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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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thermodynamic properties of 154 mineral end‐members, 13 silicate liquid end‐members and 22 aqueous fluid species are presented in a revised and updated data set. The use of a temperature‐dependent thermal expansion and bulk modulus, and the use of high‐pressure equations of state for solids and fluids, allows calculation of mineral–fluid equilibria to 100 kbar pressure or higher. A pressure‐dependent Landau model for order–disorder permits extension of disordering transitions to high pressures, and, in particular, allows the alpha–beta quartz transition to be handled more satisfactorily. Several melt end‐members have been included to enable calculation of simple phase equilibria and as a first stage in developing melt mixing models in NCKFMASH. The simple aqueous species density model has been extended to enable speciation calculations and mineral solubility determination involving minerals and aqueous species at high temperatures and pressures. The data set has also been improved by incorporation of many new phase equilibrium constraints, calorimetric studies and new measurements of molar volume, thermal expansion and compressibility. This has led to a significant improvement in the level of agreement with the available experimental phase equilibria, and to greater flexibility in calculation of complex mineral equilibria. It is also shown that there is very good agreement between the data set and the most recent available calorimetric data.\u003C\u002Fjats:p>",{"EN":961},"An internally consistent thermodynamic data set for phases of petrological interest",{"VOID":963},"10.1111\u002Fj.1525-1314.1998.00140.x","PUBLICATION","Auto Verify",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1525-1314.1998.00140.x",[969,988],{"id":970,"sortIndex":32,"researcher":28,"roles":971,"affiliations":972,"properties":981,"displayName":985,"givenName":28,"familyName":28},"ad65e235-cd5d-4ee1-a270-2b2c5a80f967",[],[973],{"id":974,"sortIndex":32,"affiliation":975,"properties":28},"c0d745d6-ab32-4bdb-a7f5-86be8551de18",{"id":974,"createTime":28,"updateTime":28,"relativeEntities":976,"slug":28,"properties":977,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":980,"statistic":28},[],{"title":978},{"EN":979},"1  Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK (email: tjbh@esc.cam.ac.uk), 2 School of Earth Sciences, University of Melbourne, Parkville, Victoria 3052, Australia",[],{"orcid":982,"title":984,"openalex":986},{"VOID":983},"https:\u002F\u002Forcid.org\u002F0000-0003-2852-9515",{"EN":985},"T. 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J., 1995, Thermal expansion of scapolite., American Mineralogist, 79, 878",{},{"id":28,"text":1104,"url":28,"identifiers":1105},"10.2138\u002Fam-1996-5-615",{"doi":1104},{"id":28,"text":1107,"url":28,"identifiers":1108},"Baker J., 1994, Standard thermodynamic properties of meionite, Ca4Al6Si6O24CO3, from experimental phase equilibria., American Mineralogist, 79, 478",{},{"id":28,"text":1110,"url":28,"identifiers":1111},"10.1029\u002FJB091iB07p07505",{"doi":1110},{"id":28,"text":1113,"url":28,"identifiers":1114},"10.1029\u002FJB094iB06p07621",{"doi":1113},{"id":28,"text":1116,"url":28,"identifiers":1117},"10.1093\u002Fpetrology\u002F29.2.445",{"doi":1116},{"id":28,"text":1119,"url":28,"identifiers":1120},"Berman R. G., 1987, Development of models for multicomponent melts: analysis of synthetic systems. In:, Reviews in Mineralogy, 17, 405",{},{"id":28,"text":1122,"url":28,"identifiers":1123},"10.1130\u002FMEM97-p97",{"doi":1122},{"id":28,"text":1125,"url":28,"identifiers":1126},"10.2475\u002Fajs.280.9.907",{"doi":1125},{"id":28,"text":1128,"url":28,"identifiers":1129},"10.1029\u002FJB087iB08p07073",{"doi":1128},{"id":28,"text":1131,"url":28,"identifiers":1132},"10.1016\u002F0012-821X(80)90098-9",{"doi":1131},{"id":28,"text":1134,"url":28,"identifiers":1135},"10.1007\u002FBF00371195",{"doi":1134},{"id":28,"text":1137,"url":28,"identifiers":1138},"10.2138\u002Fam-1995-3-404",{"doi":1137},{"id":28,"text":1140,"url":28,"identifiers":1141},"10.1007\u002F978-1-4612-3128-8_7",{"doi":1140},{"id":28,"text":1143,"url":28,"identifiers":1144},"10.2475\u002Fajs.s4-40.236.161",{"doi":1143},{"id":28,"text":1146,"url":28,"identifiers":1147},"BowmanA. F.1975;An investigation of Al2SiO5phase equilibrium utilizing the scanning electron microscopeMS thesis University of Oregon Eugene Oregon USA.",{},{"id":28,"text":1149,"url":28,"identifiers":1150},"10.1029\u002FJB074i008p02089",{"doi":1149},{"id":28,"text":1152,"url":28,"identifiers":1153},"10.1016\u002F0012-821X(83)90071-7",{"doi":1152},{"id":28,"text":1155,"url":28,"identifiers":1156},"10.1016\u002F0016-7037(84)90198-4",{"doi":1155},{"id":28,"text":1158,"url":28,"identifiers":1159},"10.2475\u002Fajs.270.1.54",{"doi":1158},{"id":28,"text":1161,"url":28,"identifiers":1162},"10.2475\u002Fajs.274.8.902",{"doi":1161},{"id":28,"text":1164,"url":28,"identifiers":1165},"10.1007\u002FBF00203057",{"doi":1164},{"id":28,"text":1167,"url":28,"identifiers":1168},"Carey J. W., 1992, The molar enthalpy of dehydration of cordierite., American Mineralogist, 77, 930",{},{"id":28,"text":1170,"url":28,"identifiers":1171},"Carman J. H., 1974, Synthetic sodium phlogopite and its two hydrates: Stabilities, properties and mineralogic implications., American Mineralogist, 59, 261",{},{"id":28,"text":1173,"url":28,"identifiers":1174},"10.1007\u002FBF00206796",{"doi":1173},{"id":28,"text":1176,"url":28,"identifiers":1177},"Carpenter M. A., 1994, Thermodynamics of non‐convergent cation ordering in minerals, II: spinels and the orthopyroxene solid solution., American Mineralogist, 79, 1068",{},{"id":28,"text":1179,"url":28,"identifiers":1180},"Carpenter M. A., 1994, Thermodynamics of non‐convergent cation ordering in minerals, III: order parameter coupling in K‐feldspar., American Mineralogist, 79, 1084",{},{"id":28,"text":1182,"url":28,"identifiers":1183},"Carrington D. P., 1995, Partial melting and phase relations in high‐grade metapelites: an experimental petrogenetic grid in KFMASH system., Contributions to Mineralogy and Petrology, 120, 270, 10.1007\u002FBF00306508",{"doi":1184},"10.1007\u002FBF00306508",{"id":28,"text":1186,"url":28,"identifiers":1187},"10.1016\u002F0016-7037(93)90126-H",{"doi":1186},{"id":28,"text":1189,"url":28,"identifiers":1190},"10.1007\u002FBF00202300",{"doi":1189},{"id":28,"text":1192,"url":28,"identifiers":1193},"10.1007\u002FBF00307751",{"doi":1192},{"id":28,"text":1195,"url":28,"identifiers":1196},"10.2138\u002Fam-1995-3-410",{"doi":1195},{"id":28,"text":1198,"url":28,"identifiers":1199},"10.1016\u002F0016-7037(75)90150-7",{"doi":1198},{"id":28,"text":1201,"url":28,"identifiers":1202},"10.1016\u002F0016-7037(78)90267-3",{"doi":1201},{"id":28,"text":1204,"url":28,"identifiers":1205},"10.1016\u002F0016-7037(83)90266-1",{"doi":1204},{"id":28,"text":1207,"url":28,"identifiers":1208},"Chatterjee N. D., 1976, Margarite stability and compatibility relations in the system CaO‐Al2O3‐SiO2‐H2O as a pressure‐temperature indicator., American Mineralogist, 61, 699",{},{"id":28,"text":1210,"url":28,"identifiers":1211},"10.1007\u002FBF00372834",{"doi":1210},{"id":28,"text":1213,"url":28,"identifiers":1214},"10.1007\u002FBF00371407",{"doi":1213},{"id":28,"text":1216,"url":28,"identifiers":1217},"10.1093\u002Fpetrology\u002F14.2.185",{"doi":1216},{"id":28,"text":1219,"url":28,"identifiers":1220},"10.1007\u002FBF00375213",{"doi":1219},{"id":28,"text":1222,"url":28,"identifiers":1223},"10.1007\u002FBF00381295",{"doi":1222},{"id":28,"text":1225,"url":28,"identifiers":1226},"Chopin C., 1983, Magnesiocarpholite and magnesiochloritoid: Two index minerals of pelitic blueschists and their preliminary phase relations in the model system MgO‐Al2O3‐SiO2‐H2O., American Journal of Science, 283, 72",{},{"id":28,"text":1228,"url":28,"identifiers":1229},"ChopinC.&SobolevN. V.1995;Principal mineralogical indicators of UHP in crustal rocks. In:Ultrahigh Pressure Metamorphism(eds Coleman R. G. & Wang X.) pp. 96–131Cambridge University Press",{"doi":1230},"10.1017\u002FCBO9780511573088.004",{"id":28,"text":1232,"url":28,"identifiers":1233},"Chou I. M., 1978, Calibration of oxygen buffers at elevated P and T using the hydrogen fugacity sensor., American Mineralogist, 63, 690",{},{"id":28,"text":1235,"url":28,"identifiers":1236},"Christy A. G., 1992, A 27Al and 29Si MAS NMR and infrared spectroscopic study of Al‐Si ordering in natural and synthetic sapphirine., American Mineralogist, 77, 8",{},{"id":28,"text":1238,"url":28,"identifiers":1239},"Circone S., 1992, Substitution of Al in phlogopite: High temperature solution calorimetry, heat capacities, and thermodynamic properties of the phlogopite‐eastonite join., American Mineralogist, 77, 1191",{},{"id":28,"text":1241,"url":28,"identifiers":1242},"10.1130\u002FMEM97-p345",{"doi":1241},{"id":28,"text":1244,"url":28,"identifiers":1245},"10.1127\u002Fejm\u002F3\u002F3\u002F0485",{"doi":1244},{"id":28,"text":1247,"url":28,"identifiers":1248},"10.1007\u002FBF00205262",{"doi":1247},{"id":28,"text":1250,"url":28,"identifiers":1251},"ComodiP.&ZanazziP. F.1994High pressure structural study of muscovite.IMA 16th General Meeting Pisa abstracts 79–80",{},{"id":28,"text":1253,"url":28,"identifiers":1254},"10.2138\u002Fam-1996-7-805",{"doi":1253},{"id":28,"text":1256,"url":28,"identifiers":1257},"10.2138\u002Fam-1997-1-208",{"doi":1256},{"id":28,"text":1259,"url":28,"identifiers":1260},"Connolly J. A. D., 1985, Experimental and thermodynamic analysis of prehnite., EOS, 66",{},{"id":28,"text":1262,"url":28,"identifiers":1263},"10.1007\u002FBF00321754",{"doi":1262},{"id":28,"text":1265,"url":28,"identifiers":1266},"10.1127\u002Fejm\u002F7\u002F4\u002F0883",{"doi":1265},{"id":28,"text":1268,"url":28,"identifiers":1269},"10.1016\u002F0016-7037(93)90612-Z",{"doi":1268},{"id":28,"text":1271,"url":28,"identifiers":1272},"10.1016\u002F0022-4596(83)90122-6",{"doi":1271},{"id":28,"text":1274,"url":28,"identifiers":1275},"Dickenson M. 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Experiments, thermodynamic analysis, and consequences for geothermometry., American Journal of Science, 283, 29",{},{"id":28,"text":1295,"url":28,"identifiers":1296},"10.1086\u002F626866",{"doi":1295},{"id":28,"text":1298,"url":28,"identifiers":1299},"10.2475\u002Fajs.264.1.37",{"doi":1298},{"id":28,"text":1301,"url":28,"identifiers":1302},"10.2138\u002Fam-1995-7-801",{"doi":1301},{"id":28,"text":1304,"url":28,"identifiers":1305},"Evans B. 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Cambridge University Press Cambridge",{},{"id":28,"text":1845,"url":28,"identifiers":1846},"10.1021\u002Fj100848a050",{"doi":1845},{"id":28,"text":1848,"url":28,"identifiers":1849},"Ralph R. L., 1984, Compressibility and crystal structure of andalusite at high pressure., American Mineralogist, 69, 513",{},{"id":28,"text":1851,"url":28,"identifiers":1852},"RaoB.&JohannesW.1979;Further data on the stability of staurolite+quartz.Neues Jahrbuch für Mineralogie Monatshefte 437–447",{},{"id":28,"text":1854,"url":28,"identifiers":1855},"Reeder R. 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A.1973;Thermochemistry of the garnets and some related compoundsUnpublished PhD thesis Department of Chemistry University of Chicago USA.",{},{"id":28,"text":1944,"url":28,"identifiers":1945},"10.1016\u002F0016-7037(88)90181-0",{"doi":1944},{"id":28,"text":1947,"url":28,"identifiers":1948},"10.1130\u002FMEM97-p75",{"doi":1947},{"id":28,"text":1950,"url":28,"identifiers":1951},"10.1007\u002Fs004100050175",{"doi":1950},{"id":28,"text":1953,"url":28,"identifiers":1954},"Smyth J. 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V., 1983, The extraction‐quench technique for determination of the thermodynamic properties of solute complexes: application to quartz solubility in fluid mixtures., American Mineralogist, 68, 731",{},{"id":28,"text":2029,"url":28,"identifiers":2030},"10.1093\u002Fpetrology\u002F27.2.541",{"doi":2029},{"id":28,"text":2032,"url":28,"identifiers":2033},"Wechsler B. A., 1984, Crystal structure of ilmenite (FeTiO2) at high temperature and at high pressure., American Mineralogist, 69, 176",{},{"id":28,"text":2035,"url":28,"identifiers":2036},"10.1016\u002F0016-7037(66)90109-8",{"doi":2035},{"id":28,"text":2038,"url":28,"identifiers":2039},"10.2138\u002Fam-1995-5-603",{"doi":2038},{"id":28,"text":2041,"url":28,"identifiers":2042},"10.2475\u002Fajs.281.8.1091",{"doi":2041},{"id":28,"text":2044,"url":28,"identifiers":2045},"10.1016\u002F0016-7037(89)90383-9",{"doi":2044},{"id":28,"text":2047,"url":28,"identifiers":2048},"Winter J. 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Progress in Experimental Petrology,, 3rd NERC report, 6, 17",{},{"id":28,"text":2056,"url":28,"identifiers":2057},"10.1007\u002FBF00320977",{"doi":2056},{"id":28,"text":2059,"url":28,"identifiers":2060},"Wunder B., 1993, Synthesis, stability and properties of Al2SiO4(OH)2: a fully hydrated analogue of topaz., American Mineralogist, 78, 285",{},{"id":28,"text":2062,"url":28,"identifiers":2063},"10.1029\u002F94GL00026",{"doi":2062},{"id":28,"text":2065,"url":28,"identifiers":2066},"Zhang L., 1992, Compressibility of grunerite., American Mineralogist, 77, 480",{},{"id":28,"text":2068,"url":28,"identifiers":2069},"Zharikov V. 