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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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For this purpose, the Permian sandstone reservoirs in the Upper Shihezi Formation, Gubei low buried hill, Jiyang Depression, was taken as the object. Referring to the evolution histories of reservoirs and tectonics, the diagenesis of the reservoirs and its coupling with tectonic activity were investigated, with the aid of techniques like core observation, casting sheet observation, scanning electron microscopy (SEM), cathode luminescence, electron probe, back scattering, fluid inclusion, and pore permeability tests. The results show that the Permian sandstone reservoirs in the Upper Shihezi Formation, Gubei low buried hill, Jiyang Depression, are low-porosity, low-permeability reservoirs with complex diagenesis. The diagenetic evolution sequence can be summarized as early feldspar corrosion\u002Fkaolinite cemention\u002Fearly pyrite cemention→carbonate cemention\u002Fsecondary enlargement of quartz→quartz corrosion\u002Fcorrosion of quartz and its secondary enlargement→late calcite cemention→late pyrite cemention\u002Fcarbonate corrosion\u002Flate feldspar corrosion\u002Fcorrosion of dissolvable miscellaneous matrix; compaction effect exists throughout the evolution process. The reservoirs went through (I) shallow burial epidiagenesis, (II) near-surface hydrothermal diagenesis, (III) deep burial alkaline diagenesis, and (IV) continuous burial acid diagenesis. The diagenetic evolution of these four stages is significantly affected by tectonic activities, and the article lists the evidence that diagenesis is affected by tectonic activity. The research results lay the basis for the prediction and evaluation of the Permian sandstone reservoirs in the Upper Shihezi Formation, Gubei low buried hill, Jiyang Depression, and shed new light on the exploration of tight sandstone reservoirs.",{"EN":924},"Coupling between tectonic activity and diagenetic evolution of a clastic buried hill—a case study from Gubei low buried hill in Jiyang Depression of Bohai Bay Basin",{"VOID":926},"Al Owais AA, El-Hallag IS (2020) Investigation of the nucleation process of electrodeposited nanostructured cobalt films using Brij 76 lyotropic liquid crystal. J New Mater Electrochem Syst 23(2):133–138. https:\u002F\u002Fdoi.org\u002F10.14447\u002Fjnmes.v23i2.a10\nAmel H, Jafarian A, Husinec A, Koeshidayatullah A, Swennen R (2015) Microfacies, depositional environment and diagenetic evolution controls on the reservoir quality of the Permian Upper Dalan Formation, Kish Gas Field, Zagros Basin. Mar Pet Geol 67:57–71. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.marpetgeo.2015.04.012\nBjørlykke K, Jahren J (2012) Open or closed geochemical systems during diagenesis in sedimentary basins: constraints on mass transfer during diagenesis and the prediction of porosity in sandstone and carbonate reservoirs. AAPG Bull 96:2193e2214\nBjørlykke K (2014) Relationships between depositional environments, burial history and rock properties. Some principal aspects of iagenetic process in sedimentary basins. Sediment Geol 301, 1e14\nBi G, Lyu C, Li C, Chen G, Zhang G, Zhou Q, Li C, Zhao Y (2019) Impact of early hydrocarbon charge on the diagenetic history and reservoir quality of the Central Canyon sandstones in the Qiongdongnan Basin, South China Sea. J Asian Earth Sci 185:104022. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.jseaes.2019.104022\nDeng Y (2017) Formation and characteristics of large-medium buried-hill hydrocarbon reservoirs in Bohai Sea. Petroleum Research 2(2):97–106. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.ptlrs.2017.07.001\nHadi MS, Saud SN, Hamzah E, Mamat MF (2019) Hydrogen embrittlement of 316L stainless steels exposed in 1.0M hydrochloric acid solution. Ann Chim Sci Mater 43(6):369–375. https:\u002F\u002Fdoi.org\u002F10.18280\u002Facsm.430602\nHan C, Tian J, Hu C, Liu H, Wang W, Huan Z, Feng S (2020) Lithofacies characteristics and their controlling effects on reservoirs in buried hills of metamorphic rocks: a case study of late Paleozoic units in the Aryskum depression, South Turgay Basin, Kazakhstan. J Pet Sci Eng 191:107137. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.petrol.2020.107137\nHou M, Cao H, Li H, Chen A, Wei A, Chen Y, Wang Y, Zhou X, Ye T (2019) Characteristics and controlling factors of deep buried-hill reservoirs in the BZ19-6 structural belt, Bohai sea area. Natural Gas Industry B 6(4):305–316. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.ngib.2019.01.011\nHu H, Jiang Y, Gluyas J, Zhao K, Fang J, Wang Y, Lu Y (2019) Mass transfer between sandstones and interbedded mudstones: impact on petroleum charge, Bohai Bay Basin, China. Mar Pet Geol 107:81–98. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.marpetgeo.2019.05.007\nJin F, Wang X, Li H, Wu X, Fu L, Lou D, Zhang J, Feng J (2019) Formation of the primary petroleum reservoir in Wumaying inner buried-hill of Huanghua Depression, Bohai Bay Basin, China. Pet Explor Dev 46(3):543–552. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS1876-3804(19)60034-0\nMeng WG, Chen ZY, Li P, Guo YM, Gao XZ, Hui XF (2009) Exploration theories and practices of buried-hill reservoirs: a case from Liaohe Depression. Pet Explor Dev 36(2):136–143. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS1876-3804(09)60116-6\nMerizgui T, Hadjadj A, Kious M, Gaoui B (2019) Enhanced of electrical properties and shielding efficiency of hybrid composite with temperature. Revue des Composites et des Matériaux Avancés 29(6):171–177. https:\u002F\u002Fdoi.org\u002F10.18280\u002Frcma.290604\nMorad S, Al-Ramadan K, Ketzer JM, De Ros L (2010) The impact of diagenesis on the heterogeneity of sandstone reservoirs: a review of the role of depositional facies and sequence stratigraphy. AAPG Bull 94:1267e1309\nQian W, Yin T, Zhang C, Hou G, He M (2020) Diagenesis and diagenetic stages prediction of Ed2 reservoir in the west of Bozhong sag. Petroleum 6(1):23–30. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.petlm.2019.04.003\nRathanasalam V, Perumalsami J, Jayakumar K (2019) Effect of ultrafine ground granulated blast-furnace slag (UFGGBFS) and copper slag on ambient cured geopolymer concrete. Ann Chim Sci Mater 43(6):377–382. https:\u002F\u002Fdoi.org\u002F10.18280\u002Facsm.430603\nRaza M, Khan F, Khan MY, Riaz MT, Khan U (2020) Reservoir characterization of the B-interval of lower goru formation, miano 9 and 10, miano area, Lower Indus Basin, Pakistan. Environ Earth Sci Res J 7(1):18–32. https:\u002F\u002Fdoi.org\u002F10.18280\u002Feesrj.070103\nTaylor TR, Giles MR, Hathon LA, Diggs TN, Braunsdorf NR, Birbiglia GV (2010) Sandstone diagenesis and reservoir quality prediction: models, myths,and reality. AAPG Bull 94:1093e1132\nTeillet T, Fournier F, Gisquet F, Montaggioni LF, Borgomano J, Villeneuve Q, Hong F (2019) Diagenetic history and porosity evolution of an Early Miocene carbonate buildup (Upper Burman Limestone), Yadana gas field, offshore Myanmar. Mar Pet Geol 109:589–606. