol., 7, 180",{},{"id":26,"text":1024,"url":26,"identifiers":1025},"Sillitoe R. H., 1989, Gold deposits in Western Pacific island arcs: The magmatic connection, Econ. Geol. Monogr., 6, 274",{},{"id":26,"text":1027,"url":26,"identifiers":1028},"Wang F‐T., 2001, Characteristics and significance of the Tuwu porphyry copper deposit, Xinjiang, Chinese Geol., 28, 36",{},{"id":26,"text":1030,"url":26,"identifiers":1031},"Wang S‐L., 2002, Types, characteristics of gold deposits in eastern Tianshan, Xinjiang, and their prospecting directions, 20",{},{"id":26,"text":1033,"url":26,"identifiers":1034},"10.2113\u002F95.7.1537",{"doi":1033},{"id":26,"text":1036,"url":26,"identifiers":1037},"10.1093\u002Fpetrology\u002F41.9.1455",{"doi":1036},{"id":26,"text":1039,"url":26,"identifiers":1040},"10.1016\u002FS0009-2541(01)00333-3",{"doi":1039},{"id":26,"text":1042,"url":26,"identifiers":1043},"Windley B. F., 1995, The Evolving Continents, 526",{},{"id":26,"text":1045,"url":26,"identifiers":1046},"Yin Y‐Q., 1996, Kuorzhenkuola epithermal Au deposit at Sawur Mountains, Xinjiang, Geol. Explor. Non-Ferrous Metals, 5, 278",{},{"id":26,"text":1048,"url":26,"identifiers":1049},"10.1080\u002F00206819209465586",{"doi":1048},{"id":26,"text":1051,"url":26,"identifiers":1052},"Zhai W., 1999, Characteristics and genesis of the Yiermand hot‐spring gold deposit in Yining country, Xinjiang, Mineral Deposits, 18, 47",{},{"id":26,"text":1054,"url":26,"identifiers":1055},"Zhang D‐Q., 1991, The Zijinshan Cu‐Au deposit—The first example of quartz‐alunite type epithermal deposits in the Continent of China, Geol. Rev., 37, 481",{},{"id":26,"text":1057,"url":26,"identifiers":1058},"Zhang L‐C, 1999, Geochemical dynamics of ore‐forming processes of Shiyingtan epithermal gold deposit, Eastern Tianshan, Jour. Xi'an College Eng., 21, 13",{},{"id":26,"text":1060,"url":26,"identifiers":1061},"Zhou T‐F., 2000, Mag‐matism and Metallogeny at Nurt Area, Altay, Xinjiang, 127",{},false,{"id":1064,"createTime":1065,"updateTime":1065,"relativeEntities":1066,"slug":1067,"properties":1068,"entityType":780,"verifyStatus":25,"verifyTime":1065,"verifyNote":781,"syncStatus":28,"languages":1080,"translateLanguages":26,"viewCount":36,"primaryUrl":1081,"fullTextUrl":26,"authors":1082,"publicationType":892,"publisherRelationship":1104,"citationCount":568,"citationInfo":1142,"publishDate":1144,"publishYear":1145,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":1146,"isForceReanalyzing":1062},"d17acb80-e522-4bac-ae94-9224af0a12f5","2024-09-21T06:13:39.636+00:00",[],"From-Predictive-Mapping-of-Mineral-Prospectivity-to-Quantitative-Estimation-of-Number-of-Undiscovered-Prospects",{"mag":1069,"keywords":1071,"openalex":1072,"abstract":1074,"title":1076,"doi":1078},{"VOID":1070},"1882925433",{},{"VOID":1073},"W1882925433",{"EN":1075},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>This paper proposes that the spatial pattern of known prospects of the deposit‐type sought is the key to link predictive mapping of mineral prospectivity (PMMP) and quantitative mineral resource assessment (QMRA). This proposition is demonstrated by PMMP for hydrothermal Au‐Cu deposits (HACD) and by estimating the number of undiscovered prospects for HACD in Catanduanes Island (Philippines). The results of analyses of the spatial pattern of known prospects of HACD and their spatial associations with geological features are consistent with existing knowledge of geological controls on hydrothermal Au‐Cu mineralization in the island and elsewhere, and are used to define spatial recognition criteria of regional‐scale prospectivity for HACD. Integration of layers of evidence representing the spatial recognition criteria of prospectivity via application of data‐driven evidential belief functions results in a map of prospective areas occupying 20% of the island with fitting‐ and prediction‐rates of 76% and 70%, respectively. The predictive map of prospective areas and a proxy measure for degrees of exploration based on the spatial pattern of known prospects of HACD were used in one‐level prediction of undiscovered mineral endowment, which yielded estimates of 79 to 112 undiscovered prospects of HACD. Application of radial‐density fractal analysis of the spatial pattern of known prospects of HACD results in an estimate of 113 undiscovered prospects of HACD. Thus, the results of the study support the proposition that PMMP can be a part of QMRA if the spatial pattern of discovered prospects of the deposit‐type sought is considered in both PMMP and QMRA.