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10.1007\u002FBF00205210",{"doi":4396},"10.1007\u002FBF00205210",{"id":28,"text":4398,"url":28,"identifiers":4399},"Yamamoto, 1977, The system MgO-SiO2-H2O at high pressures and temperatures -stability feld for hydroxyl-chondrodite, hydroxyl-clinohumite and 10Å-phase, American Journal of Science, 277, 288, 10.2475\u002Fajs.277.3.288",{"doi":4400},"10.2475\u002Fajs.277.3.288",{"id":28,"text":4402,"url":28,"identifiers":4403},"Yin, 1983, Displacement of equilibria of OH-tremolite and F-tremolite solid solution. I. Determination of the equilibrium P-T curve of OH-tremolite, EOS (Transactions of the American Geophysical Union), 64, 347",{},{"id":28,"text":4405,"url":28,"identifiers":4406},"Yoder, 1968, Akermanite and related melilite-bearing assemblages, Carnegie Institute of Washington Yearbook, 66, 471",{},{"id":28,"text":4408,"url":28,"identifiers":4409},"Yong, 2006, Heat capacity and phase equilibria of hollandite polymorph of KAlSi3O8, Physics and Chemistry of Minerals, 33, 167, 10.1007\u002Fs00269-006-0063-4",{"doi":4410},"10.1007\u002Fs00269-006-0063-4",{"id":28,"text":4412,"url":28,"identifiers":4413},"Yong, 2008, Heat capacity and phase equilibria of wadeite-type K2Si4O9, Contributions to Mineralogy and Petrology, 155, 137, 10.1007\u002Fs00410-007-0232-6",{"doi":4414},"10.1007\u002Fs00410-007-0232-6",{"id":28,"text":4416,"url":28,"identifiers":4417},"Zhang, 1992, High-pressure 57Fe resonance and compressibility of Ca(Fe,Mg)Si2O6 clinopyroxene, American Mineralogist, 77, 462",{},{"id":28,"text":4419,"url":28,"identifiers":4420},"Zhang, 1992, Compressibility of grunerite, American Mineralogist, 77, 480",{},{"id":28,"text":4422,"url":28,"identifiers":4423},"Zhang, 1993, Melting and subsolidus relations of SiO2 at 9-14 GPa, Journal of Geophysical Research, 98, 19785, 10.1029\u002F93JB02218",{"doi":4424},"10.1029\u002F93JB02218",{"id":28,"text":4426,"url":28,"identifiers":4427},"Zhang, 1996, In situ X-ray observations of the coesite-stishovite transition: reversed phase boundary and kinetics, Physics and Chemistry of Minerals, 23, 1, 10.1007\u002FBF00202987",{"doi":4428},"10.1007\u002FBF00202987",{"id":28,"text":4430,"url":28,"identifiers":4431},"Zhang, 1997, X-ray diffraction study of magnesite at high-pressure and high-temperature, Physics and Chemistry of Minerals, 24, 122, 10.1007\u002Fs002690050025",{"doi":4432},"10.1007\u002Fs002690050025",{"id":28,"text":4434,"url":28,"identifiers":4435},"Zhang, 1998, Effects of substitution in calcite-structure carbonates: thermoelastic properties, American Mineralogist, 83, 280, 10.2138\u002Fam-1998-3-411",{"doi":4436},"10.2138\u002Fam-1998-3-411",{"id":28,"text":4438,"url":28,"identifiers":4439},"Zhao, 1997, Thermoelastic equation of state of jadeite NaAlSi2O6: an energy-dispersive Rietveld refinement study of low symmetry and multiple phases diffraction, Geophysical Research Letters, 24, 5, 10.1029\u002F96GL03769",{"doi":4440},"10.1029\u002F96GL03769",{"id":28,"text":4442,"url":28,"identifiers":4443},"Zhao, 1989, X-ray diffraction data for graphite to 20 GPa, Physical Review B, 40, 993, 10.1103\u002FPhysRevB.40.993",{"doi":4444},"10.1103\u002FPhysRevB.40.993",{"id":28,"text":4446,"url":28,"identifiers":4447},"Zharikov, 1969, High temperature mineral equilibria in the system CaO-SiO2-CO2, Geochemistry International, 6, 853",{},{"id":28,"text":4449,"url":28,"identifiers":4450},"Zhu, 1994, Enthalpy of formation of wollastonite (CaSiO3) and anorthite (CaAl2Si2O8) by experimental phase equilibrium measurements and high-temperature solution calorimetry, American Mineralogist, 79, 134",{},{"id":28,"text":4452,"url":28,"identifiers":4453},"Ziegenbein, 1974, Wollastonitbildung aus Quartz und calcit bei Pf = 2, 4, und 6 kbar, Fortschritte der Mineralogie, 44, 77",{},{"id":4455,"createTime":4456,"updateTime":4456,"relativeEntities":4457,"slug":4458,"properties":4459,"entityType":964,"verifyStatus":26,"verifyTime":4456,"verifyNote":965,"languages":4470,"translateLanguages":28,"viewCount":32,"primaryUrl":4471,"fullTextUrl":28,"authors":4472,"publicationType":1005,"publisherRelationship":4509,"citationCount":4559,"citationInfo":4560,"publishDate":4568,"publishYear":4561,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":4569,"openAccess":28,"references":4570,"isForceReanalyzing":2076},"71a485d1-f4d7-4d73-9d90-9495cef4ac7d","2024-11-29T04:56:10.574+00:00",[],"Metamorphic-zircon-formation-by-solid-state-recrystallization-of-protolith-igneous-zircon",{"openalex":4460,"mag":4462,"abstract":4464,"title":4466,"doi":4468},{"VOID":4461},"W1521262137",{"VOID":4463},"1521262137",{"EN":4465},"\u003Cjats:p>Protolith zircon in high‐grade metagranitoids from Queensland, Australia, partially recrystallized during granulite‐grade metamorphism. We describe the zircon in detail using integrated cathodoluminescence, U–Pb isotope, trace element and electron backscatter diffraction pattern (EBSP) analyses. Primary igneous oscillatory zoning is partially modified or obliterated in areas within single crystals, but is well preserved in other areas. A variety of secondary internal structures are observed, with large areas of transgressive recrystallized zircon usually dominant. Associated with these areas are recrystallization margins, interpreted to be recrystallization fronts, that have conformable boundaries with transgressive recrystallized areas, but contrasting cathodoluminescence and trace element chemistry. Trace element analyses of primary and secondary structures provide compelling evidence for closed‐system solid‐state recrystallization. By this process, trace elements in the protolith zircon are purged during recrystallization and partitioned between the enriched recrystallization front and depleted recrystallized areas. However, recrystallization is not always efficient, often leaving a ‘memory’ of the protolith trace element and isotopic composition. This results in the measurement of ‘mixed’ U–Pb isotope ages. Nonetheless, the age of metamorphism has been determined. A correlation between apparent age and Th\u002FU ratio is indicative of incomplete re‐setting by partial recrystallization. Recrystallization is shown to probably not significantly affect Lu–Hf ages. Recrystallization has been determined by textural and trace element analysis and EBSP data not to have proceeded by sub‐grain rotation or local dissolution\u002Fre‐precipitation, but probably by grain‐boundary migration and defect diffusion. The formation of metamorphic zircon by solid‐state recrystallization is probably common to high‐grade terranes worldwide. The recognition of this process of formation is essential for correct interpretation of zircon‐derived U–Pb ages and subsequent tectonic models.\u003C\u002Fjats:p>",{"EN":4467},"Metamorphic zircon formation by solid‐state recrystallization of protolith igneous zircon",{"VOID":4469},"10.1046\u002Fj.1525-1314.2000.00266.x",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1046\u002Fj.1525-1314.2000.00266.x",[4473,4492],{"id":4474,"sortIndex":32,"researcher":28,"roles":4475,"affiliations":4476,"properties":4485,"displayName":4489,"givenName":28,"familyName":28},"569e0c0f-86bb-48dc-965c-e7b2d37e6e67",[],[4477],{"id":4478,"sortIndex":32,"affiliation":4479,"properties":28},"d83ecc79-3696-4812-a1bf-04488ef999ec",{"id":4478,"createTime":28,"updateTime":28,"relativeEntities":4480,"slug":28,"properties":4481,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4484,"statistic":28},[],{"title":4482},{"EN":4483},"Institute of Advanced Studies, Research School of Earth Sciences Australian National University  Canberra ACT 0200 Australia",[],{"orcid":4486,"title":4488,"openalex":4490},{"VOID":4487},"https:\u002F\u002Forcid.org\u002F0000-0002-7869-946X",{"EN":4489},"P. W. O. Hoskin",{"VOID":4491},"A5076715057",{"id":4493,"sortIndex":40,"researcher":28,"roles":4494,"affiliations":4495,"properties":4504,"displayName":4506,"givenName":28,"familyName":28},"4fd604f3-e342-48df-a8ea-e73b025e7a94",[],[4496],{"id":4497,"sortIndex":32,"affiliation":4498,"properties":28},"f5c84a2b-56f3-4765-9613-a3e2e9ec9a78",{"id":4497,"createTime":28,"updateTime":28,"relativeEntities":4499,"slug":28,"properties":4500,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4503,"statistic":28},[],{"title":4501},{"VI":4502},"Minerals Division, Australian Geological Survey Organisation, GPO Box 378, Canberra, ACT 2601, Australia",[],{"title":4505,"openalex":4507},{"EN":4506},"L. P. Black",{"VOID":4508},"A5113672852",{"url":28,"publisher":4510,"properties":4552},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":4511,"slug":872,"properties":4512,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":4517,"manageAffiliations":4526,"indexDatabases":4537,"url":943,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":4513,"eissn":4514,"issn":4515,"title":4516},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[4518,4522],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":4519,"label":4520,"description":4521,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},{"id":893,"createTime":28,"updateTime":28,"relativeEntities":4523,"label":4524,"description":4525,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":896},{},[4527,4532],{"id":900,"createTime":28,"updateTime":28,"relativeEntities":4528,"slug":28,"properties":4529,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4531,"statistic":28},[],{"title":4530},{"EN":904},[],{"id":907,"createTime":28,"updateTime":28,"relativeEntities":4533,"slug":28,"properties":4534,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4536,"statistic":28},[],{"title":4535},{"EN":911},[],[4538,4545],{"id":915,"indexDatabase":4539,"url":927,"indexYears":28,"academicFieldIds":4544,"indexDatabaseRanking":28},{"id":917,"createTime":28,"updateTime":28,"relativeEntities":4540,"label":4541,"description":4542,"key":924,"publicationTags":4543,"standard":28},[],{"EN":920,"VI":920},{"EN":922,"VI":923},[926,813],[929],{"id":931,"indexDatabase":4546,"url":937,"indexYears":938,"academicFieldIds":4551,"indexDatabaseRanking":942},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":4547,"label":4548,"description":4549,"key":781,"publicationTags":4550,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[940,941],{"issue":4553,"pages":4555,"volume":4557},{"VOID":4554},"4",{"VOID":4556},"423-439",{"VOID":4558},"18",1582,{"total":4559,"publishYear":4561,"statisticByYear":4562},2000,{"2012":206,"2013":162,"2014":4563,"2015":329,"2016":826,"2017":451,"2018":155,"2019":4564,"2020":690,"2021":4565,"2022":4566,"2023":4567,"2024":159},84,108,113,115,110,"2000-07-01",[926,942],[],{"id":4572,"createTime":4573,"updateTime":4573,"relativeEntities":4574,"slug":4575,"properties":4576,"entityType":964,"verifyStatus":26,"verifyTime":4573,"verifyNote":965,"languages":4586,"translateLanguages":28,"viewCount":32,"primaryUrl":4587,"fullTextUrl":28,"authors":4588,"publicationType":1005,"publisherRelationship":4621,"citationCount":4671,"citationInfo":4672,"publishDate":4675,"publishYear":4673,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":4676,"openAccess":28,"references":4677,"isForceReanalyzing":2076},"85b3b72c-f10f-4abc-9090-8b79bc624e55","2024-09-18T18:54:39.100+00:00",[],"An-internally-consistent-dataset-with-uncertainties-and-correlations-3-Applications-to-geobarometry-worked-examples-and-a-computer-program",{"openalex":4577,"mag":4579,"abstract":4581,"title":4583,"doi":4585},{"VOID":4578},"W1972909865",{"VOID":4580},"1972909865",{"EN":4582},"\u003Cjats:p>\u003Cjats:bold>Abstract\n\t\t\t\t\t\u003C\u002Fjats:bold> This paper provides methods and a description of a Pascal computer program, \u003Cjats:sc>thermocalc\u003C\u002Fjats:sc>, for various thermodynamic calculations using the thermodynamic dataset presented in earlier papers in this series (Holland & Powell, 1985; Powell & Holland, 1985). The dataset involves uncertainties on the thermodynamic parameters and therefore allows uncertainties to be calculated on results, for example in geothermometry and geobarometry. Recommendations are made for the uncertainties on activities to be used in calculations on rocks, particular emphasis being placed on preventing underestimates of these uncertainties at small mole fractions. Apposite examples of phase diagram and rock calculations are presented with ouput from \u003Cjats:sc>thermocalc\u003C\u002Fjats:sc>, demonstrating the utility of the program. Of the rock calculations, the most valuable are considered to be those involving simultaneous combination ‘least squares’of calculated conditions for a set of reactions applicable to a rock. This set of reactions involves the independent reactions which can be written between the end‐members in the minerals in a rock and in the thermodynamic dataset. In contrast to an approach based on specific geothermometers and geobarometers, this approach maximizes the benefit of having an internally consistent thermodynamic dataset. \u003Cjats:sc>thermocalc\u003C\u002Fjats:sc> is available in IBM PC and Mac versions, from Roger Powell for A$25 or Tim Holland for £10 per version.