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.marpetgeo.2019.06.044\nTong K, Zhao C, Lü Z, Zhang Y, Zheng H, Xu S, Wang J, Pan L (2012) Reservoir evaluation and fracture characterization of the metamorphic buried hill reservoir in Bohai Bay Basin. Pet Explor Dev 39(1):62–69. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS1876-3804(12)60015-9\nVan Dilla MA, Dean PN, Fuscoe JC, Gray JW, Lucas JN, Peters DC, Trask BJ, van den Engh GJ (1989) Flow cytometric analysis and sorting of chromosomes. New Trends in Genetic Risk Assessment:225–245. https:\u002F\u002Fdoi.org\u002F10.1016\u002FB978-0-12-388176-2.50024-2\nWang E, Liu G, Pang X, Li C, Wu Z (2020a) Diagenetic evolution and formation mechanisms of middle to deep clastic reservoirs in the Nanpu sag, Bohai Bay Basin, East China. Pet Explor Dev 47(2):343–356. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS1876-3804(20)60051-9\nWang J, Zhao L, Zhang X, Yang Z, Cao H, Chen L, Shan F, Liu M (2015) Buried hill karst reservoirs and their controls on productivity. Pet Explor Dev 42(6):852–860. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS1876-3804(15)30082-3\nWang S, Wang G, Lai J, Li D, Liu S, Chen X, Yang K, Song L (2020) Logging identification and evaluation of vertical zonation of buried hill in Cambrian dolomite reservoir: a study of Yingmai-Yaha buried hill structural belt, northern Tarim Basin. J Pet Sci Eng 195:107758. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.petrol.2020.107758\nWang ZJ, Li J, Ye PE, Wang CL, Cui XW (2019) Microstructure and hydration mechanism of autoclaved aerated concrete from fly ash. J New Mater Electrochem Syst 22(2):85–90. https:\u002F\u002Fdoi.org\u002F10.14447\u002Fjnmes.v22i2.a04\nWolela A (2012) Diagenetic evolution and reservoir potential of the Barremian–Cenomanian Debre Libanose Sandstone, Blue Nile (Abay) Basin, Ethiopia. Cretac Res 36:83–95. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.cretres.2012.02.007\nWorden RH, Burley SD (2003) Sandstone diagenesis: the evolution of sand to stone. In: Burley, S.D., Worden, R.H. (Eds.), Sandstone Diagenesis: Recent and Ancient, vol. 4. IAS Special Publication, pp. e44\nXie Y, Luo X, Wang D, Xu C, Xu Y, Hou M, Chen A (2019) Hydrocarbon accumulation of composite-buried hill reservoirs in the western subsag of Bozhong sag, Bohai Bay Basin. Natural Gas Industry B 6(6):546–555. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.ngib.2019.05.002\nXiong Y, Tan X, Dong G, Wang L, Ji H, Liu Y, Wen C (2020) Diagenetic differentiation in the Ordovician Majiagou Formation, Ordos Basin, China: facies, geochemical and reservoir heterogeneity constraints. J Pet Sci Eng 191:107179. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.petrol.2020.107179\nYan SQ, Wang QK, Wang HF, Qiu SL, Zeng ZQ, Fang Y (2020) Strength control factors of chlorite schist under schistose structure. Int J Des Nat Ecodyn 15(5):631–637. https:\u002F\u002Fdoi.org\u002F10.18280\u002Fijdne.150503\nYang T, Cao Y, Friis H, Wang Y, Zhou L (2018) Diagenetic evolution and chemical changes of deep-water mudstones of Shahejie Formation in the Dongying Sag, Jiyang Depression, Eastern China. Mar Pet Geol 93:14–32. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.marpetgeo.2018.02.005\nYu K, Qiu L, Cao Y, Sun P, Qu C, Yang Y (2019) Hydrothermal origin of early Permian saddle dolomites in the Junggar Basin, NW China. J Asian Earth Sci 184:103990. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.jseaes.2019.103990",{"VOID":928},"10.1007\u002Fs12517-021-06566-w","PUBLICATION","https:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs12517-021-06566-w",[932,948,970,990,1005,1018],{"id":933,"sortIndex":32,"researcher":28,"roles":934,"affiliations":936,"properties":945,"displayName":947,"givenName":28,"familyName":28},"cd8fe9f0-2069-42ea-8f3b-7a6404616057",[935],"AUTHOR",[937],{"id":938,"sortIndex":32,"affiliation":939,"properties":28},"c99a1c33-a942-4a46-9897-3a5dfb66f256",{"id":938,"createTime":28,"updateTime":28,"relativeEntities":940,"slug":28,"properties":941,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":944,"statistic":28},[],{"title":942},{"VI":943},"School of Geosciences, China University of Petroleum, Qingdao, China",[],{"title":946},{"VI":947},"Yelei 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Qiao","ARTICLE",{"url":930,"publisher":1033,"properties":1053},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1034,"slug":872,"properties":1035,"entityType":25,"verifyStatus":882,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1039,"manageAffiliations":1040,"indexDatabases":1041,"url":28,"thumbnailPath":28,"statistic":1048,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1036,"title":1037,"eissn":1038},{"VOID":877},{"EN":879},{"VOID":875},[],[],[1042],{"id":887,"indexDatabase":1043,"url":893,"indexYears":894,"academicFieldIds":28,"indexDatabaseRanking":788},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1044,"label":1045,"description":1046,"key":781,"publicationTags":1047,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],{"impactFactor":32,"impactFactorByYear":1049,"i10Index":123,"i10IndexLast5Year":40,"totalPublication":897,"totalPublicationByYear":1050,"totalCitation":567,"totalCitationByYear":1051,"totalCitationPerPublication":513,"totalCitationPerPublicationByYear":1052,"hindexLast5Year":45,"hindex":45},{"2019":513,"2020":513,"2021":32,"2022":32,"2023":32},{"2008":205,"2009":149,"2010":161,"2011":331,"2012":899,"2013":900,"2014":901,"2015":902,"2016":903,"2017":904,"2018":617,"2019":905,"2020":906,"2021":907,"2022":908,"2023":909,"2024":567},{"2018":278,"2019":40,"2020":127,"2021":145},{"2018":105,"2019":32,"2020":107,"2021":513},{"pages":1054,"volume":1056},{"VOID":1055},"1-12",{"VOID":1057},"14","2021-01-28",2021,[783],false,{"id":1063,"createTime":1064,"updateTime":1065,"relativeEntities":1066,"slug":1067,"properties":1068,"entityType":929,"verifyStatus":26,"verifyTime":1065,"verifyNote":1077,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1078,"fullTextUrl":28,"authors":1079,"publicationType":1031,"publisherRelationship":1197,"citationCount":28,"citationInfo":28,"publishDate":1223,"publishYear":1224,"citationAnalyzeStatus":882,"lastCitationAnalyze":28,"indexDatabases":1225,"openAccess":28,"references":28,"isForceReanalyzing":1061},"0009643b-bcb0-4bbd-8876-9f81a6a0e511","2024-02-10T22:03:43.377+00:00","2024-12-14T08:21:38.734+00:00",[],"Petrogenesis-and-evolution-of-the-Nuweibi-rare-metal-granite-Central-Eastern-Desert-Egypt",{"abstract":1069,"title":1071,"references":1073,"doi":1075},{"EN":1070},"The Nuweibi rare-metal granite in the Central Eastern Desert of Egypt is highly evolved fine- to medium-grained leucogranite affected by pervasive albitization and greisenization. The intrusion holds an important tin–tantalum resource in the Egyptian Eastern Desert. Columbite–tantalite and cassiterite disseminations occur within the granite body, while the quartz ± feldspar veins cutting across the Nuweibi granite host only cassiterite disseminations. Microscopically, quartz and alkali-feldspar are the