\u003C\u002Fjats:p>",{"EN":1077},"From Predictive Mapping of Mineral Prospectivity to Quantitative Estimation of Number of Undiscovered Prospects",{"VOID":1079},"10.1111\u002Fj.1751-3928.2010.00146.x",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1751-3928.2010.00146.x",[1083],{"id":1084,"sortIndex":36,"researcher":26,"roles":1085,"affiliations":1086,"properties":1097},"0d06f115-1046-4166-8088-872be237da5d",[],[1087],{"id":1088,"sortIndex":36,"affiliation":1089,"properties":26},"31f2b22f-54d4-4247-9265-ec0926574a05",{"id":1090,"createTime":1091,"updateTime":1091,"relativeEntities":1092,"slug":1093,"properties":1094,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"71ec486d-a6fa-40d9-a823-7cdeaf90ebcd","2024-09-21T06:13:39.652+00:00",[],"Department-of-Earth-Systems-Analysis-Faculty-of-Geo-Information-Science-and-Earth-Observation-ITC-University-of-Twente-Enschede-The-Netherlands",{"title":1095},{"EN":1096},"Department of Earth Systems Analysis, Faculty of Geo‐Information Science and Earth Observation (ITC), University of Twente, Enschede, The Netherlands",{"openalex":1098,"orcid":1100,"title":1102},{"VOID":1099},"A5007016189",{"VOID":1101},"https:\u002F\u002Forcid.org\u002F0000-0003-1765-0352",{"EN":1103},"Emmanuel John M. 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Soc., 140, 499, 10.1144\u002Fgsjgs.140.3.0499",{"doi":1712},"10.1144\u002Fgsjgs.140.3.0499",{"id":26,"text":1714,"url":26,"identifiers":1715},"Harding, R. R. and Hawkes, J. R. (1971) The Rb:Sr age and K\u002FRb ratios of samples from the St Austell granite, Cornwall. Inst. Geol. Sci. Rept, No. 71\u002F6.",{},{"id":26,"text":1717,"url":26,"identifiers":1718},"Hawkes, 1984, Geology of Granites and Their Metallogenic Relations, 571",{},{"id":26,"text":1720,"url":26,"identifiers":1721},"Hawkes, 1978, The Variscan granites of south-west England: a progress report, Proc. Ussher Soc, 4, 158",{},{"id":26,"text":1723,"url":26,"identifiers":1724},"Higgins, 1990, Comment on “Origin of alkali-feldspar granites: an example from the Poimena granite, northeastern Tasmania, Australia”, Geochim. Cosmochim. Acta., 54, 2305, 10.1016\u002F0016-7037(90)90056-Q",{"doi":1725},"10.1016\u002F0016-7037(90)90056-Q",{"id":26,"text":1727,"url":26,"identifiers":1728},"Hills, 1938, Andalusite and sillimanite in uncontaminat-ed igneous rocks, Geol. Mag., 75, 296, 10.1017\u002FS001675680009155X",{"doi":1729},"10.1017\u002FS001675680009155X",{"id":26,"text":1731,"url":26,"identifiers":1732},"Holtz, 1992, Effects of H2O on liquidus phase relations in the haplogran-ite system at 2 and 5 kbar, Amer. Mineral., 77, 1223",{},{"id":26,"text":1734,"url":26,"identifiers":1735},"Jackson, 1989, Evolution of the Cornubian ore field, southwest England: Part I. Mineral deposits and ore-forming processes, Econ. Geol., 84, 1101, 10.2113\u002Fgsecongeo.84.5.1101",{"doi":1736},"10.2113\u002Fgsecongeo.84.5.1101",{"id":26,"text":1738,"url":26,"identifiers":1739},"James, 1944, Mine temperatures in west Cornwall, Trans. Roy. Geol. Soc. Cornwall, 17, 164",{},{"id":26,"text":1741,"url":26,"identifiers":1742},"Jefferies, 1984, The radioactive accessory mineral assemblage of the Carnmenellis Granite, Cornwall, Proc. Ussher Soc, 6, 35",{},{"id":26,"text":1744,"url":26,"identifiers":1745},"Jefferies, 1985, High Heat Production (HHP) Granites, Hydrothermal Circulation and Ore Genesis, 163",{},{"id":26,"text":1747,"url":26,"identifiers":1748},"Jefferies, 1985, The origin of sillimanite-bearing pelitic xenoliths within the Carnmenellis pluton, Cornwall, Proc. Ussher Soc, 6, 229",{},{"id":26,"text":1750,"url":26,"identifiers":1751},"Jefferies, 1985, The distribution of the rare earth elements within the Carnmenellis Pluton, Cornwall, Mineral. Mag., 49, 495, 10.1180\u002Fminmag.1985.049.353.02",{"doi":1752},"10.1180\u002Fminmag.1985.049.353.02",{"id":26,"text":1754,"url":26,"identifiers":1755},"Johannes, 1984, Beginning of melting in the granite system Qz-Or-Ab-An-H2O, Contrib. Mineral. Petrol., 86, 264, 