\u003C\u002Fjats:p>",{"EN":4584},"An internally consistent dataset with uncertainties and correlations: 3. Applications to geobarometry, worked examples and a computer program",{"VOID":1827},[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1525-1314.1988.tb00415.x",[4589,4605],{"id":4590,"sortIndex":32,"researcher":28,"roles":4591,"affiliations":4592,"properties":4601,"displayName":1002,"givenName":28,"familyName":28},"ee494f56-5e92-4bb9-b549-2b590307efa5",[],[4593],{"id":4594,"sortIndex":32,"affiliation":4595,"properties":28},"b268453f-26c3-4615-9352-3d058bbae81e",{"id":4594,"createTime":28,"updateTime":28,"relativeEntities":4596,"slug":28,"properties":4597,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4600,"statistic":28},[],{"title":4598},{"VI":4599},"Department of Geology, University of Melbourne, Parkville, Victoria 3052, Australia",[],{"orcid":4602,"title":4603,"openalex":4604},{"VOID":1000},{"EN":1002},{"VOID":1004},{"id":4606,"sortIndex":40,"researcher":28,"roles":4607,"affiliations":4608,"properties":4617,"displayName":985,"givenName":28,"familyName":28},"36a27fb2-9798-426b-b6f7-26f7669bb6dc",[],[4609],{"id":4610,"sortIndex":32,"affiliation":4611,"properties":28},"e49ad5f5-e1fc-4734-949d-a43ab22d71bb",{"id":4610,"createTime":28,"updateTime":28,"relativeEntities":4612,"slug":28,"properties":4613,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4616,"statistic":28},[],{"title":4614},{"VI":4615},"Department of Earth Sciences, University of Cambridge, Downing St, Cambridge CB2 3EQ, UK",[],{"orcid":4618,"title":4619,"openalex":4620},{"VOID":983},{"EN":985},{"VOID":987},{"url":28,"publisher":4622,"properties":4664},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":4623,"slug":872,"properties":4624,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":4629,"manageAffiliations":4638,"indexDatabases":4649,"url":943,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":4625,"eissn":4626,"issn":4627,"title":4628},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[4630,4634],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":4631,"label":4632,"description":4633,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},{"id":893,"createTime":28,"updateTime":28,"relativeEntities":4635,"label":4636,"description":4637,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":896},{},[4639,4644],{"id":900,"createTime":28,"updateTime":28,"relativeEntities":4640,"slug":28,"properties":4641,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4643,"statistic":28},[],{"title":4642},{"EN":904},[],{"id":907,"createTime":28,"updateTime":28,"relativeEntities":4645,"slug":28,"properties":4646,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4648,"statistic":28},[],{"title":4647},{"EN":911},[],[4650,4657],{"id":915,"indexDatabase":4651,"url":927,"indexYears":28,"academicFieldIds":4656,"indexDatabaseRanking":28},{"id":917,"createTime":28,"updateTime":28,"relativeEntities":4652,"label":4653,"description":4654,"key":924,"publicationTags":4655,"standard":28},[],{"EN":920,"VI":920},{"EN":922,"VI":923},[926,813],[929],{"id":931,"indexDatabase":4658,"url":937,"indexYears":938,"academicFieldIds":4663,"indexDatabaseRanking":942},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":4659,"label":4660,"description":4661,"key":781,"publicationTags":4662,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[940,941],{"issue":4665,"pages":4667,"volume":4669},{"VOID":4666},"2",{"VOID":4668},"173-204",{"VOID":4670},"6",1474,{"total":4671,"publishYear":4673,"statisticByYear":4674},1988,{"2012":152,"2013":201,"2014":206,"2015":328,"2016":200,"2017":280,"2018":162,"2019":50,"2020":157,"2021":567,"2022":151,"2023":206,"2024":130},"1988-03-01",[926,942],[4678,4681,4683,4686,4689,4692,4695,4698,4700,4703,4706,4708,4711,4713,4716],{"id":28,"text":4679,"url":28,"identifiers":4680},"10.1007\u002FBF00376220",{"doi":4679},{"id":28,"text":1213,"url":28,"identifiers":4682},{"doi":1213},{"id":28,"text":4684,"url":28,"identifiers":4685},"Ghent E.D., 1976, Plagioclose‐garnet‐Al2SiO5quartz: a potential geothermometer‐geobaro‐meter, American Mineralogist, 61, 710",{},{"id":28,"text":4687,"url":28,"identifiers":4688},"10.1007\u002FBF00373688",{"doi":4687},{"id":28,"text":4690,"url":28,"identifiers":4691},"Goldsmith J.R., 1980, The melting and breakdown reactions of anorthite at high pressures and temperatures, American Mineralogist, 65, 272",{},{"id":28,"text":4693,"url":28,"identifiers":4694},"Goldsmith J.R., 1985, The high‐low albite relations revealed by reversal of degree of order at high pressure, American Mineralogist, 70, 911",{},{"id":28,"text":4696,"url":28,"identifiers":4697},"10.1086\u002F628709",{"doi":4696},{"id":28,"text":1491,"url":28,"identifiers":4699},{"doi":1491},{"id":28,"text":4701,"url":28,"identifiers":4702},"10.1007\u002F978-1-4612-5871-1_7",{"doi":4701},{"id":28,"text":4704,"url":28,"identifiers":4705},"Newton R.C., 1982, Thermodynamic calibration of geobarometers based on the assemblages garnet‐plagioclase‐orthopyroxene‐clinopyroxene‐quartz, American Mineralogist, 67, 203",{},{"id":28,"text":3692,"url":28,"identifiers":4707},{"doi":3692},{"id":28,"text":4709,"url":28,"identifiers":4710},"10.1144\u002Fgsjgs.142.1.0029",{"doi":4709},{"id":28,"text":1824,"url":28,"identifiers":4712},{"doi":1824},{"id":28,"text":4714,"url":28,"identifiers":4715},"10.1007\u002FBF01046834",{"doi":4714},{"id":28,"text":4125,"url":28,"identifiers":4717},{"doi":4125},{"id":4719,"createTime":4720,"updateTime":4720,"relativeEntities":4721,"slug":4722,"properties":4723,"entityType":964,"verifyStatus":26,"verifyTime":4720,"verifyNote":965,"languages":4733,"translateLanguages":28,"viewCount":32,"primaryUrl":4734,"fullTextUrl":28,"authors":4735,"publicationType":1005,"publisherRelationship":4766,"citationCount":4816,"citationInfo":4817,"publishDate":4820,"publishYear":4818,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":4821,"openAccess":28,"references":4822,"isForceReanalyzing":2076},"f7f5d79d-e7cb-42ac-88d3-e2b9a2b3779e","2024-10-14T09:52:25.313+00:00",[],"An-enlarged-and-updated-internally-consistent-thermodynamic-dataset-with-uncertainties-and-correlations-the-system-K-sub-2-sub-O-Na-sub-2-sub-O-CaO-MgO-MnO-FeO-Fe-sub-2-sub-O-sub-3-sub-Al-sub-2-sub-O-sub-3-sub-TiO-sub-2-sub-SiO-sub-2-sub-C-H-sub-2-sub-O-sub-2-sub-",{"openalex":4724,"mag":4726,"abstract":4728,"title":4730,"doi":4732},{"VOID":4725},"W1980155029",{"VOID":4727},"1980155029",{"EN":4729},"\u003Cjats:p>We present, as a progress report, a revised and much enlarged version of the thermodynamic dataset given earlier (Holland & Powell, 1985). This new set includes data for 123 mineral and fluid end‐members made consistent with over 200 \u003Cjats:italic>P–T–X\u003C\u002Fjats:italic>\u003Cjats:sub>CO2\u003C\u002Fjats:sub>–\u003Cjats:italic>f\u003C\u002Fjats:italic>\u003Cjats:sub>O2\u003C\u002Fjats:sub> phase equilibrium experiments. Several improvements and advances have been made, in addition to the increased coverage of mineral phases: the data are now presented in three groups ranked according to reliability; a large number of iron‐bearing phases has been included through experimental and, in some cases, natural Fe:Mg partitioning data; H\u003Cjats:sub>2\u003C\u002Fjats:sub>O and CO\u003Cjats:sub>2\u003C\u002Fjats:sub> contents of cordierites are accounted for with the solution model of Kurepin (1985); simple Landau theory is used to model lambda anomalies in heat capacity and the Al\u002FSi order–disorder behaviour in some silicates, and Tschermak‐substituted end‐members have been derived for iron and magnesium end‐members of chlorite, talc, muscovite, biotite, pyroxene and amphibole.\u003C\u002Fjats:p>\u003Cjats:p>For the subset of data which overlap those of Berman (1988), it is encouraging to find both (1) very substantial agreement between the two sets of thermodynamic data and (2) that the two sets reproduce the phase equilibrium experimental brackets to a very similar degree of accuracy. The main differences in the two datasets involve size (123 as compared to 67 end‐members), the methods used in data reduction (least squares as compared to linear programming), and the provision for estimation of uncertainties with this dataset. For calculations on mineral assemblages in rocks, we aim to maximize the information available from the dataset, by combining the equilibria from all the reactions which can be written between the end‐members in the minerals. For phase diagram calculations, we calculate the compositions of complex solid solutions (together with \u003Cjats:italic>P\u003C\u002Fjats:italic> and \u003Cjats:italic>T\u003C\u002Fjats:italic>) involved in invariant, univariant and divariant assemblages. Moreover we strongly believe in attempting to assess the probable uncertainties in calculated equilibria and hence provide a framework for performing simple error propagation in all calculations in thermocalc, the computer program we offer for an effective use of the dataset and the calculation methods we advocate.\u003C\u002Fjats:p>",{"EN":4731},"An enlarged and updated internally consistent thermodynamic dataset with uncertainties and correlations: the system K\u003Csub>2\u003C\u002Fsub>O–Na\u003Csub>2\u003C\u002Fsub>O–CaO–MgO–MnO–FeO–Fe\u003Csub>2\u003C\u002Fsub>O\u003Csub>3\u003C\u002Fsub>–Al\u003Csub>2\u003C\u002Fsub>O\u003Csub>3\u003C\u002Fsub>–TiO\u003Csub>2\u003C\u002Fsub>–SiO\u003Csub>2\u003C\u002Fsub>–C–H\u003Csub>2\u003C\u002Fsub>–O\u003Csub>2\u003C\u002Fsub>",{"VOID":1494},[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1525-1314.1990.tb00458.x",[4736,4752],{"id":4737,"sortIndex":32,"researcher":28,"roles":4738,"affiliations":4739,"properties":4748,"displayName":985,"givenName":28,"familyName":28},"5527f4eb-e320-46c5-ac32-35a96810dea1",[],[4740],{"id":4741,"sortIndex":32,"affiliation":4742,"properties":28},"18d5b297-f098-4e1f-8499-9d5d0124ce5c",{"id":4741,"createTime":28,"updateTime":28,"relativeEntities":4743,"slug":28,"properties":4744,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":4747,"statistic":28},[],{"title":4745},{"VI":4746},"Department 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:4839},{"doi":1116},{"id":28,"text":4841,"url":28,"identifiers":4842},"10.1007\u002FBF00379451",{"doi":4841},{"id":28,"text":4844,"url":28,"identifiers":4845},"Berman R. G., 1987, Reviews in Mineralogy, 405",{},{"id":28,"text":1122,"url":28,"identifiers":4847},{"doi":1122},{"id":28,"text":2351,"url":28,"identifiers":4849},{"doi":2351},{"id":28,"text":2359,"url":28,"identifiers":4851},{"doi":2359},{"id":28,"text":1128,"url":28,"identifiers":4853},{"doi":1128},{"id":28,"text":1134,"url":28,"identifiers":4855},{"doi":1134},{"id":28,"text":2384,"url":28,"identifiers":4857},{"doi":2384},{"id":28,"text":1131,"url":28,"identifiers":4859},{"doi":1131},{"id":28,"text":2370,"url":28,"identifiers":4861},{"doi":2370},{"id":28,"text":4863,"url":28,"identifiers":4864},"Bohlen S. R., 1983, Thermodynamics and phase equilibrium of ferrosilite: Potential oxygen barometer in mantle rocks, EOS (Transactions of the American Geophysical Union), 64, 350",{},{"id":28,"text":2377,"url":28,"identifiers":4866},{"doi":2377},{"id":28,"text":4868,"url":28,"identifiers":4869},"Bohlen S. R., 1983, Experimental investigations and geological applications of equilibria in the system FeO–TiO2–Al2O3–SiO2–H2O, American Mineralogist, 68, 1049",{},{"id":28,"text":4871,"url":28,"identifiers":4872},"Boyd F. R., 1959, Researches in Geochemistry, 1",{},{"id":28,"text":1155,"url":28,"identifiers":4874},{"doi":1155},{"id":28,"text":2446,"url":28,"identifiers":4876},{"doi":2446},{"id":28,"text":4878,"url":28,"identifiers":4879},"10.1093\u002Fpetrology\u002F10.1.56",{"doi":4878},{"id":28,"text":4881,"url":28,"identifiers":4882},"Carman J. H., 1974, Synthetic sodium phlogopite and its hydrates: Stabilities, properties and mineralogic implications, American Mineralogist, 59, 261",{},{"id":28,"text":4884,"url":28,"identifiers":4885},"Carman J. H., 1983, Experimental studies on glaucophane stability, American Journal of Science, 283, 414",{},{"id":28,"text":4887,"url":28,"identifiers":4888},"10.1007\u002F978-94-009-2891-6_9",{"doi":4887},{"id":28,"text":4890,"url":28,"identifiers":4891},"10.1016\u002F0016-7037(85)90310-2",{"doi":4890},{"id":28,"text":1198,"url":28,"identifiers":4893},{"doi":1198},{"id":28,"text":1201,"url":28,"identifiers":4895},{"doi":1201},{"id":28,"text":4897,"url":28,"identifiers":4898},"10.1016\u002F0016-7037(81)90289-1",{"doi":4897},{"id":28,"text":1204,"url":28,"identifiers":4900},{"doi":1204},{"id":28,"text":2502,"url":28,"identifiers":4902},{"doi":2502},{"id":28,"text":2506,"url":28,"identifiers":4904},{"doi":2506},{"id":28,"text":4906,"url":28,"identifiers":4907},"Chatterjee N. D., 1974, Synthesis and upper thermal stability limit of 2M‐margarite, CaAl2Al2Si2O10(OH)2, Schweizerische