essential mineral constituents of Nuweibi granite, with minor mica (muscovite + rare biotite), while cassiterite, columbite–tantalite, zircon, allanite, beryl, tourmaline, titanite, and fluorite are accessories. Whole-rock geochemistry and micoanalytical data together with laser ablation inductively coupled plasma mass spectrometer (LA-ICP-MS) dating of zircon and columbite have been used to constrain the evolution of the granite intrusion and associated mineralization. The Nuweibi granite is weakly peraluminous with extremely low MgO, CaO, TiO2, P2O5, Ba, and Sr contents and elevated Sn, Ta, Nb, and Rb contents. The REE patterns exhibit distinct tetrad effects, as well as negative Eu and Y anomalies. Also, the bulk rock Zr\u002FHf ratios are consistently \u003C 10. The Nd isotopic system is disturbed and εNd values suggest a juvenile mantle and\u002For Neoproterozoic crustal source. The U–Pb system in zircon is disturbed and leaked continuously, while the U–Pb age of columbite is ~ 620 Ma. The geochemical and isotopic systematics of the Nuweibi intrusion reflect very advanced degree of fractionation combined with late magmatic fluid overprint which redistributed Sn and other mobile elements, while Ta still characterizes the igneous system.",{"EN":1072},"Petrogenesis and evolution of the Nuweibi rare-metal granite, Central Eastern Desert, Egypt",{"VOID":1074},"Abdeen M, Greiling R, Sadek M, Hamad S (2014) Magnetic fabrics and Pan African structural evolution in the Najd Fault corridor in the Eastern Desert of Egypt. J Afr Earth Sci 99:93–108\nAbdel-Rahman AM (2006) Petrogenesis of anorogenic peralkaline granitic complexes from Eastern Egypt. Mineral Mag 70:27–50\nAbdel-Rahman AM, Doig R (1987) The Rb–Sr geochronological evolution of the Ras Gharib segment of the northern Nubian Shield. Geol Soc Lond 144:577–586\nAbu El-Leil I, Mussa MA (1984) Structural factors controlling rare metal occurrences at Igla-Barramiya area, Eastern desert, Egypt. Ann Geol Surv Egypt 14:309–318\nAgangi A, Kamenetsky VS, McPhie J (2010) The role of fluorine in the concentration and transport of lithophile trace elements in felsic magmas: insights from the Gawler Range Volcanics, South Australia. Chem Geol 273:314–325\nAli Kh (2003) Geology and radioactivity of Naba-Nuweibi area, Central Eastern Desert, Egypt. Unpub. Ph.D. thesis, Ain Shams University, Cairo, Egypt, 194 p\nAli KA, Stern RG, Manton W, Kimura J, Khamees HA (2009) Geochemistry, Nd isotopes and U–Pb SHRIMP zircon dating of Neoproterozoic volcanic rocks from the Central Eastern Desert of Egypt: new insights into the ~750 Ma crust-forming event. Precambrian Res 171:1–22\nAli KA, Moghazi A, Maurice AE, Omar SA, Wang Q, Wilde SA, Moussa EM, Manton WI, Stern RG (2012) Composition, age, and origin of the ~620 Ma Humr Akarim and Humrat Mukbid A-type granites: no evidence for pre-Neoproterozoic basement in the Eastern Desert, Egypt. Int J Earth Sci (Geol Rundsch) 101:1705–1722\nAl-Saleh AM, Boyle AP, Musset AE (1998) Metamorphism and 40Ar\u002F39Ar dating of the Halaban Ophiolite and associated units: evidence for two-stage orogenesis in the Arabian Shield. J Geol Soc Lond 155:165–175\nAnders E, Grevesse N (1989) Abundances of the elements: meteoritic and solar. 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Nolte",{"url":1078,"publisher":1198,"properties":1218},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1199,"slug":872,"properties":1200,"entityType":25,"verifyStatus":882,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1204,"manageAffiliations":1205,"indexDatabases":1206,"url":28,"thumbnailPath":28,"statistic":1213,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1201,"title":1202,"eissn":1203},{"VOID":877},{"EN":879},{"VOID":875},[],[],[1207],{"id":887,"indexDatabase":1208,"url":893,"indexYears":894,"academicFieldIds":28,"indexDatabaseRanking":788},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1209,"label":1210,"description":1211,"key":781,"publicationTags":1212,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],{"impactFactor":32,"impactFactorByYear":1214,"i10Index":123,"i10IndexLast5Year":40,"totalPublication":897,"totalPublicationByYear":1215,"totalCitation":567,"totalCitationByYear":1216,"totalCitationPerPublication":513,"totalCitationPerPublicationByYear":1217,"hindexLast5Year":45,"hindex":45},{"2019":513,"2020":513,"2021":32,"2022":32,"2023":32},{"2008":205,"2009":149,"2010":161,"2011":331,"2012":899,"2013":900,"2014":901,"2015":902,"2016":903,"2017":904,"2018":617,"2019":905,"2020":906,"2021":907,"2022":908,"2023":909,"2024":567},{"2018":278,"2019":40,"2020":127,"2021":145},{"2018":105,"2019":32,"2020":107,"2021":513},{"pages":1219,"volume":1221},{"VOID":1220},"1-15",{"VOID":1222},"11","2018-12-01",2018,[783],{"id":1227,"createTime":1228,"updateTime":1229,"relativeEntities":1230,"slug":1231,"properties":1232,"entityType":929,"verifyStatus":26,"verifyTime":1229,"verifyNote":1077,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1241,"fullTextUrl":28,"authors":1242,"publicationType":1031,"publisherRelationship":1286,"citationCount":28,"citationInfo":28,"publishDate":1311,"publishYear":1312,"citationAnalyzeStatus":882,"lastCitationAnalyze":28,"indexDatabases":1313,"openAccess":28,"references":28,"isForceReanalyzing":1061},"0009e405-e98c-46d7-8cc6-6caa997b0adf","2023-12-27T05:48:33.686+00:00","2024-12-21T12:44:04.127+00:00",[],"An-initial-assessment-of-tidal-energy-resources-using-GIS-for-Miani-Hor-Baluchistan-province-Pakistan",{"abstract":1233,"title":1235,"references":1237,"doi":1239},{"EN":1234},"An attempt is made for the first time to assess tidal energy resources at Miani Hor tidal lagoon of Baluchistan province of Pakistan by applying an innovative approach using Geographical Information System (GIS) tools\u002Ftechniques to develop different geo-statistical models. Baluchistan is the largest province of Pakistan and fortunate to have a natural tidal lagoon called Miani Hor. The potential of harnessing tidal energy in Miani Hor tidal lagoon is considered to provide great benefits for future energy resource in Baluchistan province of Pakistan, but no relevant research has been carried out to estimate potential of tidal energy at Miani Hor tidal lagoon; the main reason seems to be unavailability of tidal data at said site. Therefore, a study is required to estimate and exploit energy resources of Miani Hor tidal lagoon. For this purpose, tidal data of five different locations was acquired along the coast, predictions were made for tidal data at Miani Hor, and validation was performed. To estimate the energy resources at Miani Hor, best-fitted method was selected for the model development. Based on the results of model, consideration of tidal lagoon impoundment and location for the sluices is discussed. Finally, with an impoundment area of 161.50 km2 and sluices’ width of 1.72 km, 121.1 MW power generation is estimated with proposed turbine array.",{"EN":1236},"An initial assessment of tidal energy resources using GIS for Miani Hor, Baluchistan province, Pakistan",{"VOID":1238},"AEDB (2017) RE Projects. Alternative