10.1007\u002FBF00373672",{"doi":1756},"10.1007\u002FBF00373672",{"id":26,"text":1758,"url":26,"identifiers":1759},"Johannes, 1996, Petrogenesis and Experimental Petrology of Granitic Rocks, 10.1007\u002F978-3-642-61049-3",{"doi":1760},"10.1007\u002F978-3-642-61049-3",{"id":26,"text":1762,"url":26,"identifiers":1763},"Lee, 1987, Heat flow, heat production and thermo-tectonic setting in mainland UK, Jour. Geol. Soc., 144, 35, 10.1144\u002Fgsjgs.144.1.0035",{"doi":1764},"10.1144\u002Fgsjgs.144.1.0035",{"id":26,"text":1766,"url":26,"identifiers":1767},"Liew, T. C. (1983) Petrogenesis of the Peninsular Malaysian granitoid batholiths. PhD Thesis, Australian National Univ., Canberra, Australia.",{},{"id":26,"text":1769,"url":26,"identifiers":1770},"Lister, 1984, Xenolith assimilation in the granites of south-west England, Proc. Ussher Soc, 6, 46",{},{"id":26,"text":1772,"url":26,"identifiers":1773},"London, 1990, The berlinite substitution, A1P = 2Si, in alkali feldspars from differentiated peraluminous igneous rocks (granites, pegmatites and rhyolites), Geol. Soc Amer. Abstr. Prog., 22, A346",{},{"id":26,"text":1775,"url":26,"identifiers":1776},"London, 1992, Phosphorus in S-type magmas: the P2O5 content of feldspars from peraluminous granites, pegmatites, and rhyolites, Amer. Mineral, 77, 126",{},{"id":26,"text":1778,"url":26,"identifiers":1779},"London, 1997, Estimating abundances of volatiles and other mobile components in evolved silicic melts through mineral-melt equilibria, Jour. Petrol, 38, 1691, 10.1093\u002Fpetroj\u002F38.12.1691",{"doi":1780},"10.1093\u002Fpetroj\u002F38.12.1691",{"id":26,"text":1782,"url":26,"identifiers":1783},"McKenzie, 1975, Petrology of the South Mountain Batholith, Nova Scotia, Canad. Jour. 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Geol. Soc., 139, 533, 10.1144\u002Fgsjgs.139.4.0533",{"doi":1847},"10.1144\u002Fgsjgs.139.4.0533",{"id":26,"text":1849,"url":26,"identifiers":1850},"Shaw, A. L. and Guilbert, J. M. (1990) Geochemistry and metal-logeny of Arizona peraluminous granitoids with reference to Appalachian and European occurrences, in Stein, H. J. and Hannah, J. L. (eds.) Ore-bearing Systems; Petrogenesis and Mineralizing Processes. Geol. Soc. Amer. Spec. Paper, 246, 317-356.",{},{"id":26,"text":1852,"url":26,"identifiers":1853},"Sheppard, 1977, The Cornubian batholith, SW England: D\u002FH and 18O\u002F16O studies of kaolinite and other alteration minerals, Jour. Geol. Soc., 133, 573, 10.1144\u002Fgsjgs.133.6.0573",{"doi":1854},"10.1144\u002Fgsjgs.133.6.0573",{"id":26,"text":1856,"url":26,"identifiers":1857},"Simpson, 1979, Uranium mineralization and granite magmatism in the British Isles, Phil. Trans. Roy. Soc. London, A291, 385, 10.1098\u002Frsta.1979.0034",{"doi":1858},"10.1098\u002Frsta.1979.0034",{"id":26,"text":1860,"url":26,"identifiers":1861},"Stemprok, 1995, A comparison of the Krusné hory-Erzgebirge (Czeck Republic-Germany) and Cornish (UK) granites, Proc. Ussher Soc, 8, 347",{},{"id":26,"text":1863,"url":26,"identifiers":1864},"Stimac, 1995, Enclaves and their bearing on the origin of the Cornubian batholith, southwest England, Mineral. Mag., 59, 273, 10.1180\u002Fminmag.1995.059.395.12",{"doi":1865},"10.1180\u002Fminmag.1995.059.395.12",{"id":26,"text":1867,"url":26,"identifiers":1868},"Stone, 1987, Geochemistry and origin of the Carnmenel-lis pluton, Cornwall: further considerations, Proc. Ussher Soc, 6, 454",{},{"id":26,"text":1870,"url":26,"identifiers":1871},"Stone, 1988, The significance of almandine garnets in the Lundy and Dartmoor granites, Mineral. Mag., 52, 651, 10.1180\u002Fminmag.1988.052.368.09",{"doi":1872},"10.1180\u002Fminmag.1988.052.368.09",{"id":26,"text":1874,"url":26,"identifiers":1875},"Stone, 2000, The early Cornubian plutons; a geochemistry study, comparisons and some implications, Proc. Ussher Soc, 10, 37",{},{"id":26,"text":1877,"url":26,"identifiers":1878},"Stone, 1961, The metasomatic origin of the potash feldspar megacrysts in the granites of southwest England, Jour. Geol., 69, 464, 10.1086\u002F626762",{"doi":1879},"10.1086\u002F626762",{"id":26,"text":1881,"url":26,"identifiers":1882},"Stone, 1985, High Heat Production (HHP) Granites, Hydrothermal Circulation and Ore Genesis, 571",{},{"id":26,"text":1884,"url":26,"identifiers":1885},"Stone, 1989, Geochemistry