Mineralogische und Petrologische Mitteilungen, 54, 753",{},{"id":28,"text":4909,"url":28,"identifiers":4910},"Chatterjee N. D., 1976, Margarite stability and compatibility relations in the system CaO–Al2O3–SiO2–H2O as a pressure‐temperature indicator, American Mineralogist, 61, 699",{},{"id":28,"text":2516,"url":28,"identifiers":4912},{"doi":2516},{"id":28,"text":1213,"url":28,"identifiers":4914},{"doi":1213},{"id":28,"text":4916,"url":28,"identifiers":4917},"Chernosky J. V., 1973, The stability of chrysotile, Mg3Si2O5(OH)4, and the free energy of formation of talc, Mg3Si4O10(OH)2, Geological Society of American Abstracts with Programs, 5, 575",{},{"id":28,"text":4919,"url":28,"identifiers":4920},"Chernosky J. V., 1974, The upper stability of clinochlore at low pressure and the free energy of formation of Mg‐cordierite, American Mineralogist, 59, 496",{},{"id":28,"text":4922,"url":28,"identifiers":4923},"Chernosky J. V., 1976, Gibbs free energy of enstatite, clinochlore and hydrous Mg‐cordierite evaluated from phase equilibrium data, EOS (Transactions of the American Geophysical Union), 57, 1020",{},{"id":28,"text":4925,"url":28,"identifiers":4926},"Chernosky J. V., 1976, The stability of anthophyllite–a re‐evaluation based on new experimental data, American Mineralogist, 61, 1145",{},{"id":28,"text":4928,"url":28,"identifiers":4929},"Chernosky J. V., 1978, The stability of clinochlore and quartz at low pressure, American Mineralogist, 63, 73",{},{"id":28,"text":4931,"url":28,"identifiers":4932},"Chernosky J. V., 1982, The stability of clinochrysotile, Canadian Mineralogist, 20, 19",{},{"id":28,"text":4934,"url":28,"identifiers":4935},"Chernosky J. V., 1979, The stability of anthophyllite in the presence of quartz, American Mineralogist, 84, 294",{},{"id":28,"text":4937,"url":28,"identifiers":4938},"Chernosky J. V., 1986, The stability of clinochlore in mixed volatile, CO2–H2O fluids, EOS (Transactions of the American Geophysical Union), 67, 407",{},{"id":28,"text":4940,"url":28,"identifiers":4941},"Chernosky J. V., 1986, Experimental reversal of the equilibrium: Clinochlore + 2 magnesite = 3 forsterite + spinel + 2CO2+ 4H2O, EOS (Transactions of the American Geophysical Union), 67, 1279",{},{"id":28,"text":4943,"url":28,"identifiers":4944},"Chernosky J. V., 1985, Equilibria in the system MgO–SiO2–H2O: experimental determination of the stability of Mg‐anthophyllite, American Mineralogist, 70, 223",{},{"id":28,"text":1216,"url":28,"identifiers":4946},{"doi":1216},{"id":28,"text":1222,"url":28,"identifiers":4948},{"doi":1222},{"id":28,"text":4950,"url":28,"identifiers":4951},"Chopin C., 1983, Magnesiocarpholite and magnesiochloritoid: Two index minerals of pelitic blueschists and their preliminary phase relations in the model system MgO–Al2O3–SiO2–H2O, American Journal of Science, 283, 72",{},{"id":28,"text":4953,"url":28,"identifiers":4954},"Colville P., 1966, Relationships between cell parameters and chemical compositions of monoclinic amphiboles, American Mineralogist, 51, 1727",{},{"id":28,"text":4956,"url":28,"identifiers":4957},"Conolly J. A. D., 1985, Experimental and thermodynamic analysis of prehnite, EOS (Transactions of the American Geophysical Union), 66, 388",{},{"id":28,"text":2630,"url":28,"identifiers":4959},{"doi":2630},{"id":28,"text":2660,"url":28,"identifiers":4961},{"doi":2660},{"id":28,"text":4963,"url":28,"identifiers":4964},"10.2475\u002Fajs.280.3.265",{"doi":4963},{"id":28,"text":4966,"url":28,"identifiers":4967},"10.1016\u002F0016-7037(81)90165-4",{"doi":4966},{"id":28,"text":4969,"url":28,"identifiers":4970},"Dutrow B. L., 1986, Upper thermal stability of staurolite + quartz at medium pressures: A reinvestigation, Terra Cognita, 6, 214",{},{"id":28,"text":2708,"url":28,"identifiers":4972},{"doi":2708},{"id":28,"text":1298,"url":28,"identifiers":4974},{"doi":1298},{"id":28,"text":4976,"url":28,"identifiers":4977},"Essene E. J., 1980, Thermodynamic properties and phase equilibria for fayalite, Geological Society of American Abstracts with Programs, 12, 422",{},{"id":28,"text":4979,"url":28,"identifiers":4980},"Fawcett J. J., 1966, Phase relationships of chlorites in the system MgO–Al2O3–SiO2–H2O, American Mineralogist, 61, 303",{},{"id":28,"text":1310,"url":28,"identifiers":4982},{"doi":1310},{"id":28,"text":1316,"url":28,"identifiers":4984},{"doi":1316},{"id":28,"text":1319,"url":28,"identifiers":4986},{"doi":1319},{"id":28,"text":1325,"url":28,"identifiers":4988},{"doi":1325},{"id":28,"text":1328,"url":28,"identifiers":4990},{"doi":1328},{"id":28,"text":4992,"url":28,"identifiers":4993},"10.2475\u002Fajs.271.1.37",{"doi":4992},{"id":28,"text":2848,"url":28,"identifiers":4995},{"doi":2848},{"id":28,"text":2852,"url":28,"identifiers":4997},{"doi":2852},{"id":28,"text":4999,"url":28,"identifiers":5000},"10.1093\u002Fpetrology\u002F9.3.444",{"doi":4999},{"id":28,"text":2859,"url":28,"identifiers":5002},{"doi":2859},{"id":28,"text":2863,"url":28,"identifiers":5004},{"doi":2863},{"id":28,"text":1343,"url":28,"identifiers":5006},{"doi":1343},{"id":28,"text":5008,"url":28,"identifiers":5009},"Goldsmith J. R., 1980, The melting and breakdown reactions of anorthite at high pressures and temperatures, American Mineralogist, 65, 272",{},{"id":28,"text":5011,"url":28,"identifiers":5012},"Goldsmith J. R., 1981, The join CaAl2Si2O8–H2O (anorthite–water) at elevated pressures and temperatures, American Mineralogist, 66, 1183",{},{"id":28,"text":1350,"url":28,"identifiers":5014},{"doi":1350},{"id":28,"text":2895,"url":28,"identifiers":5016},{"doi":2895},{"id":28,"text":5018,"url":28,"identifiers":5019},"Goldsmith J. R., 1977, Scapolite–plagioclase stability relations at high pressures and temperatures in the system NaAlSi3O8–CaAl2Si2O8–CaCO3–CaSO4, American Mineralogist, 62, 1063",{},{"id":28,"text":5021,"url":28,"identifiers":5022},"10.1086\u002F626865",{"doi":5021},{"id":28,"text":2915,"url":28,"identifiers":5024},{"doi":2915},{"id":28,"text":2919,"url":28,"identifiers":5026},{"doi":2919},{"id":28,"text":5028,"url":28,"identifiers":5029},"Greenwood H. J., 1967, Wollastonite: Stability in H2O–CO2 mixtures and occurrence in a contact‐metamorphic aureole near Salmo, British Columbia, Canada, American Mineralogist, 52, 1669",{},{"id":28,"text":5031,"url":28,"identifiers":5032},"Greenwood H. J., 1967, Researches in Geochemistry II, 542",{},{"id":28,"text":5034,"url":28,"identifiers":5035},"10.1016\u002F0021-9614(74)90230-4",{"doi":5034},{"id":28,"text":5037,"url":28,"identifiers":5038},"Guiraud M., 1989, Calculated mineral equilibria in the greenschist–blueschist–eclogite facies in Na2O–FeO–MgO–Al2O3–SiO2–H2O, Contributions to Mineralogy and Petrology",{},{"id":28,"text":5040,"url":28,"identifiers":5041},"Haas H., 1972, Diaspore‐corundum equilibrium determined by epitaxis of diaspore on corundum, American Mineralogist, 57, 1375",{},{"id":28,"text":2959,"url":28,"identifiers":5043},{"doi":2959},{"id":28,"text":1380,"url":28,"identifiers":5045},{"doi":1380},{"id":28,"text":2966,"url":28,"identifiers":5047},{"doi":2966},{"id":28,"text":1383,"url":28,"identifiers":5049},{"doi":1383},{"id":28,"text":5051,"url":28,"identifiers":5052},"10.2475\u002Fajs.254.8.468",{"doi":5051},{"id":28,"text":2976,"url":28,"identifiers":5054},{"doi":2976},{"id":28,"text":5056,"url":28,"identifiers":5057},"10.1144\u002FGSL.SP.1979.008.01.36",{"doi":5056},{"id":28,"text":5059,"url":28,"identifiers":5060},"Haselton H. T., 1982, Low temperature heat‐capacity measurements on synthetic CaAl2SiO6 pyroxene, EOS (Transactions of the American Geophysical Union), 63, 467",{},{"id":28,"text":5062,"url":28,"identifiers":5063},"Haselton H. T., 1984, Low temperature heat capacities of CaAl2SiO6 glass and pyroxene and thermal expansion of CaAl2SiO6 pyroxene, American Mineralogist, 69, 481",{},{"id":28,"text":1404,"url":28,"identifiers":5065},{"doi":1404},{"id":28,"text":1398,"url":28,"identifiers":5067},{"doi":1398},{"id":28,"text":5069,"url":28,"identifiers":5070},"Hays J. F., 1967, Lime‐alumina‐silica, Carnegie Institute of Washington Yearbook, 65, 234",{},{"id":28,"text":5072,"url":28,"identifiers":5073},"Hazen R. M., 1977, Effects of temperature and pressure on the crystal structure of ferromagnesian olivine, American Mineralogist, 62, 286",{},{"id":28,"text":5075,"url":28,"identifiers":5076},"Hazen R. M., 1978, The crystal structures and compressibilities of layer minerals at high pressure. II. Phlogopite and chlorite, American Mineralogist, 63, 293",{},{"id":28,"text":5078,"url":28,"identifiers":5079},"Heinrich W., 1980, Die obere Stabilitätsgrenze von Lawsonit plus Albit bzw Jadeit, Fortschritte der Mineralogie, 58, 49",{},{"id":28,"text":5081,"url":28,"identifiers":5082},"Helgeson H. C., 1978, Summary and critique of the thermodynamic properties of rock‐forming minerals, American Journal of Science, 278, 229",{},{"id":28,"text":5084,"url":28,"identifiers":5085},"Hemingway B. S., 1987, Quartz: Heat capacities from 340 to 1000 K and revised values for the thermodynamic properties, American Mineralogist, 72, 273",{},{"id":28,"text":5087,"url":28,"identifiers":5088},"Hemingway B. S., 1986, Akermanite: Phase transitions in heat capacity and thermal expansion, and revised thermodynamic data, Canadian Mineralogist, 24, 425",{},{"id":28,"text":5090,"url":28,"identifiers":5091},"Hemingway B. S., 1984, Heat capacity and thermodynamic functions for gehlenite and staurolite: with comments on the Schottky anomaly in the heat capacity of Staurolite, American Mineralogist, 69, 307",{},{"id":28,"text":5093,"url":28,"identifiers":5094},"Henderson C. E., 1983, Thermodynamics and phase equilibria of clinochlore (Mg5Al)(Si3Al)10(OH)8, EOS (Transactions of the American Geophysical Union), 64, 466",{},{"id":28,"text":3050,"url":28,"identifiers":5096},{"doi":3050},{"id":28,"text":5098,"url":28,"identifiers":5099},"Hewitt D. A., 1973, Stability of the assemblage muscovite–calcite–quartz, American Mineralogist, 58, 785",{},{"id":28,"text":5101,"url":28,"identifiers":5102},"Hewitt D. A., 1975, Stability of the assemblage phlogopite–calcite–quartz, American Mineralogist, 60, 391",{},{"id":28,"text":5104,"url":28,"identifiers":5105},"Hewitt D. A., 1975, Physical properties of some synthetic Fe–Mg–Al trioctahedral biotites, American Mineralogist, 60, 854",{},{"id":28,"text":1458,"url":28,"identifiers":5107},{"doi":1458},{"id":28,"text":1461,"url":28,"identifiers":5109},{"doi":1461},{"id":28,"text":1464,"url":28,"identifiers":5111},{"doi":1464},{"id":28,"text":5113,"url":28,"identifiers":5114},"Holdaway M. J., 1987, H content of staurolite as determined by H extraction line and ion microprobe, American Mineralogist, 71, 1135",{},{"id":28,"text":1470,"url":28,"identifiers":5116},{"doi":1470},{"id":28,"text":1476,"url":28,"identifiers":5118},{"doi":1476},{"id":28,"text":5120,"url":28,"identifiers":5121},"Holland T. J. B., 1980, The reaction albite = jadeite + quartz determined experimentally in the range 600–1200 °C, American Mineralogist, 65, 129",{},{"id":28,"text":5123,"url":28,"identifiers":5124},"Holland T. J. B., 1984, Stability relations of ortho‐ and clinozoisite, NERC Progress in Experimental Petrology, Progress Report, 6, 185",{},{"id":28,"text":1482,"url":28,"identifiers":5126},{"doi":1482},{"id":28,"text":5128,"url":28,"identifiers":5129},"Holland T. J. B., 1989, the dependence of entropy on volume for silicate and oxide minerals: a review and a predictive model, American Mineralogist, 74, 5",{},{"id":28,"text":5131,"url":28,"identifiers":5132},"10.1007\u002FBF00372259",{"doi":5131},{"id":28,"text":1491,"url":28,"identifiers":5134},{"doi":1491},{"id":28,"text":5136,"url":28,"identifiers":5137},"Holm J. L., 1966, The thermodynamic properties of the aluminum silicates, American Mineralogist, 51, 1608",{},{"id":28,"text":5139,"url":28,"identifiers":5140},"10.1007\u002FBF00383105",{"doi":5139},{"id":28,"text":1525,"url":28,"identifiers":5142},{"doi":1525},{"id":28,"text":1531,"url":28,"identifiers":5144},{"doi":1531},{"id":28,"text":5146,"url":28,"identifiers":5147},"Huang W. L., 1975, Melting and subsolidus phase relationships for CaSiO3 to 35 kilobars pressure, American Mineralogist, 60, 213",{},{"id":28,"text":5149,"url":28,"identifiers":5150},"Huckenholz H. G., 1975, Grossularite, its solidus and liquidus relations in the system CaO–Al2O3–SiO2–H2O up to 10kbars, Neues Jahrbuch für Mineralogie Abhandlungen, 124, 1",{},{"id":28,"text":5152,"url":28,"identifiers":5153},"Huckenholz H. G., 1971, Andradite stability relations in the CaSiO3–Fe2O3 join up to 30 kb, Neues Jahrbuch für Mineralogie Abhandlungen, 114, 246",{},{"id":28,"text":5155,"url":28,"identifiers":5156},"Huebner J. S., 1969, Stability relations of rhodachrosite in the system manganese–carbon–oxygen, American Mineralogist, 54, 457",{},{"id":28,"text":5158,"url":28,"identifiers":5159},"Huebner J. S., 1968, Rhodachrosite decarbonation in the system MnO–SiO2–CO2, Geological Society of America Special Publication, 121, 144",{},{"id":28,"text":3189,"url":28,"identifiers":5161},{"doi":3189},{"id":28,"text":3203,"url":28,"identifiers":5163},{"doi":3203},{"id":28,"text":1537,"url":28,"identifiers":5165},{"doi":1537},{"id":28,"text":5167,"url":28,"identifiers":5168},"Ivaldi