Energy Development Board. http:\u002F\u002Fwww.aedb.org\u002Findex.php\u002Fae-technologies\u002Fcarbon-credit\u002Fclean-development-mechanism-cdm. Accessed August 24, 2017\nAmer M, Daim TU (2011) Selection of renewable energy technologies for a developing county: a case of Pakistan. Energy Sustain Dev 15(4):420–435\nAmjad AS, Jusoff K (2007) Mangrove conservation through community participation in Pakistan: the case of Sonmiani Bay. In: The 5th WSEAS International Conference on Environment, Ecosystems and Development (EED'07), Puerto De La Cruz, Tenerife, Canary Islands, Spain\nAndritz (2016) Andritz. https:\u002F\u002Fwww.andritz.com\u002Findex.htm. September 2016\nAsif M (2009) Sustainable energy options for Pakistan. Renew Sust Energ Rev 13(4):903–909\nBlunden L, Bahaj A (2006) Initial evaluation of tidal stream energy resources at Portland Bill, UK. Renew Energy 31(2):121–132\nBlunden L, Bahaj A, Aziz N (2013) Tidal current power for Indonesia? An initial resource estimation for the Alas Strait. Renew Energy 49:137–142\nCarballo R, Iglesias G, Castro A (2009) Numerical model evaluation of tidal stream energy resources in the Ría de Muros (NW Spain). Renew Energy 34(6):1517–1524\nDefne Z, Haas KA, Fritz HM (2011) GIS based multi-criteria assessment of tidal stream power potential: a case study for Georgia, USA. Renew Sust Energ Rev 15(5):2310–2321\nEMSD (2013) Electrical and mechanical services department. Renewable Energy http:\u002F\u002Fwww.emsd.gov.hk\u002Femsd\u002Fe_download\u002Fsgi\u002Fre_pamphlet.pdf. 2014\nESRI (March 2017). http:\u002F\u002Fdesktop.arcgis.com\u002Fen\u002Farcmap\u002Flatest\u002Fextensions\u002Fgeostatistical-analyst\u002Fusing-cross-validation-to-assess-parameter-values.htm. Accessed March 2017\nGorlov A (2001) Tidal energy. Academic, London\nInsaf A, Baig MS, Kausar A, Rauf T, Shahzad M, Khan SA, Uddin Z (2016) Estimation of various tidal parameters and possibility for harnessing tidal energy along the southeast coastal area of Karachi, Pakistan. Sci Int (Lahore) 28(1):179–185\nKarsten RH, McMillan J, Lickley M, Haynes R (2008) Assessment of tidal current energy in the Minas passage, bay of Fundy. Proc Inst Mech Eng A J Power Energy 222(5):493–507\nLedoux H, Gold C (2005) An efficient natural neighbour interpolation algorithm for geoscientific modelling. In: Developments in Spatial Data Handling. Springer, Berlin, Heidelberg, pp 97–108\nLewis M, Neill S, Robins P, Hashemi M (2015) Resource assessment for future generations of tidal-stream energy arrays. Energy 83:403–415\nMaulud KA, Karim O, Sopian K, Darus ZM, Ramly EM (2008) Identification a potential wave energy location in Malaysia using GIS. In WSEAS International Conference. Proceedings. Mathematics and Computers in Science and Engineering (No. 10). WSEAS\nMaulud KA, Mohtar WW, Karim OA (2013) Spatial multi criteria analysis for the determination of areas with high potential wave energy. Jurnal Teknologi 65(2):113–120\nMitas L, Mitasova H (1999) Spatial interpolation. Geogr Inf Syst 1:481–492\nMT (2016) Mavel Turbines http:\u002F\u002Fwww.mavel.cz\u002F. Accessed September 2016\nMukhtar I, Hannan A (2012) Constrains on mangrove forests and conservation projects in Pakistan. J Coast Conserv 16(1):51–62\nNeill SP, Jordan JR, Couch SJ (2012) Impact of tidal energy converter (TEC) arrays on the dynamics of headland sand banks. Renew Energy 37(1):387–397\nNobre A, Pacheco M, Jorge R, Lopes M, Gato L (2009) Geo-spatial multi-criteria analysis for wave energy conversion system deployment. Renew Energy 34(1):97–111\nOssberger (2016) Ossberger Hydro. http:\u002F\u002Fwww.ossberger.de\u002Fcms\u002Fen\u002Fhome\u002F. Accessed September 2016\nPEY (2015) Pakistan energy yearbook 2015. Hydrocarbon Development Institute of Pakistan, Islambad\nPMD Climate Data Processing Centre (2015) Pakistan Meteorological Department. http:\u002F\u002Fwww.pmd.gov.pk\u002Fcdpc\u002Fhome.htm. Accessed December 2015\nPolagye B, Kawase M, Malte P (2009) In-stream tidal energy potential of Puget Sound, Washington. Proc Inst Mech Eng A J Power Energy 223(5):571–587\nRamachandra T, Shruthi B (2007) Spatial mapping of renewable energy potential. Renew Sust Energ Rev 11(7):1460–1480\nRashid A (2012) Status and potentials of tidal in-stream energy resources in the southern coasts of Iran: a case study. Renew Sust Energ Rev 16(9):6668–6677\nRF (2016) Renewables First. https:\u002F\u002Fwww.renewablesfirst.co.uk\u002F. Accessed September 2016\nSahir MH, Qureshi AH (2008) Assessment of new and renewable energy resources potential and identification of barriers to their significant utilization in Pakistan. Renew Sust Energ Rev 12(1):290–298\nSliz-Szkliniarz B, Vogt J (2011) GIS-based approach for the evaluation of wind energy potential: a case study for the Kujawsko–Pomorskie Voivodeship. Renew Sust Energ Rev 15(3):1696–1707\nSutherland G, Foreman M, Garrett C (2007) Tidal current energy assessment for Johnstone Strait, Vancouver island. Proceedings of the Institution of Mechanical Engineers, Part A: Journal of Power and Energy 221 (2):147–157\nTIC (2016) Toshiba International Corporation http:\u002F\u002Fwww.tic.toshiba.com.au\u002F. Accessed September 2016\nTwidell J, Weir AD (2015) Renewable energy resources. Routledge. https:\u002F\u002Fdoi.org\u002F10.4324\u002F9781315766416\nUNDP, U (2000) WEC (2000) World Energy Assessment: Energy and the challenge of sustainability. United Nations Development Programme, New York\nVan Hoesen J, Letendre S (2010) Evaluating potential renewable energy resources in Poultney, Vermont: a GIS-based approach to supporting rural community energy planning. Renew Energy 35(9):2114–2122\nVE (2016) VerdErg. http:\u002F\u002Fwww.verdergrenewableenergy.com\u002F. Accessed September 2016\nVLH (2016) Very low head turbine. http:\u002F\u002Fwww.vlh-turbine.com\u002F. Accessed September 2016\nWikipedia (2017) Balochistan, Pakistan. https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBalochistan,_Pakistan. Accessed July 25, 2016",{"VOID":1240},"10.1007\u002Fs12517-020-5191-5","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs12517-020-5191-5",[1243,1258,1273],{"id":1244,"sortIndex":32,"researcher":28,"roles":1245,"affiliations":1246,"properties":1255,"displayName":1257,"givenName":28,"familyName":28},"e960bd94-b4b8-49a3-a9fb-ed185912f04e",[935],[1247],{"id":1248,"sortIndex":32,"affiliation":1249,"properties":28},"11973f20-ac45-48a2-b76b-19004bc75e85",{"id":1248,"createTime":28,"updateTime":28,"relativeEntities":1250,"slug":28,"properties":1251,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1254,"statistic":28},[],{"title":1252},{"VI":1253},"Department of Applied Physics, University of Karachi, Sindh, Pakistan",[],{"title":1256},{"VI":1257},"Ambreen Insaf",{"id":1259,"sortIndex":40,"researcher":28,"roles":1260,"affiliations":1261,"properties":1270,"displayName":1272,"givenName":28,"familyName":28},"66c64304-53c1-419f-80f6-e58d380f0a40",[935],[1262],{"id":1263,"sortIndex":32,"affiliation":1264,"properties":28},"0f2f998b-29ee-40ba-b2af-d82e24dbbd2b",{"id":1263,"createTime":28,"updateTime":28,"relativeEntities":1265,"slug":28,"properties":1266,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1269,"statistic":28},[],{"title":1267},{"VI":1268},"Department