of the Isles of Scilly pluton, Proc. Ussher Soc, 7, 152",{},{"id":26,"text":1887,"url":26,"identifiers":1888},"Stussi, 1989, Granitoid chemistry and associated mineralization in the French Variscan, Econ. Geol., 84, 1363, 10.2113\u002Fgsecongeo.84.5.1363",{"doi":1889},"10.2113\u002Fgsecongeo.84.5.1363",{"id":26,"text":1891,"url":26,"identifiers":1892},"Sweetman, 1987, The geochemistry of the Blackstairs Unit of the Leinster Granite, Ireland, Jour. Geol. Soc., 144, 971, 10.1144\u002Fgsjgs.144.6.0971",{"doi":1893},"10.1144\u002Fgsjgs.144.6.0971",{"id":26,"text":1895,"url":26,"identifiers":1896},"Tammemagi, 1975, A radiogeologic study of the granites of SW England, Jour. Geol. Soc., 131, 415, 10.1144\u002Fgsjgs.131.4.0415",{"doi":1897},"10.1144\u002Fgsjgs.131.4.0415",{"id":26,"text":1899,"url":26,"identifiers":1900},"Tammemagi, 1974, Terrestrial heat flow and heat generation in south-west England, Geophys. Jour. Roy. Astronomical Soc, 38, 83, 10.1111\u002Fj.1365-246X.1974.tb04110.x",{"doi":1901},"10.1111\u002Fj.1365-246X.1974.tb04110.x",{"id":26,"text":1903,"url":26,"identifiers":1904},"Taylor, 1985, The Continental Crust: Its Composition and Evolution, 312",{},{"id":26,"text":1906,"url":26,"identifiers":1907},"Thompson, 1984, An assessment of the relative roles of crust and mantle in magma genesis: an elemental approach, Phil. Trans. Roy. Soc. London, A310, 549, 10.1098\u002Frsta.1984.0008",{"doi":1908},"10.1098\u002Frsta.1984.0008",{"id":26,"text":1910,"url":26,"identifiers":1911},"Turtle, 1958, Origin of Granite in the Light of Experimental Studies in the System NaAl3SiO8-KAl3SiO8-SiO2-H2O, Geol. Soc. Amer. Mem., 74",{},{"id":26,"text":1913,"url":26,"identifiers":1914},"Molen, 1979, Experimental deformation of partially-melted granite, Contrib. Mineral. Petrol., 70, 299, 10.1007\u002FBF00375359",{"doi":1915},"10.1007\u002FBF00375359",{"id":26,"text":1917,"url":26,"identifiers":1918},"Vidal, 1984, Geochemical comparison between Himalayan and Hercynian leucogranites, Phys. Earth Planet. Int., 35, 179, 10.1016\u002F0031-9201(84)90041-4",{"doi":1919},"10.1016\u002F0031-9201(84)90041-4",{"id":26,"text":1921,"url":26,"identifiers":1922},"Ward, 1992, Rare earth element behaviour during evolution and alteration of the Dartmoor granite, SW England, Jour. Petrol., 33, 785, 10.1093\u002Fpetrology\u002F33.4.785",{"doi":1923},"10.1093\u002Fpetrology\u002F33.4.785",{"id":26,"text":1925,"url":26,"identifiers":1926},"Watson, 1983, Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types, Earth Planet. Sci. Lett., 64, 295, 10.1016\u002F0012-821X(83)90211-X",{"doi":1927},"10.1016\u002F0012-821X(83)90211-X",{"id":26,"text":1929,"url":26,"identifiers":1930},"Watson, 1984, Variscan-Caledonian comparisons: late orogenic granites, Proc. Ussher Soc, 6, 2",{},{"id":26,"text":1932,"url":26,"identifiers":1933},"Webb, 1985, High Heat Production (HHP) Granites, Hydrothermal Circulation and Ore Genesis, 409",{},{"id":26,"text":1935,"url":26,"identifiers":1936},"Wheildon, J. , Francis, M. F. , Ellis, J. R. L. and Thomas-Berts, A. (1981) Investigation of the S.W. England Thermal Anomaly Zone. Luxembourg: Commission of European Communities Report EUR 7276 EN, 410 p.",{},{"id":26,"text":1938,"url":26,"identifiers":1939},"White, 1988, Some supracrustal (S-type) granites of the Lachlan Fold Belt, Trans. Roy. Soc. Edinburgh Earth Sci., 79, 169, 10.1017\u002FS026359330001419X",{"doi":1940},"10.1017\u002FS026359330001419X",{"id":26,"text":1942,"url":26,"identifiers":1943},"Willis-Richards, 1989, Evolution of the Cornubian ore field, southwest England: Part I. Batholith modeling and ore distribution, Econ. Geol., 84, 1078, 10.2113\u002Fgsecongeo.84.5.1078",{"doi":1944},"10.2113\u002Fgsecongeo.84.5.1078",{"id":26,"text":1946,"url":26,"identifiers":1947},"Wilson, I. R. (1972) Wall rock alteration at Geevor Mine, Cornwall, and Ashanti Mine, Ghana. PhD Thesis, Univ. Leeds, Leeds, England.",{},{"id":26,"text":1949,"url":26,"identifiers":1950},"Wilson, 1974, Distribution of uranium in the Land's End granite and aureole, and various greenstones from Cornwall, Proc. Ussher Soc, 3, 166",{},{"id":26,"text":1952,"url":26,"identifiers":1953},"Wolf, 1994, Apatite dissolution into peraluminous haplogranitic melts: an experimental study of solubilities and