G., 1988, Crystal structure at 25 and 700° of magnesiochloritoid from a high pressure assemblage (Monte Rosa), American Mineralogist, 73, 358",{},{"id":28,"text":5170,"url":28,"identifiers":5171},"Jacobs G. K., 1979, Experimental and thermodynamic analysis of decarbonation reactions and the high temperature heat capacity of calcite, EOS (Transactions of the American Geophysical Union), 60, 406",{},{"id":28,"text":5173,"url":28,"identifiers":5174},"Jacobs G. K., 1981, Devolatilization equilibria in H2O–CO2 and H2O–CO2–NaCl fluids: an experimental and thermodynamic evaluation at elevated pressures and temperatures, American Mineralogist, 66, 1135",{},{"id":28,"text":3273,"url":28,"identifiers":5176},{"doi":3273},{"id":28,"text":3277,"url":28,"identifiers":5178},{"doi":3277},{"id":28,"text":1558,"url":28,"identifiers":5180},{"doi":1558},{"id":28,"text":5182,"url":28,"identifiers":5183},"Jenkins D. M., 1986, Phase equilibria and crystallochemical properties of Mg‐chlorite, American Mineralogist, 71, 924",{},{"id":28,"text":1564,"url":28,"identifiers":5185},{"doi":1564},{"id":28,"text":3297,"url":28,"identifiers":5187},{"doi":3297},{"id":28,"text":3301,"url":28,"identifiers":5189},{"doi":3301},{"id":28,"text":3305,"url":28,"identifiers":5191},{"doi":3305},{"id":28,"text":3309,"url":28,"identifiers":5193},{"doi":3309},{"id":28,"text":1573,"url":28,"identifiers":5195},{"doi":1573},{"id":28,"text":1582,"url":28,"identifiers":5197},{"doi":1582},{"id":28,"text":3352,"url":28,"identifiers":5199},{"doi":3352},{"id":28,"text":3360,"url":28,"identifiers":5201},{"doi":3360},{"id":28,"text":3371,"url":28,"identifiers":5203},{"doi":3371},{"id":28,"text":5205,"url":28,"identifiers":5206},"Kerrick D. M., 1984, The andalusite–sillimanite equilibrium revisited, Geological Society of America Abstracts with Programs, 16, 558",{},{"id":28,"text":3391,"url":28,"identifiers":5208},{"doi":3391},{"id":28,"text":5210,"url":28,"identifiers":5211},"Klein C., 1978, Regional metamorphism of Proterozoic iron‐formation, Labrador Trough, Canada, American Mineralogist, 63, 898",{},{"id":28,"text":5213,"url":28,"identifiers":5214},"Ko H. C., 1977, Proceedings of the 7th Symposium on Thermophysical Properties. Washington D.C. (American Society of Mechanical Engineers), 392",{},{"id":28,"text":5216,"url":28,"identifiers":5217},"Koziol A., 1986, Definition of anorthite = grossular + kyanite + quartz in the range 650–1250 °C, Geological Society of America Abstracts with Programs, 188, 661",{},{"id":28,"text":5219,"url":28,"identifiers":5220},"10.1007\u002FBF00376087",{"doi":5219},{"id":28,"text":5222,"url":28,"identifiers":5223},"10.1016\u002F0012-821X(73)90071-X",{"doi":5222},{"id":28,"text":5225,"url":28,"identifiers":5226},"Kurepin V. A., 1985, H2O and CO2 contents of cordierite as an indicator of thermodynamic conditions of formation, Geochemistry International, 22, 148",{},{"id":28,"text":5228,"url":28,"identifiers":5229},"Lager G. A., 1978, High‐temperature study of six olivines, American Mineralogist, 63, 365",{},{"id":28,"text":5231,"url":28,"identifiers":5232},"Lange R. A., 1986, Phase transitions in leucite KAlSiO6, orthorhombic KAlSiO4, and their iron analogues (KFeSi2O6, KFeSiO4), American Mineralogist, 71, 937",{},{"id":28,"text":5234,"url":28,"identifiers":5235},"Latard D., 1981, Experimental results bearing on the stability of the blueschist facies minerals deerite, howieite, and zussmanite, and their petrological significance, Bulletin Mineralogique, 104, 431, 10.3406\u002Fbulmi.1981.7490",{"doi":5236},"10.3406\u002Fbulmi.1981.7490",{"id":28,"text":1640,"url":28,"identifiers":5238},{"doi":1640},{"id":28,"text":5240,"url":28,"identifiers":5241},"Levien L., 1981, High pressure crystal structure and compressibility of coesite, American Mineralogist, 66, 324",{},{"id":28,"text":5243,"url":28,"identifiers":5244},"Lindsley D. H., 1966, P–T projection for part of the system kalsilite–silica, Carnegie Institute of Washington Yearbook, 65, 244",{},{"id":28,"text":5246,"url":28,"identifiers":5247},"Lindsley D. H., 1981, The formation of pigeonite on the join hedenbergite‐ferrosilate at 11.5 kbar: experiments and a solution model, American Mineralogist, 66, 1175",{},{"id":28,"text":5249,"url":28,"identifiers":5250},"Lindsley D. H., 1983, Pyroxene thermometry, American Mineralogist, 68, 477",{},{"id":28,"text":5252,"url":28,"identifiers":5253},"Liou J. G., 1971, Synthesis and stability of prehnite, Ca2Al2Si3O10(OH)2, American Mineralogist, 56, 507",{},{"id":28,"text":1661,"url":28,"identifiers":5255},{"doi":1661},{"id":28,"text":5257,"url":28,"identifiers":5258},"Liou J. G., 1974, Stability relations of andradite–quartz in the system Ca–Fe–Si–O–H, American Mineralogist, 59, 1016",{},{"id":28,"text":3540,"url":28,"identifiers":5260},{"doi":3540},{"id":28,"text":3581,"url":28,"identifiers":5262},{"doi":3581},{"id":28,"text":3594,"url":28,"identifiers":5264},{"doi":3594},{"id":28,"text":5266,"url":28,"identifiers":5267},"Massonne H.‐J., 1986, High pressure syntheses and X‐ray properties of white micas in the system K2O–MgO–Al2O3–SiO2–H2O, Neues Jahrbuch für Mineralogie Abhandlungen, 153, 177",{},{"id":28,"text":1701,"url":28,"identifiers":5269},{"doi":1701},{"id":28,"text":5271,"url":28,"identifiers":5272},"Massonne H. J., 1981, Experimentelle der Reaktionskurve Chlorit + Quartz = Talk + Disthen im System MgO–Al2O3–SiO2–H2O, Fortschritte der Mineralogie, 59, 122",{},{"id":28,"text":5274,"url":28,"identifiers":5275},"Matsui Y., 1974, Iron (II)‐magnesium exchange equilibrium between olivine and calcium‐free pyroxene over a temperature range 800 to 1300°, Bulletin de Societe de Mineralogie et de Cristallographie, 97, 122",{},{"id":28,"text":5277,"url":28,"identifiers":5278},"10.2475\u002Fajs.265.1.28",{"doi":5277},{"id":28,"text":3638,"url":28,"identifiers":5280},{"doi":3638},{"id":28,"text":3634,"url":28,"identifiers":5282},{"doi":3634},{"id":28,"text":5284,"url":28,"identifiers":5285},"Metz G. W., 1983, The heat capacity and phase equilibria of almandine, EOS (Transactions of the American Geophysical Union), 64, 346",{},{"id":28,"text":5287,"url":28,"identifiers":5288},"Miller Ch., 1986, Alpine high‐pressure metamorphism in the Eastern Alps, Schweitzerische Mineralogische und Petrologische Mitteilungen, 66, 139",{},{"id":28,"text":5290,"url":28,"identifiers":5291},"10.1029\u002FJB085iB12p06983",{"doi":5290},{"id":28,"text":5293,"url":28,"identifiers":5294},"10.2475\u002Fajs.286.7.540",{"doi":5293},{"id":28,"text":5296,"url":28,"identifiers":5297},"Moecher D. P., 1985, S298 of an intermediate scapolite and phase equilibrium constraints on Al–Si disorder, EOS (Transactions of the American Geophysical Union), 66, 390",{},{"id":28,"text":5299,"url":28,"identifiers":5300},"Moore P. B., 1972, Atomic arrangement of merwinite, Ca3Mg“SiO4”2, an unusual dense‐packed structure of geophysical interest, American Mineralogist, 57, 1355",{},{"id":28,"text":1737,"url":28,"identifiers":5302},{"doi":1737},{"id":28,"text":3696,"url":28,"identifiers":5304},{"doi":3696},{"id":28,"text":5306,"url":28,"identifiers":5307},"10.1126\u002Fscience.151.3715.1222",{"doi":5306},{"id":28,"text":3706,"url":28,"identifiers":5309},{"doi":3706},{"id":28,"text":3710,"url":28,"identifiers":5311},{"doi":3710},{"id":28,"text":3688,"url":28,"identifiers":5313},{"doi":3688},{"id":28,"text":3692,"url":28,"identifiers":5315},{"doi":3692},{"id":28,"text":5317,"url":28,"identifiers":5318},"Newton R. C., 1978, Volume behaviour of silicate solid solutions, American Mineralogist, 65, 733",{},{"id":28,"text":5320,"url":28,"identifiers":5321},"10.1007\u002FBF01164524",{"doi":5320},{"id":28,"text":5323,"url":28,"identifiers":5324},"10.1111\u002Fj.1525-1314.1986.tb00338.x",{"doi":5323},{"id":28,"text":3714,"url":28,"identifiers":5326},{"doi":3714},{"id":28,"text":5328,"url":28,"identifiers":5329},"Nitsch K.‐H., 1974, Neue Erkentnisse zur Stabilitat fur Lawsonit, Fortschritte der Mineralogie, 51, 34",{},{"id":28,"text":5331,"url":28,"identifiers":5332},"Nitsch K.‐H., 1981, Experimentelle bestimmung der gleichgewichtsdaten die reaktion Margarit + Quartz = Anorthit + Andalusit\u002FDisthen + H2O, Fortschritte der Mineralogie, 59, 139",{},{"id":28,"text":1772,"url":28,"identifiers":5334},{"doi":1772},{"id":28,"text":3763,"url":28,"identifiers":5336},{"doi":3763},{"id":28,"text":5338,"url":28,"identifiers":5339},"Perkins D., The stability of Mg‐rich garnet in the system CaO–MgO–Al2O3–SiO2 at 1000–1300 °C and high pressure, American Mineralogist, 68, 355",{},{"id":28,"text":5341,"url":28,"identifiers":5342},"10.1007\u002FBF00371508",{"doi":5341},{"id":28,"text":3842,"url":28,"identifiers":5344},{"doi":3842},{"id":28,"text":1809,"url":28,"identifiers":5346},{"doi":1809},{"id":28,"text":3849,"url":28,"identifiers":5348},{"doi":3849},{"id":28,"text":4709,"url":28,"identifiers":5350},{"doi":4709},{"id":28,"text":1824,"url":28,"identifiers":5352},{"doi":1824},{"id":28,"text":1827,"url":28,"identifiers":5354},{"doi":1827},{"id":28,"text":5356,"url":28,"identifiers":5357},"Powell R., 1989, Calculated mineral equilibria in the pelite system. KFMASH (K2O–FeO–MgO–Al2O3–SiO2–H2O), American Mineralogist",{},{"id":28,"text":5359,"url":28,"identifiers":5360},"Puhan D., 1978, Experimental study of the reaction: dolomite + K‐feldspar + H2O = phlogopite + calcite + CO2 at the total gas pressure of 4000 and 6000 bars, Neues Jahrbuch für Mineralogie Monatschefte, 3, 110",{},{"id":28,"text":3894,"url":28,"identifiers":5362},{"doi":3894},{"id":28,"text":5364,"url":28,"identifiers":5365},"Rao B., 1979, Further data on the stability of staurolite + quartz, Neues Jahrbuch für Mineralogie Monat-shefte, 437",{},{"id":28,"text":5367,"url":28,"identifiers":5368},"10.2475\u002Fajs.277.1.1",{"doi":5367},{"id":28,"text":1866,"url":28,"identifiers":5370},{"doi":1866},{"id":28,"text":1869,"url":28,"identifiers":5372},{"doi":1869},{"id":28,"text":1872,"url":28,"identifiers":5374},{"doi":1872},{"id":28,"text":3959,"url":28,"identifiers":5376},{"doi":3959},{"id":28,"text":5378,"url":28,"identifiers":5379},"Robie R. A., 1967, Selected X‐ray crystallographic data, molar volumes, and densities of minerals and related substances, United States Geological Survey Bulletin, 1248, 87",{},{"id":28,"text":5381,"url":28,"identifiers":5382},"Robie R. A., 1982, Heat capacity and entropy of fayalite Fe2SiO4) between 5.1 and 383 K: Comparison of calorimetric and equilibrium values for the QFM buffer reaction, American Mineralogist, 67, 463",{},{"id":28,"text":5384,"url":28,"identifiers":5385},"Robie R. A., 1984, Heat capacities and entropies of rhodachrosite (MnCO3) and siderite (FeCO3) between 5 and 600 K, American Mineralogist, 69, 349",{},{"id":28,"text":5387,"url":28,"identifiers":5388},"Robie R. A., 1984, Heat capacities and entropies of phlogopite (KMg3[AlSi3O10](OH)2 and paragonite (NaAl2)[AlSi3O10](OH)2) between 5 and 900 K and estimates of the enthalpies and Gibbs free energies of formation, American Mineralogist, 69, 858",{},{"id":28,"text":5390,"url":28,"identifiers":5391},"Robie R. A., 1979, Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (105 Pascals) pressure and at higher temperatures, United States Geological Survey Bulletin, 1452, 456",{},{"id":28,"text":5393,"url":28,"identifiers":5394},"Robie R. A., 1982, Heat capacities and entropies of Mg2SiO4, Mn2SiO4, and Ca2SiO4 between 5 and 380 K, American Mineralogist, 67, 470",{},{"id":28,"text":1899,"url":28,"identifiers":5396},{"doi":1899},{"id":28,"text":5398,"url":28,"identifiers":5399},"Robinson P., 1982, Reviews in mineralogy, vol 9B, Amphiboles: petrology and experimental phase relations, 787",{},{"id":28,"text":4714,"url":28,"identifiers":5401},{"doi":4714},{"id":28,"text":5403,"url":28,"identifiers":5404},"10.1111\u002Fj.1525-1314.1986.tb00345.x",{"doi":5403},{"id":28,"text":5406,"url":28,"identifiers":5407},"Scarfe C. M., 1966, An experimental study bearing on the absence of leucite in plutonic rocks, American Mineralogist, 51, 726",{},{"id":28,"text":1917,"url":28,"identifiers":5409},{"doi":1917},{"id":28,"text":5411,"url":28,"identifiers":5412},"Schramke J. A., 1982, The experimental determination of the brucite = periclase + H2O equilibrium with a new volumetric technique, American Mineralogist, 67, 269",{},{"id":28,"text":5414,"url":28,"identifiers":5415},"Schreyer W., 1968, A reconnaissance study of the system MgO–Al2O3–SiO2–H2O at pressures between 10 and 25 kb, Carnegie Institute of Washington Yearbook, 66, 380",{},{"id":28,"text":5417,"url":28,"identifiers":5418},"Schreyer W., 1969, High pressure phases in the system MgO–Al2O3–SiO2–H2O, American Journal of Science, 267, 407",{},{"id":28,"text":1929,"url":28,"identifiers":5420},{"doi":1929},{"id":28,"text":5422,"url":28,"identifiers":5423},"Seidel E., 1981, Fe‐Mg‐verteilung zurischen koexistierenden karpholithe und chloritoiden, Fortschritte der Mineralogie, 59, 