of Physics, University of Karachi, Sindh, Pakistan",[],{"title":1271},{"VI":1272},"Zaheer Uddin",{"id":1274,"sortIndex":123,"researcher":28,"roles":1275,"affiliations":1276,"properties":1283,"displayName":1285,"givenName":28,"familyName":28},"478cb91a-8d1c-4716-8ce8-7dec6f1160fa",[935],[1277],{"id":1248,"sortIndex":32,"affiliation":1278,"properties":28},{"id":1248,"createTime":28,"updateTime":28,"relativeEntities":1279,"slug":28,"properties":1280,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1282,"statistic":28},[],{"title":1281},{"VI":1253},[],{"title":1284},{"VI":1285},"Mirza Salman Baig",{"url":1241,"publisher":1287,"properties":1307},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1288,"slug":872,"properties":1289,"entityType":25,"verifyStatus":882,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1293,"manageAffiliations":1294,"indexDatabases":1295,"url":28,"thumbnailPath":28,"statistic":1302,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1290,"title":1291,"eissn":1292},{"VOID":877},{"EN":879},{"VOID":875},[],[],[1296],{"id":887,"indexDatabase":1297,"url":893,"indexYears":894,"academicFieldIds":28,"indexDatabaseRanking":788},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1298,"label":1299,"description":1300,"key":781,"publicationTags":1301,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],{"impactFactor":32,"impactFactorByYear":1303,"i10Index":123,"i10IndexLast5Year":40,"totalPublication":897,"totalPublicationByYear":1304,"totalCitation":567,"totalCitationByYear":1305,"totalCitationPerPublication":513,"totalCitationPerPublicationByYear":1306,"hindexLast5Year":45,"hindex":45},{"2019":513,"2020":513,"2021":32,"2022":32,"2023":32},{"2008":205,"2009":149,"2010":161,"2011":331,"2012":899,"2013":900,"2014":901,"2015":902,"2016":903,"2017":904,"2018":617,"2019":905,"2020":906,"2021":907,"2022":908,"2023":909,"2024":567},{"2018":278,"2019":40,"2020":127,"2021":145},{"2018":105,"2019":32,"2020":107,"2021":513},{"pages":1308,"volume":1309},{"VOID":1220},{"VOID":1310},"13","2020-02-14",2020,[783],{"id":1315,"createTime":1316,"updateTime":1317,"relativeEntities":1318,"slug":1319,"properties":1320,"entityType":929,"verifyStatus":26,"verifyTime":1317,"verifyNote":1077,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1329,"fullTextUrl":28,"authors":1330,"publicationType":1031,"publisherRelationship":1429,"citationCount":28,"citationInfo":28,"publishDate":1455,"publishYear":1456,"citationAnalyzeStatus":882,"lastCitationAnalyze":28,"indexDatabases":1457,"openAccess":28,"references":28,"isForceReanalyzing":1061},"001ab837-90d3-415c-854a-1ef84e194d0e","2024-01-02T04:02:47.168+00:00","2024-12-09T01:16:38.887+00:00",[],"Numerical-investigation-of-the-evolution-of-overlying-strata-and-distribution-of-static-and-dynamic-loads-in-a-deep-island-coal-panel",{"abstract":1321,"title":1323,"references":1325,"doi":1327},{"EN":1322},"A systematic approach to numerically simulating an island longwall panel operation is proposed: it aims to investigate the evolution of overlying strata, static stress and displacement response and dynamic load arising from roof fracturing and fault slip. The results show that due to a small gob width (70 m) on both sides, the evolution height of overlying strata is limited, i.e. the heights of the cave-in zone and fracture zone are 30.98 and 66.91 m, respectively. The numerical model matches the theoretical analysis and field observations. Dynamic analysis reveals that the envelope of mine tremors confirms the good correlation with the evolution of the fracture zone. As the mining panel is far from the fault, fault slip does not occur; at this time, the dynamic load mainly comes from roof fracturing. When mining activities approach the fault, the calculation of the dynamic response of fault slip is performed over the area where the increase of relative shear displacement during dynamic analysis exceeds 0.05 m and where the shear stress along the fault decreases. It is shown that during the initial stage of the mining process, and in a square mining panel, fault slip is more likely to occur, leading to strong tremors and rock bursts, which become more notable in the later stages of the mining of the island panel.",{"EN":1324},"Numerical investigation of the evolution of overlying strata and distribution of static and dynamic loads in a deep island coal panel",{"VOID":1326},"Aki K, Richards R G (1980) Quantitative seismology: theory and method [M]. San Francisco: Freeman\nBai M, Kendorski F S, Van Roosendaal D J. (1995) Chinese and north American high-extraction underground coal mining strata behavior and water protection experience and guidelines [C]. Proceedings of the 14th International Conference on Ground Control in Mining, Morgantown. p. 209–217\nBai QS, Tu SH, Wang FT, Zhang XG, Tu HS, Yuan Y (2014) Observation and numerical analysis of the scope of fractured zones around gate roads under longwall influence. Rock Mech Rock Eng 47(5):1939–1950. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00603-013-0457-9\nBai QS, Tu SH, Wang FT, Zhang C (2017) Field and numerical investigations of gateroad system failure induced by hard roofs in a longwall top coal caving face. Int J Coal Geol 173:176–199. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.coal.2017.02.015\nBarton N, Choubey V (1977) The shear strength of rock joints in theory and practice. Rock Mech 10(1–2):1–54. https:\u002F\u002Fdoi.org\u002F10.1007\u002FBF01261801\nBasarir H, Ferid Oge I, Aydin O (2015) Prediction of the stresses around main and tail gates during top coal caving by 3D numerical analysis. Int J Rock Mech Min Sci 76:88–97\nBizzarri A (2012) Rupture speed and slip velocity: what can we learn from simulated earthquake? Earth Planet Sci Lett 317-378:196–203\nChristopher M (2007) Multiple-seam mining in the United States: background, in: Proceedings of the New Technology for Ground Control in Multiple-seam Mining, U.S. Department of Health and Human Services, Centers for Disease Control and Prevention, National Institute for Occupational Safety and Health, Pittsburgh Research Laboratory, Pittsburgh, PA, pp. 3–14\nDomanski B, Gibowicz SJ (2008) Comparison of source parameters estimated in the frequency and time domains for seismic events at the Rudna copper mine, Poland. Acta Geophys 56(2):324–343\nDou LM, He H (2012) Study of OX-F-T spatial structure evolution of overlying strata in coal mines. China J Rock Mech Eng 31(3):453–460 (in Chinese)\nDou LM, Mu ZL, Li ZL, Cao AY, Gong SY (2014) Research progress of monitoring, forecasting, and prevention of rockburst in underground coal mining in China. Int J Coal Sci Technol 1(3):278–288. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs40789-014-0044-z\nDou LM, He J, Cao AY, Gong SY, Cai W (2015) Rock burst prevention methods based on theory of dynamic and static combined load induced in coal mine. J China Coal Soc 40(7):1469–1476 (in Chinese)\nDu XL, Song HW, Chen J (2011) Numerical simulation of the evolution of the pressure arch during coal mining. J China Univ Min Technol 40(6):863–867\nDunham EM, Bhat HS (2008) Attenuation of radiated ground motion and stresses from three-dimensional supershear rupture. J Geophys Res 113(B8):231–234\nFeng Y, Jiang FX, J d L (2015) Evaluation method of rock burst hazard induced by overall instability of island coal face. J China Coal Soc 40(5):1001–1007 (in Chinese)\nGao W, Ge MM (2016) Stability of a coal pillar for strip mining based on an elastic-plastic analysis. Int J Rock Mech Min Sci 87:23–28\nHe J, Dou LM, Cai W, Li ZL, Ding YL (2014) Mechanism of dynamic and static combined load inducing rock burst in thin coal seam. J China Coal Soc 39(11):2177–2182 (in Chinese)\nHenning J, Mitri HS (2010) Production blast-induced vibrations in longhole open stoping—a case study. Int J. Geotech Earthq Eng 1(2):1–11. https:\u002F\u002Fdoi.org\u002F10.4018\u002Fjgee.2010070101\nHofmann GF, Scheepers LJ (2011) Simulating fault slip areas of mining induced seismic tremors using static boundary element numerical modelling. Min Technol 120(1):53–64. https:\u002F\u002Fdoi.org\u002F10.1179\u002F037178411X12942393517291\nHoek E (2001) Rock mass properties for underground mines. In: Proceedings of Underground Mining Methods: Engineering Fundamentals and International Case Studies. Littleton, CO.\nIannacchione AT, Tadolini SC (2016) Occurrence, predication, and control of coal burst events in the U.S. Int J Min Sci Technol 26(1):39–46. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.ijmst.2015.11.008\nItasca Consulting Group Inc (2012) FLAC3D fast Lagrangian analysis of continua in 3 dimensions user’s guide. Itasca, Minneapolis\nIvins ER, Lyzenga GA (1968) Stress patterns in an interplane shear zone: an effective anisotropic model and implications for the transverse ranges, California. Philos Trans R Soc London, Ser A 318:285–347\nJiang YD, Wang HW, Xue S, Zhao YX, Zhu J, Pang XF (2012) Assessment and mitigation of coal bump risk during extraction of an island longwall panel. Int J Coal Geol 95(2):20–33. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.coal.2012.02.003\nKaracan CÖ, Esterhuizen GS, Schatzel SJ, Diamond WP (2007) Reservoir simulation-based modelling for characterizing longwall methane emissions and gob gas vent hole production. Int J Coal Geol 71(2–3):225–245. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.coal.2006.08.003\nKhairil (2003) A study on stress rock arch development around dual caverns [D]. Nanyang Technological University, Singapore\nLi XB, Cao WZ, Tao M, Zhou ZL, Chen ZH (2016) Influence of unloading disturbance on adjacent tunnels. Int J Rock Mech Min Sci 84:10–24\nLysmer J, Kuhlemeyer RL (1969) Finite dynamic model for infinite media. J Eng Mech 95(EM4):859–877\nMark C, Gauna M (2016) Evaluating the risk of coal bursts in underground coal mines. Int J Min Sci Technol 26(1):47–52. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.ijmst.2015.11.009\nPeng SS, Chiang HS (1984) Longwall mining [M]. Wiley, New York, p 708\nPotvin Y, Jarufe J, Wesseloo J (2013) Interpretation of seismic data and numerical modelling of fault reactivation at el Teniente, Reservas Norte sector. Min Technol IMM Trans A 119(3):175–181\nQian MG, Shi PW (2003) Mine pressure and ground control [M]. China University of Mining and Technology Press, Xuzhou, pp 69–70 (in Chinese)\nSainoki A, Mitri HS (2016) Dynamic modeling of fault slip induced by stress waves due to stope production blasts. Rock Mech Rock Eng 49(1):165–181. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00603-015-0721-2\nSaharan MR, Mitri HS, Jethwa JL (2006) Rock fracturing by explosive energy: review of state-of-the-art. Fragblast 10(1-2):61–81. https:\u002F\u002Fdoi.org\u002F10.1080\u002F13855140600858792\nShabanimashcool M, Li CC (2012) Numerical modelling of the longwall mining and stability study of the gates in the Svea Nord coalmine. Int J Rock Mech Min Sci 51:24–34. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.ijrmms.2012.02.002\nSjoberg J, Perman F, Quinteiro C, Malmgren L (2013) Numerical analysis of alternative mining sequences to minimize potential for fault slip rockbursting. Min Technol IMM Trans A 121(4):226–235\nSneilling PE, Godin L, McKinnon SD (2013) The role of geologic structure and stress in triggering remote seismicity in Creighton Mine, Sudbury, Canada. Int J Rock Mech Min Sci 58(1):166–179\nTu M (2004) Study on the growth height of separation fracture of mining rock in Panxie area. J China Coal Soc 29(6):641–645 (in Chinese)\nWang GH, Wang YX, Lu WB, Zhou W, Chen M, Yan P (2016a) On the determination of the mesh size for numerical simulations of shock wave propagation in near field underwater explosion. Appl Ocean Res 24(9):925–945\nWang HB, Zhang HB, Tian Z, Ou ZC, Zhou G (2016b) Mesh size effect and its mechanism research in numerical calculation of rock dynamics. Aata Armamentarii 37(10):1828–1836 (in Chinese)\nYang GY, Jiang FX, Wang CW (2014) Prevention and control technology of mine pressure bumping of coal mining face in seam island based on deep mining and thick topsoil of complex spatial structure of overlying strata [J]. Chin J Geotech Eng 36(1):189–194 (in Chinese)\nYavuz H (2004) An estimation method for cover pressure re-establishment distance and pressure distribution in the goaf of longwall coal mines. Int J Rock Mech Min Sci 41(2):193–205. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS1365-1609(03)00082-0\nZhang SR, Li HB, Wang GH, Kong Y (2015) Comparative analysis of mesh size effects on numerical simulation of shock wave in air blast and underwater explosion. J Hydraul Eng 46(3):298–306 (in Chinese)\nZukas JA, Scheffler DR (2000) Practical aspects of numerical simulations of dynamic events: effects of meshing. Int J Impact Eng 59:1–9",{"VOID":1328},"10.1007\u002Fs12517-017-3300-x","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs12517-017-3300-x",[1331,1355,1370,1383,1396,1409],{"id":1332,"sortIndex":32,"researcher":28,"roles":1333,"affiliations":1334,"properties":1352,"displayName":1354,"givenName":28,"familyName":28},"1a1856f4-fc65-43c9-b1cb-00e13c0330ad",[935],[1335,1343],{"id":1336,"sortIndex":32,"affiliation":1337,"properties":28},"7698d25c-9abb-4b93-9253-ca1649d05dc2",{"id":1336,"createTime":28,"updateTime":28,"relativeEntities":1338,"slug":28,"properties":1339,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1342,"statistic":28},[],{"title":1340},{"VI":1341},"School of Energy Engineering, Xi’an University of Science and Technology, Xi’an, China",[],{"id":1344,"sortIndex":40,"affiliation":1345,"properties":1351},"dbb97ae2-0a6d-4a2d-b77b-dbdd0e8cd781",{"id":1344,"createTime":28,"updateTime":28,"relativeEntities":1346,"slug":28,"properties":1347,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1350,"statistic":28},[],{"title":1348},{"VI":1349},"Key Laboratory of Western Mine Exploitation and Hazard Prevention with Ministry of Education, Xi’an, China",[],{},{"title":1353},{"VI":1354},"Guang-an 