mechanisms, Geochim. Cosmochim. Acta., 58, 4127, 10.1016\u002F0016-7037(94)90269-0",{"doi":1954},"10.1016\u002F0016-7037(94)90269-0",{"id":26,"text":1956,"url":26,"identifiers":1957},"Wyborn, 1998, Compositional changes during fractionation of felsic granites from western Tasmania, Australia, Acta Univ. Carolinae Geol., 42, 189",{},{"id":1959,"createTime":1960,"updateTime":1960,"relativeEntities":1961,"slug":1962,"properties":1963,"entityType":780,"verifyStatus":25,"verifyTime":1975,"verifyNote":781,"syncStatus":28,"languages":1976,"translateLanguages":26,"viewCount":36,"primaryUrl":1977,"fullTextUrl":26,"authors":1978,"publicationType":892,"publisherRelationship":2034,"citationCount":281,"citationInfo":2071,"publishDate":2073,"publishYear":934,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":2074,"isForceReanalyzing":1062},"4678707f-04c8-47ee-8674-fac13a6e9d56","2024-10-03T07:08:31.726+00:00",[],"Geochemical-and-Nd-Sr-Isotopic-Study-of-the-Post-Orogenic-Granites-in-the-Yidun-Arc-Belt-of-Northern-Sanjiang-Region-Southwestern-China",{"mag":1964,"keywords":1966,"openalex":1967,"abstract":1969,"title":1971,"doi":1973},{"VOID":1965},"2032340654",{},{"VOID":1968},"W2032340654",{"EN":1970},"\u003Cjats:p>\u003Cjats:bold>Abstract: \u003C\u002Fjats:bold> In the arc (basin)–back area of the Yidun arc belt in the north segment of the Sanjiang tectonic zone, southwestern China, there occurs a post‐orogenic granite belt extending for more than 300 km in NNW direction. It strides across two different tectonic units of the arc (basin)–back area and the subduction area, and is accompanied by extensive Ag‐Sn polymetal–lic mineralizations. More than ten granite bodies have very similar geochemical characteristics: high SiO\u003Cjats:sub>2\u003C\u002Fjats:sub> (73.8–76.3 wt%) and K\u003Cjats:sub>2\u003C\u002Fjats:sub>O+Na\u003Cjats:sub>2\u003C\u002Fjats:sub>O (7.16‐8.41 %), and low Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> (11.9–13.6 %), CaO (0.46‐1.54 %) and MgO (0.16‐0.61 %), as well as high enrichment of Nb, Ta, Ga and Y, and strong depletion of Sr and Eu. Most of these features are peculiar to A‐type granite. Rb‐Sr and \u003Cjats:sup>40\u003C\u002Fjats:sup>Ar\u002F\u003Cjats:sup>39\u003C\u002Fjats:sup>Ar isotopic dating results indicate that the formation ages of the granites decrease from 103.7 Ma of the north end to 75.2 Ma near the south end, and that the magmatism became younger from north to south. The tectonic environment analysis clearly reveals that they were formed in post‐orogenic within–plate extension settings. The magma genesis was controlled by a united crustal extension regime after the arc‐continent collision. The granites have low \u003Cjats:sub>Nd\u003C\u002Fjats:sub> values ranging from –4.96 to –8.40, whereas the \u003Cjats:sub>Sr\u003C\u002Fjats:sub> values vary greatly ranging from –31.7 to 296, reflecting that the source composition transited from mantle – differentiated igneous rocks in the north to basement – dominated metamorphosed sedimentary rocks in the south. Under high temperature and water‐absent conditions, the anatexes of the crustal rocks made a great amount of plagioclase separated from melts and left in magma sources. Through this mechanism, the post‐orogenic granites took geo‐chemical characteristics such as low Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> and CaO, and strong depletion of Sr and Eu.\u003C\u002Fjats:p>",{"EN":1972},"Geochemical and Nd, Sr Isotopic Study of the Post‐Orogenic Granites in the Yidun Arc Belt of Northern Sanjiang Region, Southwestern China",{"VOID":1974},"10.1111\u002Fj.1751-3928.2002.tb00128.x","2024-10-03T07:08:31.725+00:00",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1751-3928.2002.tb00128.x",[1979,1998,2013],{"id":1980,"sortIndex":36,"researcher":26,"roles":1981,"affiliations":1982,"properties":1993},"1c148f0b-cacc-4fd6-9fd3-7fd24aa26477",[],[1983],{"id":1984,"sortIndex":36,"affiliation":1985,"properties":26},"76c1b136-1ce7-47f9-8b80-93950d6919b3",{"id":1986,"createTime":1987,"updateTime":1987,"relativeEntities":1988,"slug":1989,"properties":1990,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"6181439c-1ae0-4fb6-988a-3adac0cb54eb","2024-10-03T07:08:31.739+00:00",[],"Institute-of-Mineral-Resource-Chinese-Academy-of-Geological-Sciences-Baiwanzhuang-Road-26-Beijing-100037-China-e-mail-imdcags-public3-bta-net-cn-",{"title":1991},{"EN":1992},"Institute