180",{},{"id":28,"text":4065,"url":28,"identifiers":5425},{"doi":4065},{"id":28,"text":4069,"url":28,"identifiers":5427},{"doi":4069},{"id":28,"text":1932,"url":28,"identifiers":5429},{"doi":1932},{"id":28,"text":4076,"url":28,"identifiers":5431},{"doi":4076},{"id":28,"text":4061,"url":28,"identifiers":5433},{"doi":4061},{"id":28,"text":1938,"url":28,"identifiers":5435},{"doi":1938},{"id":28,"text":5437,"url":28,"identifiers":5438},"Shmulovich K. J., 1974, Experimental study of phase equilibria in the system CaO–Al2O3–SiO2–CO2. (In Russian), Geokhimiya, 1272",{},{"id":28,"text":1947,"url":28,"identifiers":5440},{"doi":1947},{"id":28,"text":4118,"url":28,"identifiers":5442},{"doi":4118},{"id":28,"text":4125,"url":28,"identifiers":5444},{"doi":4125},{"id":28,"text":4132,"url":28,"identifiers":5446},{"doi":4132},{"id":28,"text":4147,"url":28,"identifiers":5448},{"doi":4147},{"id":28,"text":4163,"url":28,"identifiers":5450},{"doi":4163},{"id":28,"text":5452,"url":28,"identifiers":5453},"Sueno S., 1976, Orthoferrosilite: High temperature crystal chemistry, American Mineralogist, 61, 38",{},{"id":28,"text":5455,"url":28,"identifiers":5456},"Suwa Y., 1976, Stability of synthetic andradite at atmospheric pressure, American Mineralogist, 61, 26",{},{"id":28,"text":5458,"url":28,"identifiers":5459},"Taylor L. A., 1970, Thermal expansion of pyrophyllite, Carnegie Institute of Washington Yearbook, 69, 193",{},{"id":28,"text":2005,"url":28,"identifiers":5461},{"doi":2005},{"id":28,"text":2014,"url":28,"identifiers":5463},{"doi":2014},{"id":28,"text":4309,"url":28,"identifiers":5465},{"doi":4309},{"id":28,"text":4313,"url":28,"identifiers":5467},{"doi":4313},{"id":28,"text":5469,"url":28,"identifiers":5470},"Wechsler B. A., 1984, Crystal structure of ilmenite (FeTiO3) at high temperature and at high pressure, American Mineralogist, 69, 176",{},{"id":28,"text":5472,"url":28,"identifiers":5473},"10.2475\u002Fajs.272.8.735",{"doi":5472},{"id":28,"text":5475,"url":28,"identifiers":5476},"10.2475\u002Fajs.280.5.385",{"doi":5475},{"id":28,"text":4339,"url":28,"identifiers":5478},{"doi":4339},{"id":28,"text":5480,"url":28,"identifiers":5481},"Will T. M., 1989, Calculated greenschist facies mineral equilibria in the system CaO–MgO–FeO–Al2O3–SiO2–H2O–CO2, Contributions to Mineralogy and Petrology",{},{"id":28,"text":5483,"url":28,"identifiers":5484},"Yin H.‐A., 1983, Displacement of equilibria of OH‐tremolite and F‐tremolite solid solution. I. Determination of the equilibrium P–T curve of OH‐tremolite, EOS (Transactions of the American Geophysical Union), 64, 347",{},{"id":28,"text":5486,"url":28,"identifiers":5487},"Yoder H. S., 1968, Akermanite and related melilite‐bearing assemblages, Carnegie Institute of Washington Yearbook, 66, 471",{},{"id":28,"text":5489,"url":28,"identifiers":5490},"Zharkov V. A., 1969, High temperature mineral equilibria in the system CaO–SiO2–CO2, Geochemistry International, 6, 853",{},{"id":28,"text":5492,"url":28,"identifiers":5493},"Ziegenbein D., 1974, Wollastonitbildung aus Quartz und Calcit bei Pf = 2, 4, und 6 kb, Fortschritte der Mineralogie, 44, 77",{},{"id":5495,"createTime":5496,"updateTime":5496,"relativeEntities":5497,"slug":5498,"properties":5499,"entityType":964,"verifyStatus":26,"verifyTime":5496,"verifyNote":965,"languages":5510,"translateLanguages":28,"viewCount":32,"primaryUrl":5511,"fullTextUrl":28,"authors":5512,"publicationType":1005,"publisherRelationship":5581,"citationCount":5631,"citationInfo":5632,"publishDate":5637,"publishYear":5633,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":5638,"openAccess":28,"references":5639,"isForceReanalyzing":2076},"4475c990-0e7d-44e2-ba74-4b5433aa61dd","2024-09-04T15:01:05.934+00:00",[],"Raman-spectra-of-carbonaceous-material-in-metasediments-a-new-geothermometer",{"openalex":5500,"mag":5502,"abstract":5504,"title":5506,"doi":5508},{"VOID":5501},"W1960465926",{"VOID":5503},"1960465926",{"EN":5505},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Metasedimentary rocks generally contain carbonaceous material (CM) deriving from the evolution of organic matter originally present in the host sedimentary rock. During metamorphic processes, this organic matter is progressively transformed into graphite \u003Cjats:italic>s.s.\u003C\u002Fjats:italic> and the degree of organisation of CM is known as a reliable indicator of metamorphic grade. In this study, the degree of organisation of CM was systematically characterised by Raman microspectroscopy across several Mesozoic and Cenozoic reference metamorphic belts. This degree of organisation, including within‐sample heterogeneity, was quantified by the relative area of the defect band (R2 ratio). The results from the Schistes Lustrés (Western Alps) and Sanbagawa (Japan) cross‐sections show that (1) even through simple visual inspection, changes in the CM Raman spectrum appear sensitive to variations of metamorphic grade, (2) there is an excellent agreement between the R2 values calculated for the two sections when considering samples with an equivalent metamorphic grade, and (3) the evolution of the R2 ratio with metamorphic grade is controlled by temperature (\u003Cjats:italic>T\u003C\u002Fjats:italic>). Along the Tinos cross‐section (Greece), which is characterised by a strong gradient of greenschist facies overprint on eclogite facies rocks, the R2 ratio is nearly constant. Consequently, the degree of organisation of CM is not affected by the retrogression and records peak metamorphic conditions. More generally, analysis of 54 samples representative of high‐temperature, low‐pressure to high‐pressure, low‐temperature metamorphic gradients shows that there is a linear correlation between the R2 ratio and the peak temperature [\u003Cjats:italic>T\u003C\u002Fjats:italic>(°C) = −445 R2 + 641], whatever the metamorphic gradient and, probably, the organic precursor. The Raman spectrum of CM can therefore be used as a geothermometer of the maximum temperature conditions reached during regional metamorphism. Temperature can be estimated to ± 50 °C in the range 330–650 °C. A few technical indications are given for optimal application.\u003C\u002Fjats:p>",{"EN":5507},"Raman spectra of carbonaceous material in metasediments: a new geothermometer",{"VOID":5509},"10.1046\u002Fj.1525-1314.2002.00408.x",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1046\u002Fj.1525-1314.2002.00408.x",[5513,5532,5547,5562],{"id":5514,"sortIndex":32,"researcher":28,"roles":5515,"affiliations":5516,"properties":5525,"displayName":5529,"givenName":28,"familyName":28},"b7b2b34e-068c-430e-bab5-ef5d44f4ccfe",[],[5517],{"id":5518,"sortIndex":32,"affiliation":5519,"properties":28},"2ca09fad-d89f-476b-9035-976cf44c33dd",{"id":5518,"createTime":28,"updateTime":28,"relativeEntities":5520,"slug":28,"properties":5521,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":5524,"statistic":28},[],{"title":5522},{"EN":5523},"Laboratoire de Géologie, CNRS – UMR 8538, Ecole Normale Supérieure, 24 rue Lhomond, 75231 Paris Cedex 5, France ( Olivier.Beyssac@ens.fr )",[],{"orcid":5526,"title":5528,"openalex":5530},{"VOID":5527},"https:\u002F\u002Forcid.org\u002F0000-0001-8879-4762",{"EN":5529},"Olivier Beyssac",{"VOID":5531},"A5041029530",{"id":5533,"sortIndex":40,"researcher":28,"roles":5534,"affiliations":5535,"properties":5542,"displayName":5544,"givenName":28,"familyName":28},"07542e30-6363-4693-a786-75565457d04c",[],[5536],{"id":5518,"sortIndex":32,"affiliation":5537,"properties":28},{"id":5518,"createTime":28,"updateTime":28,"relativeEntities":5538,"slug":28,"properties":5539,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":5541,"statistic":28},[],{"title":5540},{"EN":5523},[],{"title":5543,"openalex":5545},{"EN":5544},"Bruno 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M. 1994.Metamorfismo de alta presion\u002Fbaja temperatura baja presion\u002Falta temperatura y tectonica del complejo Alpujarride (Cordilleras Betico‐Rifenas).PhD Thesis University of Granada . Granada .",{},{"id":28,"text":5650,"url":28,"identifiers":5651},"10.1016\u002F0024-4937(86)90015-0",{"doi":5650},{"id":28,"text":5653,"url":28,"identifiers":5654},"Bény‐Bassez C., 1985, Scanning Electron Microscopy,, 119",{},{"id":28,"text":5656,"url":28,"identifiers":5657},"Beyssac O., 2000, Pressure effects on graphitization: experimental constraints, Journal of Conference Abstracts, 5, 13",{},{"id":28,"text":5659,"url":28,"identifiers":5660},"10.1007\u002Fs00410-001-0324-7",{"doi":5659},{"id":28,"text":5662,"url":28,"identifiers":5663},"10.1016\u002F0166-5162(82)90018-0",{"doi":5662},{"id":28,"text":5665,"url":28,"identifiers":5666},"Borghi A., 1985, Metamorphism in the northern part of the Dora Maira massif (Cottian Alps), Bollettino Del Museo Regionale Di Scienze Naturali, Torino, 3, 369",{},{"id":28,"text":5668,"url":28,"identifiers":5669},"Borghi A., 1986, Composite P‐T paths in the. Internal Penninic Massifs of the Western Alps: Petrological constraints to their thermo‐mechanical evolution, Eclogae Geologicae Helvetiae, 89, 345",{},{"id":28,"text":5671,"url":28,"identifiers":5672},"Bouybaouene M., 1998, High‐Pressure granulites on top of the Beni Bousera peridotites, Morocco: a record of an ancient thickened crust in the Alboran domain, Bulletin de la Société Géologique de France, 169, 153",{},{"id":28,"text":5674,"url":28,"identifiers":5675},"10.1016\u002F0016-7037(85)90059-6",{"doi":5674},{"id":28,"text":5677,"url":28,"identifiers":5678},"10.1007\u002Fs004100050496",{"doi":5677},{"id":28,"text":5680,"url":28,"identifiers":5681},"10.1127\u002Fejm\u002F3\u002F2\u002F0263",{"doi":5680},{"id":28,"text":5683,"url":28,"identifiers":5684},"10.1016\u002FS0008-6223(97)00141-3",{"doi":5683},{"id":28,"text":5686,"url":28,"identifiers":5687},"10.1017\u002FCBO9780511573088.008",{"doi":5686},{"id":28,"text":5689,"url":28,"identifiers":5690},"10.1016\u002F0166-5162(87)90074-7",{"doi":5689},{"id":28,"text":5692,"url":28,"identifiers":5693},"10.1007\u002FBF00375447",{"doi":5692},{"id":28,"text":5695,"url":28,"identifiers":5696},"10.1016\u002FS0166-5162(00)00012-4",{"doi":5695},{"id":28,"text":5698,"url":28,"identifiers":5699},"10.1111\u002Fj.1525-1314.1992.tb00100.x",{"doi":5698},{"id":28,"text":5701,"url":28,"identifiers":5702},"10.1111\u002Fj.1525-1314.1983.tb00269.x",{"doi":5701},{"id":28,"text":5704,"url":28,"identifiers":5705},"10.1007\u002FBF00310699",{"doi":5704},{"id":28,"text":5707,"url":28,"identifiers":5708},"10.1016\u002F0008-6223(91)90064-P",{"doi":5707},{"id":28,"text":5710,"url":28,"identifiers":5711},"Faure M., 1985, Microtectonic evidence for eastward ductile shear in the Jurassic orogen of SW Japan, Journal of Metamorphic Geology, 7, 175",{},{"id":28,"text":5713,"url":28,"identifiers":5714},"Frey M., 1980, Alpine metamorphism along the GeoTraverse Basel‐Chiasso‐a review, Eclogae Geologicae Helvetiae, 73, 527",{},{"id":28,"text":5716,"url":28,"identifiers":5717},"10.1086\u002F627936",{"doi":5716},{"id":28,"text":5719,"url":28,"identifiers":5720},"10.1016\u002F0024-4937(81)90043-8",{"doi":5719},{"id":28,"text":5722,"url":28,"identifiers":5723},"10.1016\u002F0146-6380(92)90132-H",{"doi":5722},{"id":28,"text":5725,"url":28,"identifiers":5726},"10.1016\u002F0146-6380(90)90123-H",{"doi":5725},{"id":28,"text":5728,"url":28,"identifiers":5729},"10.1029\u002F2000TC900021",{"doi":5728},{"id":28,"text":5731,"url":28,"identifiers":5732},"10.1016\u002F0016-7037(94)90104-X",{"doi":5731},{"id":28,"text":5734,"url":28,"identifiers":5735},"10.1016\u002FS0008-6223(00)00120-2",{"doi":5734},{"id":28,"text":5737,"url":28,"identifiers":5738},"10.1111\u002Fj.1525-1314.1994.tb00038.x",{"doi":5737},{"id":28,"text":5740,"url":28,"identifiers":5741},"10.1007\u002FBF00373366",{"doi":5740},{"id":28,"text":5743,"url":28,"identifiers":5744},"10.1007\u002FBF00310693",{"doi":5743},{"id":28,"text":5746,"url":28,"identifiers":5747},"10.1016\u002F0008-6223(84)90009-5",{"doi":5746},{"id":28,"text":5749,"url":28,"identifiers":5750},"10.2475\u002Fajs.298.6.471",{"doi":5749},{"id":28,"text":5752,"url":28,"identifiers":5753},"10.1016\u002FS0016-7037(99)00409-3",{"doi":5752},{"id":28,"text":5755,"url":28,"identifiers":5756},"10.1103\u002FPhysRevB.20.392",{"doi":5755},{"id":28,"text":5758,"url":28,"identifiers":5759},"10.2138\u002Fam-2000-11-1206",{"doi":5758},{"id":28,"text":5761,"url":28,"identifiers":5762},"10.1111\u002Fj.1525-1314.1987.tb00375.x",{"doi":5761},{"id":28,"text":5764,"url":28,"identifiers":5765},"10.1016\u002FS0024-4937(02)00115-9",{"doi":5764},{"id":28,"text":5767,"url":28,"identifiers":5768},"10.1366\u002F0003702894202878",{"doi":5767},{"id":28,"text":5770,"url":28,"identifiers":5771},"Pasteris J. D., 1991, Raman spectra of graphite as indicators of degree of metamorphism, Canadian Mineralogist, 29, 1",{},{"id":28,"text":5773,"url":28,"identifiers":5774},"Patriat M., 1998, Post‐orogenic extension and shallow‐dipping shear zones, study of a brecciated decollement horizon in Tinos (Cyclades, Greece), Comptes Rendus de l'Académie Des Sciences, Paris, 326, 355",{},{"id":28,"text":5776,"url":28,"identifiers":5777},"10.1007\u002FBF00320978",{"doi":5776},{"id":28,"text":5779,"url":28,"identifiers":5780},"10.1038\u002F315733a0",{"doi":5779},{"id":28,"text":5782,"url":28,"identifiers":5783},"Saliot P., 1973, Les principales