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Dou",{"id":1371,"sortIndex":123,"researcher":28,"roles":1372,"affiliations":1373,"properties":1380,"displayName":1382,"givenName":28,"familyName":28},"7c959346-042d-4997-9a22-36a8bd8c735b",[935],[1374],{"id":1360,"sortIndex":32,"affiliation":1375,"properties":28},{"id":1360,"createTime":28,"updateTime":28,"relativeEntities":1376,"slug":28,"properties":1377,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1379,"statistic":28},[],{"title":1378},{"VI":1365},[],{"title":1381},{"VI":1382},"Chang-bin Wang",{"id":1384,"sortIndex":42,"researcher":28,"roles":1385,"affiliations":1386,"properties":1393,"displayName":1395,"givenName":28,"familyName":28},"5b005bf9-15c6-48e2-b8df-93a653d89534",[935],[1387],{"id":1360,"sortIndex":32,"affiliation":1388,"properties":28},{"id":1360,"createTime":28,"updateTime":28,"relativeEntities":1389,"slug":28,"properties":1390,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1392,"statistic":28},[],{"title":1391},{"VI":1365},[],{"title":1394},{"VI":1395},"Jing Li",{"id":1397,"sortIndex":45,"researcher":28,"roles":1398,"affiliations":1399,"properties":1406,"displayName":1408,"givenName":28,"familyName":28},"1324457f-6173-4d8c-81c5-6ab17de3cbfd",[935],[1400],{"id":1360,"sortIndex":32,"affiliation":1401,"properties":28},{"id":1360,"createTime":28,"updateTime":28,"relativeEntities":1402,"slug":28,"properties":1403,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1405,"statistic":28},[],{"title":1404},{"VI":1365},[],{"title":1407},{"VI":1408},"Wu Cai",{"id":1410,"sortIndex":46,"researcher":28,"roles":1411,"affiliations":1412,"properties":1426,"displayName":1428,"givenName":28,"familyName":28},"76415167-9f9c-4059-b339-25121950c456",[935],[1413,1419],{"id":1336,"sortIndex":32,"affiliation":1414,"properties":28},{"id":1336,"createTime":28,"updateTime":28,"relativeEntities":1415,"slug":28,"properties":1416,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1418,"statistic":28},[],{"title":1417},{"VI":1341},[],{"id":1344,"sortIndex":40,"affiliation":1420,"properties":1425},{"id":1344,"createTime":28,"updateTime":28,"relativeEntities":1421,"slug":28,"properties":1422,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1424,"statistic":28},[],{"title":1423},{"VI":1349},[],{},{"title":1427},{"VI":1428},"Zi-wei Ding",{"url":1329,"publisher":1430,"properties":1450},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1431,"slug":872,"properties":1432,"entityType":25,"verifyStatus":882,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1436,"manageAffiliations":1437,"indexDatabases":1438,"url":28,"thumbnailPath":28,"statistic":1445,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1433,"title":1434,"eissn":1435},{"VOID":877},{"EN":879},{"VOID":875},[],[],[1439],{"id":887,"indexDatabase":1440,"url":893,"indexYears":894,"academicFieldIds":28,"indexDatabaseRanking":788},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1441,"label":1442,"description":1443,"key":781,"publicationTags":1444,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],{"impactFactor":32,"impactFactorByYear":1446,"i10Index":123,"i10IndexLast5Year":40,"totalPublication":897,"totalPublicationByYear":1447,"totalCitation":567,"totalCitationByYear":1448,"totalCitationPerPublication":513,"totalCitationPerPublicationByYear":1449,"hindexLast5Year":45,"hindex":45},{"2019":513,"2020":513,"2021":32,"2022":32,"2023":32},{"2008":205,"2009":149,"2010":161,"2011":331,"2012":899,"2013":900,"2014":901,"2015":902,"2016":903,"2017":904,"2018":617,"2019":905,"2020":906,"2021":907,"2022":908,"2023":909,"2024":567},{"2018":278,"2019":40,"2020":127,"2021":145},{"2018":105,"2019":32,"2020":107,"2021":513},{"pages":1451,"volume":1453},{"VOID":1452},"1-22",{"VOID":1454},"10","2017-12-22",2017,[783],{"id":1459,"createTime":1460,"updateTime":1461,"relativeEntities":1462,"slug":1463,"properties":1464,"entityType":929,"verifyStatus":26,"verifyTime":1461,"verifyNote":1077,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1473,"fullTextUrl":28,"authors":1474,"publicationType":1031,"publisherRelationship":1518,"citationCount":28,"citationInfo":28,"publishDate":1543,"publishYear":1059,"citationAnalyzeStatus":882,"lastCitationAnalyze":28,"indexDatabases":1544,"openAccess":28,"references":28,"isForceReanalyzing":1061},"0021d3d7-aa48-4b9d-a4b1-3cd4496c99c5","2023-12-12T14:05:23.546+00:00","2025-01-30T10:06:07.773+00:00",[],"A-deterministic-seismic-risk-macrozonation-of-Seville",{"abstract":1465,"title":1467,"references":1469,"doi":1471},{"EN":1466},"The seismicity of the southwestern Iberian Peninsula is moderate but large events with long return periods occur (≈ 200 years). This exceeds the life of various generations, making the population unacquainted with the seismic hazard. On the one hand, this results in a low demanding seismic code which increases the seismic vulnerability and, therefore, the seismic risk. On the other hand, the local emergency services must be properly prepared to face a destructive seismic event, with emergency plans and mitigation strategies. This assumption enhances the need of assessing the seismic risk of Seville in a civil protection context. For all the aforementioned and for the lack of instrumental data of relevant earthquakes, the assessment of the seismic hazard in this area is challenging. To do this, seismogenic zones of the new seismic hazard map of Spain have been used as sources. The peak ground acceleration (PGA) for each scenario has been calculated by means of ground motion prediction equations (GMPE). To estimate the site effects, in a 1D model environment, a shear wave velocity (Vs) map of the top 5 m has been depicted based on the standard penetration test (SPT). Seville’s building stock has been classified in agreement with the previous works in Lorca and Barcelona to determine its vulnerability. The main goal of this work was to investigate the influence of the soil amplification on the seismic behaviour of different building typologies. Therefore, the final target was to plot the damage scenarios expected in Seville under a maximum credible earthquake by means of a deterministic seismic hazard assessment (DSHA). As outputs, the scenario modelled showed that around 27 000 buildings would experience a moderate damage and that 26 000 would suffer pre-collapse or even collapse. Thus, approximately 10% of the population would lose their dwellings. Regarding the human loses, around 22 000 people would suffer serious injuries and approximately 5 000 people would die. 