of Mineral Resource, Chinese Academy of Geological Sciences, Baiwanzhuang Road 26, Beijing 100037, China [e-mail: imdcags@public3.bta.net.cn]",{"openalex":1994,"title":1996},{"VOID":1995},"A5010194559",{"EN":1997},"Xiaoming Qu",{"id":1999,"sortIndex":115,"researcher":26,"roles":2000,"affiliations":2001,"properties":2008},"47ece5bb-bd0c-46a5-b40c-0638739f04d8",[],[2002],{"id":2003,"sortIndex":36,"affiliation":2004,"properties":26},"e1fd0edd-2c50-4f86-b716-f7281ce7419a",{"id":1986,"createTime":1987,"updateTime":1987,"relativeEntities":2005,"slug":1989,"properties":2006,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":2007},{"EN":1992},{"openalex":2009,"title":2011},{"VOID":2010},"A5100932318",{"EN":2012},"Zengqian 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Q., 1993, The tectono‐magmatic evolution of Yidun Island‐arc and geodynamic settings of the formation of Kuroko‐type massive sulphide deposits in Sanjiang region, S, W. China. Resource Geol., Spec. Issue, 17, 336",{},{"id":26,"text":2100,"url":26,"identifiers":2101},"Huang J. Q., 1986, The Evolution of Tethys Sea of China and the Neighbour Region",{},{"id":26,"text":2103,"url":26,"identifiers":2104},"10.1016\u002F0040-1951(93)90295-U",{"doi":2103},{"id":26,"text":2106,"url":26,"identifiers":2107},"10.1016\u002F0009-2541(93)90141-5",{"doi":2106},{"id":26,"text":2109,"url":26,"identifiers":2110},"Lu B. X., 1993, The Granitoids and Metallogenic Specialization in Sanjiang Region",{},{"id":26,"text":2112,"url":26,"identifiers":2113},"Mo X. X., 1993, The Volcanism and Metallogeny of Tethys in Sanjiang Region",{},{"id":26,"text":2115,"url":26,"identifiers":2116},"10.1093\u002Fpetrology\u002F25.4.956",{"doi":2115},{"id":26,"text":2118,"url":26,"identifiers":2119},"Qiu J. Y., 1985, Petrology of Magmatic Rocks",{},{"id":26,"text":2121,"url":26,"identifiers":2122},"Qu X. M., 2001, The characteristics and origin of Nongduke volcanic‐hosted epithermal Ag polymetallic deposit in western Sichuan Province, Mineral Deposits, 20, 199",{},{"id":26,"text":2124,"url":26,"identifiers":2125},"Qu X. M., 2001, Metallogenic geological characteristics of the Lianlong skarn‐type SnAg polymetallic deposit in western Sichuan Province, Acta Geosci. Sinica, 22, 29",{},{"id":26,"text":2127,"url":26,"identifiers":2128},"Shen W. Z., 1991, Nd, Sr, O isotopic and geological study of Xiqou spilite–keratophyre, Zhejiang Province, Acta Geol. Sinica, 337",{},{"id":26,"text":2130,"url":26,"identifiers":2131},"10.1130\u002F0091-7613(1992)020\u003C0263:VAMAKO>2.3.CO;2",{"doi":2130},{"id":26,"text":2133,"url":26,"identifiers":2134},"10.1007\u002FBF00402202",{"doi":2133},{"id":26,"text":2136,"url":26,"identifiers":2137},"Ye Q. T., 1991, The ore‐forming geological characteristics and the origin of Gacun auriferous rich‐Ag polymetallic deposit in Sichuan Province, Mineral Deposits, 10, 107",{},{"id":2139,"createTime":2140,"updateTime":2140,"relativeEntities":2141,"slug":2142,"properties":2143,"entityType":780,"verifyStatus":25,"verifyTime":2140,"verifyNote":781,"syncStatus":28,"languages":2155,"translateLanguages":26,"viewCount":36,"primaryUrl":2156,"fullTextUrl":26,"authors":2157,"publicationType":892,"publisherRelationship":2179,"citationCount":124,"citationInfo":2215,"publishDate":2217,"publishYear":1145,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":2218,"isForceReanalyzing":1062},"e2262ae0-2b03-411b-b911-d68fbc698b85","2025-02-09T15:34:11.291+00:00",[],"Regional-Exploration-Targeting-Model-for-Gangdese-Porphyry-Copper-Deposits",{"mag":2144,"keywords":2146,"openalex":2147,"abstract":2149,"title":2151,"doi":2153},{"VOID":2145},"1542116403",{},{"VOID":2148},"W1542116403",{"EN":2150},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>An exploration targeting model for Gangdese porphyry copper deposit in Tibet, China, is constructed based on (i) the age of porphyry intrusions within Gangdese magmatic arc; (ii) the regional‐scale normal E–W, N–S and N–E striking faults; and (iii) comprehensive anomalously high concentrations of Cu‐Mo‐Au‐Ag‐Pb‐Zn. These targeting elements are derived from geological map and geochemical dataset, and are