zones de métamorphisme dans les Alpes françaises. répartition et signification. Comptes rendus de l'Académie des Sciences, Paris, 276, 3081",{},{"id":28,"text":5785,"url":28,"identifiers":5786},"10.1111\u002Fj.1525-1314.1997.00038.x",{"doi":5785},{"id":28,"text":5788,"url":28,"identifiers":5789},"Trotet F. 2000.Exhumation des roches de Haute Pression – Basse Temperature le long d'un transect des Cyclades au Péloponnèse (Grèce): implications géodynamiques.PhD Thesis Université Paris 11 Paris.",{},{"id":28,"text":5791,"url":28,"identifiers":5792},"10.1016\u002F0038-1098(78)90382-4",{"doi":5791},{"id":28,"text":5794,"url":28,"identifiers":5795},"10.1063\u002F1.1674108",{"doi":5794},{"id":28,"text":4284,"url":28,"identifiers":5797},{"doi":4284},{"id":28,"text":5799,"url":28,"identifiers":5800},"10.1007\u002FBF00306643",{"doi":5799},{"id":28,"text":5802,"url":28,"identifiers":5803},"10.1016\u002F0008-6223(89)90125-5",{"doi":5802},{"id":28,"text":5805,"url":28,"identifiers":5806},"Wopenka B., 1993, Structural characterization of kerogens to granulite‐facies graphite: Applicability of Raman microprobe spectroscopy, American Mineralogist, 78, 533",{},{"id":28,"text":5808,"url":28,"identifiers":5809},"10.1046\u002Fj.1525-1314.1996.05792.x",{"doi":5808},{"id":28,"text":5811,"url":28,"identifiers":5812},"10.1111\u002Fj.1945-5100.1995.tb01115.x",{"doi":5811},{"id":5814,"createTime":5815,"updateTime":5815,"relativeEntities":5816,"slug":5817,"properties":5818,"entityType":964,"verifyStatus":26,"verifyTime":5829,"verifyNote":965,"languages":5830,"translateLanguages":28,"viewCount":32,"primaryUrl":5831,"fullTextUrl":28,"authors":5832,"publicationType":1005,"publisherRelationship":5888,"citationCount":5938,"citationInfo":5939,"publishDate":5943,"publishYear":5940,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":5944,"openAccess":28,"references":5945,"isForceReanalyzing":2076},"76e97fdf-830c-4862-94db-c74cf19f7aca","2024-09-27T14:23:53.375+00:00",[],"Progress-relating-to-calculation-of-partial-melting-equilibria-for-metapelites",{"openalex":5819,"mag":5821,"abstract":5823,"title":5825,"doi":5827},{"VOID":5820},"W2054493155",{"VOID":5822},"2054493155",{"EN":5824},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Improved activity–composition relationships for biotite, garnet and silicate liquid are used to construct updated \u003Cjats:italic>P\u003C\u002Fjats:italic>–\u003Cjats:italic>T\u003C\u002Fjats:italic> grids and pseudosections for high‐grade metapelites. The biotite model involves Ti charge‐balanced by hydrogen deprotonation on the hydroxyl site, following the substitution \u003Cjats:inline-graphic xmlns:xlink=\"http:\u002F\u002Fwww.w3.org\u002F1999\u002Fxlink\" xlink:href=\"graphic\u002FJMG_711_mu1.gif\" xlink:title=\"inline image\" \u002F>, where HD represents the hydroxyl site. Relative to equivalent biotite‐breakdown melting reactions in \u003Cjats:italic>P\u003C\u002Fjats:italic>–\u003Cjats:italic>T\u003C\u002Fjats:italic> grids in K\u003Cjats:sub>2\u003C\u002Fjats:sub>O–FeO–MgO–Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub>–SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–H\u003Cjats:sub>2\u003C\u002Fjats:sub>O (KFMASH), those in K\u003Cjats:sub>2\u003C\u002Fjats:sub>O–FeO–MgO–Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub>–SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–H\u003Cjats:sub>2\u003C\u002Fjats:sub>O–TiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–O\u003Cjats:sub>2\u003C\u002Fjats:sub> (KFMASHTO) occur at temperatures close to 50 °C higher. A further consequence of the updated activity models is that spinel‐bearing equilibria occur to higher temperature and higher pressure. In contrast, the addition of Na\u003Cjats:sub>2\u003C\u002Fjats:sub>O and CaO to KFMASH to make the Na\u003Cjats:sub>2\u003C\u002Fjats:sub>O–CaO–K\u003Cjats:sub>2\u003C\u002Fjats:sub>O–FeO–MgO–Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub>–SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–H\u003Cjats:sub>2\u003C\u002Fjats:sub>O (NCKFMASH) system lowers key biotite‐breakdown melting reactions in \u003Cjats:italic>P\u003C\u002Fjats:italic>–\u003Cjats:italic>T\u003C\u002Fjats:italic> space relative to KFMASH. Combination of the KFMASHTO and NCKFMASH systems to make Na\u003Cjats:sub>2\u003C\u002Fjats:sub>O–CaO–K\u003Cjats:sub>2\u003C\u002Fjats:sub>O–FeO–MgO–Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub>–SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–H\u003Cjats:sub>2\u003C\u002Fjats:sub>O–TiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–O\u003Cjats:sub>2\u003C\u002Fjats:sub> (NCKFMASHTO) results in key biotite‐breakdown melting reactions occurring at temperatures intermediate between those in KFMASHTO and those in NCKFMASH. Given such differences, the choice of model system will be critical to inferred \u003Cjats:italic>P\u003C\u002Fjats:italic>–\u003Cjats:italic>T\u003C\u002Fjats:italic> conditions in the application of mineral equilibria modelling to rocks. Further, pseudosections constructed in KFMASH, NCKFMASH and NCKFMASHTO for several representative rock compositions show substantial differences not only in the \u003Cjats:italic>P\u003C\u002Fjats:italic>–\u003Cjats:italic>T\u003C\u002Fjats:italic> conditions of key metamorphic assemblages but also overall topology, with the calculations in NCKFMASHTO more reliably reflecting equilibria in rocks. Application of mineral equilibria modelling to rocks should be undertaken in the most comprehensive system possible, if reliable quantitative \u003Cjats:italic>P\u003C\u002Fjats:italic>–\u003Cjats:italic>T\u003C\u002Fjats:italic> information is to be derived.\u003C\u002Fjats:p>",{"EN":5826},"Progress relating to calculation of partial melting equilibria for metapelites",{"VOID":5828},"10.1111\u002Fj.1525-1314.2007.00711.x","2024-09-27T14:23:53.374+00:00",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1525-1314.2007.00711.x",[5833,5860,5874],{"id":5834,"sortIndex":32,"researcher":28,"roles":5835,"affiliations":5836,"properties":5853,"displayName":5857,"givenName":28,"familyName":28},"4a5afc2c-5deb-4ede-8b6d-4bd38200a014",[],[5837,5845],{"id":5838,"sortIndex":32,"affiliation":5839,"properties":28},"545c52b5-c329-4582-9510-859b3e4dd1f6",{"id":5838,"createTime":28,"updateTime":28,"relativeEntities":5840,"slug":28,"properties":5841,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":5844,"statistic":28},[],{"title":5842},{"EN":5843},"Present address:Institute of Geoscience, University of Mainz, D-55099 Mainz, Germany.",[],{"id":5846,"sortIndex":40,"affiliation":5847,"properties":28},"b2897dca-ead6-4b52-8d59-fd78f06fbfdb",{"id":5846,"createTime":28,"updateTime":28,"relativeEntities":5848,"slug":28,"properties":5849,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":5852,"statistic":28},[],{"title":5850},{"EN":5851},"School of Earth Sciences, University of Melbourne, Melbourne, Vic. 3010, Australia ([email protected])",[],{"orcid":5854,"title":5856,"openalex":5858},{"VOID":5855},"https:\u002F\u002Forcid.org\u002F0000-0002-5270-3985",{"EN":5857},"R. 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L., 1990, Manganese, ferric iron, and the equilibrium between garnet and biotite, American Mineralogist, 75, 886",{},{"id":28,"text":6071,"url":28,"identifiers":6072},"10.1093\u002Fpetrology\u002F44.6.967",{"doi":6071},{"id":28,"text":6074,"url":28,"identifiers":6075},"10.1111\u002Fj.1525-1314.2004.00501.x",{"doi":6074},{"id":6077,"createTime":6078,"updateTime":6078,"relativeEntities":6079,"slug":6080,"properties":6081,"entityType":964,"verifyStatus":26,"verifyTime":6078,"verifyNote":965,"languages":6091,"translateLanguages":28,"viewCount":32,"primaryUrl":6092,"fullTextUrl":28,"authors":6093,"publicationType":1005,"publisherRelationship":6155,"citationCount":6203,"citationInfo":6204,"publishDate":6208,"publishYear":4561,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":6209,"openAccess":28,"references":6210,"isForceReanalyzing":2076},"2bee77c6-ccbe-4411-b535-6d1737bb2c92","2024-09-27T14:23:44.379+00:00",[],"The-effect-of-TiO-sub-2-sub-and-Fe-sub-2-sub-O-sub-3-sub-on-metapelitic-assemblages-at-greenschist-and-amphibolite-facies-conditions-mineral-equilibria-calculations-in-the-system-K-sub-2-sub-O-FeO-MgO-Al-sub-2-sub-O-sub-3-sub-SiO-sub-2-sub-H-sub-2-sub-O-TiO-sub-2-sub-Fe-sub-2-sub-O-sub-3-sub-",{"openalex":6082,"mag":6084,"abstract":6086,"title":6088,"doi":6090},{"VOID":6083},"W1998977948",{"VOID":6085},"1998977948",{"EN":6087},"\u003Cjats:p>Mineral equilibria calculations in the system K\u003Cjats:sub>2\u003C\u002Fjats:sub>O–FeO–MgO–Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub>–SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–H\u003Cjats:sub>2\u003C\u002Fjats:sub>O–TiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–Fe\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> (KFMASHTO) using thermocalc and its internally consistent thermodynamic dataset constrain the effect of TiO\u003Cjats:sub>2\u003C\u002Fjats:sub> and Fe\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> on greenschist and amphibolite facies mineral equilibria in metapelites. The end‐member data and activity–composition relationships for biotite and chloritoid, calibrated with natural rock data, and activity–composition data for garnet, calibrated using experimental data, provide new constraints on the effects of TiO\u003Cjats:sub>2\u003C\u002Fjats:sub> and Fe\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> on the stability of these minerals. Thermodynamic models for ilmenite–hematite and magnetite–ulvospinel solid solutions accounting for order–disorder in these phases allow the distribution of TiO\u003Cjats:sub>2\u003C\u002Fjats:sub> and Fe\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> between oxide minerals and silicate minerals to be calculated. The calculations indicate that small to moderate amounts of TiO\u003Cjats:sub>2\u003C\u002Fjats:sub> and Fe\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> in typical metapelitic bulk compositions have little effect on silicate mineral equilibria in metapelites at greenschist to amphibolite facies, compared with those calculated in KFMASH. The addition of large amounts of TiO\u003Cjats:sub>2\u003C\u002Fjats:sub> to typical pelitic bulk compositions has little effect on the stability of silicate assemblages; in contrast, rocks rich in Fe\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> develop a markedly different metamorphic succession from that of common Barrovian sequences. 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T., 1995, The effect of Mn on the phase relations of medium‐grade pelites: constraints from natural assemblages on petrogenetic grid topology., Journal of Petrology, 36, 1549",{},{"id":28,"text":6223,"url":28,"identifiers":6224},"10.1130\u002F0016-7606(1960)71[1:PMAGOT]2.0.CO;2",{"doi":6223},{"id":28,"text":6226,"url":28,"identifiers":6227},"EugsterH. P.1959Reduction and oxidation in metamorphism. In:Researches in Geochemistry(ed. Abelson P. H.) Vol. 1 pp. 397426Wiley New York",{},{"id":28,"text":1310,"url":28,"identifiers":6229},{"doi":1310},{"id":28,"text":6231,"url":28,"identifiers":6232},"10.1007\u002FBF01167285",{"doi":6231},{"id":28,"text":6234,"url":28,"identifiers":6235},"Guidotti C.V., 1991, Ferric iron in metamorphic biotite and its petrologic and crystallochemical implications., American Mineralogist, 76, 161",{},{"id":28,"text":6237,"url":28,"identifiers":6238},"Guidotti C. V., 1984, Micas in metamorphic rocks. In: Micas (ed. Bailey, S. W.)., Mineralogical Society of America Reviews in Mineralogy, 13, 357",{},{"id":28,"text":6240,"url":28,"identifiers":6241},"HarteB.&HudsonN. F. C.1979Pelite facies series and the temperature and pressures of Dalradian metamorphism in E. Scotland. In:The Caledonides io the British Isles—Reviewed(eds Harris A. L. Holland C. H. & Leake B. E.) pp. 323337Geological Society of London London",{},{"id":28,"text":1503,"url":28,"identifiers":6243},{"doi":1503},{"id":28,"text":1506,"url":28,"identifiers":6245},{"doi":1506},{"id":28,"text":963,"url":28,"identifiers":6247},{"doi":963},{"id":28,"text":6249,"url":28,"identifiers":6250},"Indares A., 1985, Biotite–garnet geothermometry in the granulite facies: the influence of Ti and Al in biotite., American Mineralogist, 70, 272",{},{"id":28,"text":6252,"url":28,"identifiers":6253},"Kleemann U., 1994, Garnet–biotite thermometry revisited: the effect of AlVI and Ti in biotite., American Mineralogist, 81, 1425",{},{"id":28,"text":6255,"url":28,"identifiers":6256},"KorzinskiiD. S.1959Physiochemical Basis of the Analysis of the Paragenesis of Minerals.Publ. Monograph Consultants Bureau New York",{},{"id":28,"text":1676,"url":28,"identifiers":6258},{"doi":1676},{"id":28,"text":6260,"url":28,"identifiers":6261},"O’Neill H. StC., 1984, Cation distributions and thermodynamic properties of binary spinel solid solutions., American Mineralogist, 69, 733",{},{"id":28,"text":6263,"url":28,"identifiers":6264},"O’Neill H. StC., 1992, The temperature dependence of the cation distribution in magnesioferrite from powder XRD structural refinements and Mossbauer spectroscopy., American Mineralogist, 77, 725",{},{"id":28,"text":6028,"url":28,"identifiers":6266},{"doi":6028},{"id":28,"text":1827,"url":28,"identifiers":6268},{"doi":1827},{"id":28,"text":6270,"url":28,"identifiers":6271},"Powell R., 1990, Calculated mineral equilibria in the pelite system K2O–FeO–MgO–Al2O3– SiO2–H2., American Mineralogist, 78, 107",{},{"id":28,"text":1830,"url":28,"identifiers":6273},{},{"id":28,"text":6036,"url":28,"identifiers":6275},{"doi":6036},{"id":28,"text":1836,"url":28,"identifiers":6277},{"doi":1836},{"id":28,"text":6279,"url":28,"identifiers":6280},"10.1007\u002FBF00371584",{"doi":6279},{"id":28,"text":6282,"url":28,"identifiers":6283},"Rumble D., 1976, Oxide minerals in metamorphic rocks., Mineralogical Society of America Reviews in Mineralogy, 3, R1",{},{"id":28,"text":6285,"url":28,"identifiers":6286},"10.1007\u002FBF00321989",{"doi":6285},{"id":28,"text":6288,"url":28,"identifiers":6289},"10.1007\u002FBF00375302",{"doi":6288},{"id":28,"text":6291,"url":28,"identifiers":6292},"10.1111\u002Fj.1525-1314.1992.tb00080.x",{"doi":6291},{"id":28,"text":6294,"url":28,"identifiers":6295},"Thompson J. B., 1957, The graphical analysis of mineral assemblages in pelitic schists., American Mineralogist, 42, 842",{},{"id":28,"text":6297,"url":28,"identifiers":6298},"Thompson J. B., 1972, Oxides and sulfides in regional metamorphism of pelitic schists., International Geological Congress, Montreal, 10, 27",{},{"id":28,"text":6300,"url":28,"identifiers":6301},"10.1007\u002FBF00306435",{"doi":6300},{"id":28,"text":6303,"url":28,"identifiers":6304},"Williams M. L., 1990, Manganese, ferric iron, and the equilibrium between garnet and biotite., American Mineralogist, 75, 886",{},{"id":28,"text":6306,"url":28,"identifiers":6307},"Woodland A. B., 1993, Synthesis and stability of Fe2+3Fe3+2Si3O12 garnet and phase relations with Fe3Al2Si3O12−Fe2+3Fe3+2Si3O12 solutions., American Mineralogist, 78, 1000",{},{"id":28,"text":6309,"url":28,"identifiers":6310},"10.2475\u002Fajs.261.10.929",{"doi":6309},{"id":6312,"createTime":6313,"updateTime":6313,"relativeEntities":6314,"slug":6315,"properties":6316,"entityType":964,"verifyStatus":26,"verifyTime":6327,"verifyNote":965,"languages":6328,"translateLanguages":28,"viewCount":32,"primaryUrl":6329,"fullTextUrl":28,"authors":6330,"publicationType":1005,"publisherRelationship":6409,"citationCount":6458,"citationInfo":6459,"publishDate":6466,"publishYear":6460,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":6467,"openAccess":28,"references":6468,"isForceReanalyzing":2076},"d9ec828d-1dc2-433c-aeb7-ea50564f9f61","2024-09-27T14:23:53.145+00:00",[],"New-mineral-activity-composition-relations-for-thermodynamic-calculations-in-metapelitic-systems",{"openalex":6317,"mag":6319,"abstract":6321,"title":6323,"doi":6325},{"VOID":6318},"W1997842666",{"VOID":6320},"1997842666",{"EN":6322},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>New activity–composition (\u003Cjats:italic>a\u003C\u002Fjats:italic>–\u003Cjats:italic>x\u003C\u002Fjats:italic>) relations for minerals commonly occurring in metapelites are presented for use with the internally consistent thermodynamic dataset of Holland & Powell (\u003Cjats:ext-link xmlns:xlink=\"http:\u002F\u002Fwww.w3.org\u002F1999\u002Fxlink\" xlink:href=\"#jmg12071-bib-0024\" \u002F>, \u003Cjats:italic>Journal of Metamorphic Geology\u003C\u002Fjats:italic>,\u003Cjats:bold> 29\u003C\u002Fjats:bold>, 333–383). The \u003Cjats:italic>a\u003C\u002Fjats:italic>–\u003Cjats:italic>x\u003C\u002Fjats:italic> relations include a broader consideration of Fe\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub> in minerals, changes to the formalism of several phases and order–disorder in all ferromagnesian minerals where Fe–Mg mixing occurs on multiple sites. The \u003Cjats:italic>a\u003C\u002Fjats:italic>–\u003Cjats:italic>x\u003C\u002Fjats:italic> relations for chlorite, biotite, garnet, chloritoid, staurolite, cordierite, orthopyroxene, muscovite, paragonite and margarite have been substantially reparameterized using the approach outlined in the companion paper in this issue. For the first time, the entire set of \u003Cjats:italic>a\u003C\u002Fjats:italic>–\u003Cjats:italic>x\u003C\u002Fjats:italic> relations for the common ferromagnesian minerals in metapelitic rocks is parameterized simultaneously, with attention paid to ensuring that they can be used together to calculate phase diagrams of geologically appropriate topology. The \u003Cjats:italic>a\u003C\u002Fjats:italic>–\u003Cjats:italic>x\u003C\u002Fjats:italic> relations developed are for use in the Na\u003Cjats:sub>2\u003C\u002Fjats:sub>O–CaO–K\u003Cjats:sub>2\u003C\u002Fjats:sub>O–FeO–MgO–Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub>–SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–H\u003Cjats:sub>2\u003C\u002Fjats:sub>O–TiO\u003Cjats:sub>2\u003C\u002Fjats:sub>–O\u003Cjats:sub>2\u003C\u002Fjats:sub> (NCKFMASHTO) system for both subsolidus and suprasolidus conditions. Petrogenetic grids in KFMASH and KFMASHTO are similar in topology to those produced with earlier end‐member datasets and \u003Cjats:italic>a\u003C\u002Fjats:italic>–\u003Cjats:italic>x\u003C\u002Fjats:italic> relations, but with some notable differences. In particular, in subsolidus equilibria, the FeO\u002F(FeO + MgO) of garnet is now greater than in coexisting staurolite, bringing a number of key staurolite‐bearing equilibria into better agreement with inferences from field and petrographic observations. Furthermore, the addition of Fe\u003Cjats:sup>3+\u003C\u002Fjats:sup> and Ti to a number of silicate phases allows more plausible equilibria to be calculated in relevant systems. Pseudosections calculated with the new \u003Cjats:italic>a\u003C\u002Fjats:italic>–\u003Cjats:italic>x\u003C\u002Fjats:italic> relations are also topologically similar to equivalent diagrams using earlier \u003Cjats:italic>a\u003C\u002Fjats:italic>–\u003Cjats:italic>x\u003C\u002Fjats:italic> relations, although with many low variance fields shifting in \u003Cjats:italic>P\u003C\u002Fjats:italic>–\u003Cjats:italic>T\u003C\u002Fjats:italic> space to somewhat lower pressure conditions.\u003C\u002Fjats:p>",{"EN":6324},"New mineral activity–composition relations for thermodynamic calculations in metapelitic systems",{"VOID":6326},"10.1111\u002Fjmg.12071","2024-09-27T14:23:53.144+00:00",[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fjmg.12071",[6331,6347,6363,6377,6394],{"id":6332,"sortIndex":32,"researcher":28,"roles":6333,"affiliations":6334,"properties":6343,"displayName":5857,"givenName":28,"familyName":28},"a0d605c2-ee31-4a75-9502-99fc19cc2cfd",[],[6335],{"id":6336,"sortIndex":32,"affiliation":6337,"properties":28},"86d17e49-17a5-4fe6-8850-23ae44239613",{"id":6336,"createTime":28,"updateTime":28,"relativeEntities":6338,"slug":28,"properties":6339,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6342,"statistic":28},[],{"title":6340},{"EN":6341},"Institute of Geoscience University of Mainz D‐55099 Mainz Germany",[],{"orcid":6344,"title":6345,"openalex":6346},{"VOID":5855},{"EN":5857},{"VOID":5859},{"id":6348,"sortIndex":40,"researcher":28,"roles":6349,"affiliations":6350,"properties":6359,"displayName":1002,"givenName":28,"familyName":28},"d6d6020d-e297-48d5-a762-6e32c003dc12",[],[6351],{"id":6352,"sortIndex":32,"affiliation":6353,"properties":28},"cf94a309-c4bb-470e-9088-066c59ff90fd",{"id":6352,"createTime":28,"updateTime":28,"relativeEntities":6354,"slug":28,"properties":6355,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6358,"statistic":28},[],{"title":6356},{"VI":6357},"School of Earth Sciences, University of Melbourne, Melbourne, Vic. 3010, Australia",[],{"orcid":6360,"title":6361,"openalex":6362},{"VOID":1000},{"EN":1002},{"VOID":1004},{"id":6364,"sortIndex":123,"researcher":28,"roles":6365,"affiliations":6366,"properties":6373,"displayName":985,"givenName":28,"familyName":28},"17f3a2be-b807-4f57-a557-262af3ca0a92",[],[6367],{"id":2099,"sortIndex":32,"affiliation":6368,"properties":28},{"id":2099,"createTime":28,"updateTime":28,"relativeEntities":6369,"slug":28,"properties":6370,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6372,"statistic":28},[],{"title":6371},{"VI":2104},[],{"orcid":6374,"title":6375,"openalex":6376},{"VOID":983},{"EN":985},{"VOID":987},{"id":6378,"sortIndex":42,"researcher":28,"roles":6379,"affiliations":6380,"properties":6387,"displayName":6391,"givenName":28,"familyName":28},"1ef8d5f3-3623-424a-b2e3-c63e4c1a79ef",[],[6381],{"id":6336,"sortIndex":32,"affiliation":6382,"properties":28},{"id":6336,"createTime":28,"updateTime":28,"relativeEntities":6383,"slug":28,"properties":6384,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6386,"statistic":28},[],{"title":6385},{"EN":6341},[],{"orcid":6388,"title":6390,"openalex":6392},{"VOID":6389},"https:\u002F\u002Forcid.org\u002F0000-0001-8704-4396",{"EN":6391},"Tim Johnson",{"VOID":6393},"A5030105240",{"id":6395,"sortIndex":45,"researcher":28,"roles":6396,"affiliations":6397,"properties":6404,"displayName":6406,"givenName":28,"familyName":28},"aaf6bcf2-c213-4f49-82d2-d8c2d3d4ab97",[],[6398],{"id":6336,"sortIndex":32,"affiliation":6399,"properties":28},{"id":6336,"createTime":28,"updateTime":28,"relativeEntities":6400,"slug":28,"properties":6401,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6403,"statistic":28},[],{"title":6402},{"EN":6341},[],{"title":6405,"openalex":6407},{"EN":6406},"E. 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diagrams involving solid solutions are calculated by solving sets of non‐linear equations. In calculating \u003Cjats:italic>P–T \u003C\u002Fjats:italic> projections and compatibility diagrams, the equations used for each equilibrium are the equilibrium relationships for an independent set of reactions between the end‐members of the phases in the equilibrium. Invariant points and univariant lines in \u003Cjats:italic>P–T \u003C\u002Fjats:italic> projections can be calculated directly, as can coordinates in compatibility diagrams. In calculating \u003Cjats:italic>P–T \u003C\u002Fjats:italic> and \u003Cjats:italic>T–x\u003C\u002Fjats:italic>\u002F\u003Cjats:italic>P–x\u003C\u002Fjats:italic> pseudosections – diagrams drawn for particular bulk compositions – the equilibrium relationship equations are augmented by mass balance equations. Lines in pseudosections, where the mode of one phase in the lower variance equilibrium is zero, and points, where the modes of two phases are zero, can then be calculated directly. The software, THERMOCALC, allows the calculation of these and a range of other types of phase diagram. Examples of phase diagrams and phase diagram movies, with instructions for their production, along with the THERMOCALC input and output files, and the Mathematica\u003Cjats:sup>TM\u003C\u002Fjats:sup> functions for assembling them, are presented in this paper, partly in hard copy and partly on the JMG web sites (http:\u002F\u002Fwww.gly.bris.ac.uk\u002Fwww\u002Fjmg\u002Fjmg.html, or equivalent Australian or USA sites).\u003C\u002Fjats:p>",{"EN":6596},"Calculating phase diagrams involving solid solutions via non‐linear equations, with examples using THERMOCALC",{"VOID":1836},[31],"https:\u002F\u002Fonlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1525-1314.1998.00157.x",[6601,6617,6631],{"id":6602,"sortIndex":32,"researcher":28,"roles":6603,"affiliations":6604,"properties":6613,"displayName":1002,"givenName":28,"familyName":28},"dbcfa724-f4e2-47be-a6d7-ab953a887430",[],[6605],{"id":6606,"sortIndex":32,"affiliation":6607,"properties":28},"0eed017b-c8ec-4b79-90fa-e366479c5bb0",{"id":6606,"createTime":28,"updateTime":28,"relativeEntities":6608,"slug":28,"properties":6609,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6612,"statistic":28},[],{"title":6610},{"EN":6611},"School of Earth Sciences, The University of Melbourne, Victoria 3052, Australia,",[],{"orcid":6614,"title":6615,"openalex":6616},{"VOID":1000},{"EN":1002},{"VOID":1004},{"id":6618,"sortIndex":40,"researcher":28,"roles":6619,"affiliations":6620,"properties":6627,"displayName":985,"givenName":28,"familyName":28},"5f067f01-2fcb-40c9-8d28-25c000e8fe86",[],[6621],{"id":2099,"sortIndex":32,"affiliation":6622,"properties":28},{"id":2099,"createTime":28,"updateTime":28,"relativeEntities":6623,"slug":28,"properties":6624,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6626,"statistic":28},[],{"title":6625},{"VI":2104},[],{"orcid":6628,"title":6629,"openalex":6630},{"VOID":983},{"EN":985},{"VOID":987},{"id":6632,"sortIndex":123,"researcher":28,"roles":6633,"affiliations":6634,"properties":6641,"displayName":6643,"givenName":28,"familyName":28},"874cc0a7-2e8a-4c3e-b80c-e2041db09d03",[],[6635],{"id":6606,"sortIndex":32,"affiliation":6636,"properties":28},{"id":6606,"createTime":28,"updateTime":28,"relativeEntities":6637,"slug":28,"properties":6638,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6640,"statistic":28},[],{"title":6639},{"EN":6611},[],{"title":6642,"openalex":6644},{"EN":6643},"B. 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