integrated by weights of evidence with the aid of geographic information system (GIS). The resulting prospectivity for porphyry copper deposits delineated by posterior probability demonstrates that the target areas extend along the Yaluzangbujiang River and contain the two large deposits, Qulong and Chongjiang, located in the eastern and central part of the Gangdese belt, respectively. These results indicate that the proposed exploration targeting model is a potential tool to map regional‐scale mineral prospectivity. The target areas with high values of favorability, especially where high concentrations of Cu‐Mo‐Au‐Ag‐Pb‐Zn are present, are the potential areas for finding undiscovered porphyry copper deposits.\u003C\u002Fjats:p>",{"EN":2152},"Regional Exploration Targeting Model for Gangdese Porphyry Copper Deposits",{"VOID":2154},"10.1111\u002Fj.1751-3928.2011.00166.x",[102],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1751-3928.2011.00166.x",[2158],{"id":2159,"sortIndex":36,"researcher":26,"roles":2160,"affiliations":2161,"properties":2172},"7a71b70f-0b59-4d92-8978-6d04701d9690",[],[2162],{"id":2163,"sortIndex":36,"affiliation":2164,"properties":26},"5d67e1d5-2c2a-44be-af02-c2083ef83eba",{"id":2165,"createTime":2166,"updateTime":2166,"relativeEntities":2167,"slug":2168,"properties":2169,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"2e1b06d9-2390-44cf-a742-f2db7f22892f","2025-02-09T15:34:11.312+00:00",[],"State-Key-Laboratory-of-Geological-Processes-and-Mineral-Resources-China-University-of-Geosciences-Wuhan-Beijing-China",{"title":2170},{"EN":2171},"State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Beijing, China",{"openalex":2173,"orcid":2175,"title":2177},{"VOID":2174},"A5008183305",{"VOID":2176},"https:\u002F\u002Forcid.org\u002F0000-0002-5639-3128",{"EN":2178},"Renguang Zuo",{"url":26,"publisher":2180,"properties":2210},{"id":659,"createTime":660,"updateTime":661,"relativeEntities":2181,"slug":663,"properties":2182,"entityType":24,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36,"subjectFields":2188,"manageAffiliations":2189,"indexDatabases":2190,"url":752,"thumbnailPath":26,"statistic":2205,"gsStatistic":26,"type":26,"analyzePriority":26},[],{"country":2183,"issn":2184,"introduce":2185,"eissn":2186,"title":2187},{"VOID":666},{"VOID":668},{"EN":670},{"VOID":672},{"EN":674},[],[],[2191,2198],{"id":733,"indexDatabase":2192,"url":748,"indexYears":26,"academicFieldIds":2197,"indexDatabaseRanking":26},{"id":735,"createTime":736,"updateTime":737,"relativeEntities":2193,"label":2194,"description":2195,"key":744,"publicationTags":2196,"standard":26},[],{"EN":740,"VI":740},{"VI":742,"EN":743},[746,747],[750,751],{"id":713,"indexDatabase":2199,"url":726,"indexYears":727,"academicFieldIds":2204,"indexDatabaseRanking":731},{"id":715,"createTime":716,"updateTime":717,"relativeEntities":2200,"label":2201,"description":2202,"key":723,"publicationTags":2203,"standard":26},[],{"EN":720,"VI":720},{"EN":720,"VI":722},[725],[729,730],{"impactFactor":36,"impactFactorByYear":2206,"i10Index":114,"i10IndexLast5Year":36,"totalPublication":114,"totalPublicationByYear":2207,"totalCitation":126,"totalCitationByYear":2208,"totalCitationPerPublication":757,"totalCitationPerPublicationByYear":2209,"hindexLast5Year":114,"hindex":114},{"2012":59,"2013":162},{"2002":115,"2011":115},{"2002":281,"2011":568},{"2002":281,"2011":568},{"volume":2211,"pages":2212,"issue":2214},{"VOID":1137},{"VOID":2213},"296-303",{"VOID":1519},{"total":124,"publishYear":26,"statisticByYear":2216},{"2012":115,"2013":115,"2014":114,"2015":114,"2016":59,"2017":115,"2018":115,"2021":114,"2022":115},"2011-07-01",[2219,2222,2225,2228,2231,2234,2237,2240,2243,2246,2249,2252,2255,2258,2261,2264,2267,2270,2273,2276,2279,2282,2285,2288,2291,2294,2297,2300,2303,2306,2309,2312,2315,2318,2321,2324,2327,2330,2333,2336,2339],{"id":26,"text":2220,"url":26,"identifiers":2221},"Agterberg F. P.(1989)Systematic approach to dealing with uncertainty of geoscience information in mineral exploration. Proceedings of the 21st APCOM Symposium Las Vegas USA Chapter 18 p. 165–178.",{},{"id":26,"text":2223,"url":26,"identifiers":2224},"10.1038\u002F307017a0",{"doi":2223},{"id":26,"text":2226,"url":26,"identifiers":2227},"10.1007\u002Fs00126-003-0375-y",{"doi":2226},{"id":26,"text":2229,"url":26,"identifiers":2230},"10.1038\u002F35088045",{"doi":2229},{"id":26,"text":2232,"url":26,"identifiers":2233},"Bonham‐Carter G. 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Deposits, 22, 1",{},{"id":26,"text":2259,"url":26,"identifiers":2260},"Hou Z., 2003, Re–Os age for molybdenite from the Gangdese porphyry copper belt on Tibetan plateau: implication for geodynamic setting and duration of the Cu mineralization., Sci. China, 33, 509",{},{"id":26,"text":2262,"url":26,"identifiers":2263},"10.1016\u002FS0012-821X(04)00007-X",{"doi":2262},{"id":26,"text":2265,"url":26,"identifiers":2266},"10.1016\u002Fj.oregeorev.2008.09.006",{"doi":2265},{"id":26,"text":2268,"url":26,"identifiers":2269},"10.1126\u002Fscience.274.5293.1692",{"doi":2268},{"id":26,"text":2271,"url":26,"identifiers":2272},"10.1046\u002Fj.1440-0952.2000.00816.x",{"doi":2271},{"id":26,"text":2274,"url":26,"identifiers":2275},"Li G., 2004, Diagenetic and mineralization ages for the porphyry copper deposits in the gangdise metallogenic belt, southern Xizang, Geotectonica et Metallogenia, 28, 165",{},{"id":26,"text":2277,"url":26,"identifiers":2278},"Lord D., 2001, Measuring exploration success: an alternative to the discovery‐cost‐per‐ounce method of quantifying exploration effectiveness, SEG Newsl., 45, 10",{},{"id":26,"text":2280,"url":26,"identifiers":2281},"10.2113\u002Fgsecongeo.65.4.373",{"doi":2280},{"id":26,"text":2283,"url":26,"identifiers":2284},"10.1093\u002Fpetroj\u002F40.9.1399",{"doi":2283},{"id":26,"text":2286,"url":26,"identifiers":2287},"Qu X., 2001, Is Gangdese porphyry copper belt the second “yulong” copper belt?, Miner. Deposits, 20, 355",{},{"id":26,"text":2289,"url":26,"identifiers":2290},"Qu X., 2003, 40Ar\u002F39Ar ages of porphyries from the Gangdese porphyry Cu belt in south Tibet and implication to geodynamic setting, Acta Geol. Sin., 77, 245",{},{"id":26,"text":2292,"url":26,"identifiers":2293},"10.1016\u002Fj.oregeorev.2005.03.012",{"doi":2292},{"id":26,"text":2295,"url":26,"identifiers":2296},"10.2113\u002Fgsecongeo.98.8.1515",{"doi":2295},{"id":26,"text":2298,"url":26,"identifiers":2299},"Rui Z., 2003, Metallogenic epoch of Gangdese porphyry copper belt and uplift of Qinghai‐Tibetan Plateau, Miner. Deposits, 22, 224",{},{"id":26,"text":2301,"url":26,"identifiers":2302},"Rui Z., 2004, The response of porphyry copper deposits to important geological events in Xizang (Tibet), Earth Sci. Front., 11, 145",{},{"id":26,"text":2304,"url":26,"identifiers":2305},"10.2113\u002Fgsecongeo.67.2.184",{"doi":2304},{"id":26,"text":2307,"url":26,"identifiers":2308},"Sillitoe R. H.(1993)Gold‐rich porphyry copper deposits: geological model and exploration implication. Mineral Deposit Modeling Geological Association of Canada Special Paper 40 465–478.",{},{"id":26,"text":2310,"url":26,"identifiers":2311},"10.1016\u002FS0375-6742(97)00029-0",{"doi":2310},{"id":26,"text":2313,"url":26,"identifiers":2314},"10.1016\u002Fj.oregeorev.2009.03.003",{"doi":2313},{"id":26,"text":2316,"url":26,"identifiers":2317},"10.1146\u002Fannurev.earth.28.1.211",{"doi":2316},{"id":26,"text":2319,"url":26,"identifiers":2320},"Zheng Y., 2004, Finding, characteristics and significances of Qulong superlarge porphyry copper (molybdenum) deposit, Tibet, Earth Sci. J. China Univ. Geosci., 29, 103",{},{"id":26,"text":2322,"url":26,"identifiers":2323},"Zheng Y., 2004, Finding and significances of Chongjiang porphyry copper (molybdenum, aurum) deposit, Tibet, Earth Sci. J. China Univ. Geosci., 29, 333",{},{"id":26,"text":2325,"url":26,"identifiers":2326},"Zheng Y., 2006, The discovery of Zhunuo porphyry copper deposit in Tibet and its significance, Earth Sci. Front., 13, 233",{},{"id":26,"text":2328,"url":26,"identifiers":2329},"10.1007\u002Fs11434-007-0406-7",{"doi":2328},{"id":26,"text":2331,"url":26,"identifiers":2332},"10.1180\u002Fminmag.2008.072.1.531",{"doi":2331},{"id":26,"text":2334,"url":26,"identifiers":2335},"Zuo R., 2007, Synthetic information prediction of porphyry copper in Tibet, Cent. South Univ. Technol., 38, 368",{},{"id":26,"text":2337,"url":26,"identifiers":2338},"10.1016\u002Fj.oregeorev.2008.11.004",{"doi":2337},{"id":26,"text":2340,"url":26,"identifiers":2341},"10.1016\u002Fj.gexplo.2008.08.003",{"doi":2340}]