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Instituto Geológico y Minero de España (eds), Madrid\nRe M (2000) Natural catastrophes, current position, special issue. Munich Reinsurance Co., Munich\nRehman F, El-Hady SM, Atef AH, Harbi HM (2016) Seismic hazard assessment of western coastal province of Saudi Arabia: deterministic approach. Earthquake Sci 29(5):299–309\nRuiz-Constán A, Ruiz-Armenteros AM, Galindo-Zaldívar J, Lamas-Fernández F, Sousa JJ, Sanz de Galdeano C et al (2017) Factors determining subsidence in urbanized floodplains: evidence from MTInSAR in Seville. Earth Surface Processes Landforms 42(14):2484–2497\nSalgado-Gálvez MA, Cardona OD, Carreño ML, Barbat AH (2015) Probabilistic seismic hazard and risk assessment in Spain. Monograph Series in Earthquake Engineering, ed. AH Barbat\nSilva V, Crowley H, Varum H, Pinho R (2015) Seismic risk assessment for mainland Portugal. Bull Earthquake Eng 13(2):429–457\nSousa ML, Carvalho A, Bilé Serra J, Mateus M, Martins A(2008) Estudo do risco sísmico e de tsunamis do Algarve (ERSTA), Relatório final. LNEC tec. report 295\u002F2008, Lisbon, 1–85. (In Portuguese)\nSpence R, So E, Jenny S, Castella H, Ewald M, Booth E (2008) The global earthquake vulnerability estimation system (GEVES): an approach for earthquake risk assessment for insurance applications. Bull Earthq Eng 6:463–483\nStewart JP, Douglas J, Javanbarg M, Bozorgnia Y, Abrahamson N, Boore D, Campbell K, Delavaud E, Erdik M, Stafford P (2015) Selection of ground motion prediction equations for the global earthquake model. Earthquake Spectra 31(1):19–45\nStewart JP, Choi Y, Graves RW (2005) Empirical characterization of site conditions on strong ground motion. University of California, Berkeley\nTezcan S, Ozdemir Z (2011) A refined formula for the allowable soil pressure using shear wave velocities. Open Civil Eng J 5(1)\nUnited Nations. International Strategy for Disaster Reduction. Secretariat. (2015) Global assessment report on DRR 2015: making development sustainable: the future of disaster risk management. UN\nVilanova SP, Fonseca JF (2007) Probabilistic seismic-hazard assessment for Portugal. Bull Seismol Soc Am 97(5):1702–1717\nVilanova SP, Fonseca JF (2004) Seismic hazard impact of the Lower Tagus Valley Fault Zone (SW Iberia). J Seismol 8:331–345. https:\u002F\u002Fdoi.org\u002F10.1023\u002FB:JOSE.0000038457.01879.b0\nVillamor Pérez MP, Stirling MW, Tsige Aga M, Berryman KR, Martínez Díaz JJ, Martín-González F (2012) Contribution of active faults in the intraplate area of Iberia to seismic hazard: The Alentejo-Plasencia Fault. J Iberian Geol 38(1):85–111\nWang JP, Huang D, Yang Z (2012) Deterministic seismic hazard map for Taiwan developed using an in-house Excel-based program. Comput Geosci 48:111–116\nZadehmohamad M (2020) Evaluation of cyclic displacement amplitude of integral bridge abutment on backfill soil pressure and settlements. J Transport Res",{"VOID":1472},"10.1007\u002Fs12517-021-08626-7","https:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs12517-021-08626-7",[1475,1490,1505],{"id":1476,"sortIndex":32,"researcher":28,"roles":1477,"affiliations":1478,"properties":1487,"displayName":1489,"givenName":28,"familyName":28},"6d183ae4-ad63-4e67-8e6b-1ae6966b7f7c",[935],[1479],{"id":1480,"sortIndex":32,"affiliation":1481,"properties":28},"6c0cb1a8-6ac7-4524-8862-144a81f2e7b5",{"id":1480,"createTime":28,"updateTime":28,"relativeEntities":1482,"slug":28,"properties":1483,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1486,"statistic":28},[],{"title":1484},{"VI":1485},"Department of Emergency Planning National, Portuguese National Authority for Civil Protection, Carnaxide, Portugal",[],{"title":1488},{"VI":1489},"Luis Fazendeiro Sá",{"id":1491,"sortIndex":40,"researcher":28,"roles":1492,"affiliations":1493,"properties":1502,"displayName":1504,"givenName":28,"familyName":28},"c7f8a4b9-9735-4280-9b83-61f425716202",[935],[1494],{"id":1495,"sortIndex":32,"affiliation":1496,"properties":28},"26132f3c-92f6-444a-b517-76c1a7bac370",{"id":1495,"createTime":28,"updateTime":28,"relativeEntities":1497,"slug":28,"properties":1498,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1501,"statistic":28},[],{"title":1499},{"VI":1500},"Department of Building Structures and Geotechnical Engineering, University of Seville, Seville, Spain",[],{"title":1503},{"VI":1504},"Antonio Morales-Esteban",{"id":1506,"sortIndex":123,"researcher":28,"roles":1507,"affiliations":1508,"properties":1515,"displayName":1517,"givenName":28,"familyName":28},"3f39fecd-9ac6-4b98-8337-3546b292dd2a",[935],[1509],{"id":1495,"sortIndex":32,"affiliation":1510,"properties":28},{"id":1495,"createTime":28,"updateTime":28,"relativeEntities":1511,"slug":28,"properties":1512,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1514,"statistic":28},[],{"title":1513},{"VI":1500},[],{"title":1516},{"VI":1517},"Percy Durand Neyra",{"url":1473,"publisher":1519,"properties":1539},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1520,"slug":872,"properties":1521,"entityType":25,"verifyStatus":882,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1525,"manageAffiliations":1526,"indexDatabases":1527,"url":28,"thumbnailPath":28,"statistic":1534,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1522,"title":1523,"eissn":1524},{"VOID":877},{"EN":879},{"VOID":875},[],[],[1528],{"id":887,"indexDatabase":1529,"url":893,"indexYears":894,"academicFieldIds":28,"indexDatabaseRanking":788},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1530,"label":1531,"description":1532,"key":781,"publicationTags":1533,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],{"impactFactor":32,"impactFactorByYear":1535,"i10Index":123,"i10IndexLast5Year":40,"totalPublication":897,"totalPublicationByYear":1536,"totalCitation":567,"totalCitationByYear":1537,"totalCitationPerPublication":513,"totalCitationPerPublicationByYear":1538,"hindexLast5Year":45,"hindex":45},{"2019":513,"2020":513,"2021":32,"2022":32,"2023":32},{"2008":205,"2009":149,"2010":161,"2011":331,"2012":899,"2013":900,"2014":901,"2015":902,"2016":903,"2017":904,"2018":617,"2019":905,"2020":906,"2021":907,"2022":908,"2023":909,"2024":567},{"2018":278,"2019":40,"2020":127,"2021":145},{"2018":105,"2019":32,"2020":107,"2021":513},{"pages":1540,"volume":1542},{"VOID":1541},"1-21",{"VOID":1057},"2021-11-10",[783],{"id":1546,"createTime":1547,"updateTime":1548,"relativeEntities":1549,"slug":1550,"properties":1551,"entityType":929,"verifyStatus":26,"verifyTime":1548,"verifyNote":1077,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1560,"fullTextUrl":28,"authors":1561,"publicationType":1031,"publisherRelationship":1577,"citationCount":28,"citationInfo":28,"publishDate":1603,"publishYear":1604,"citationAnalyzeStatus":882,"lastCitationAnalyze":28,"indexDatabases":1605,"openAccess":28,"references":28,"isForceReanalyzing":1061},"0027768c-19d1-4aa6-9a3f-b4b84f1d37a6","2023-12-07T10:36:03.319+00:00","2025-01-12T20:00:25.230+00:00",[],"Assessing-the-potential-for-hydrocarbon-generation-in-early-Eocene-and-Paleocene-sequences-of-the-Punjab-Platform-Basin-Pakistan-through-geochemical-and-petrophysical-analysis",{"abstract":1552,"title":1554,"references":1556,"doi":1558},{"EN":1553},"A study was carried out in the Punjab Platform Basin located in Pakistan to evaluate the potential for hydrocarbon in the early Eocene and Paleocene sequences using petrophysical and geochemical techniques. The assessment of reservoir properties for the Sakesar Formation was carried out using wireline logs, which included measurements of water saturation, hydrocarbon saturation, and porosity. Moreover, 21 well-cutting samples were collected to assess the source rock potential of the Nammal (early Eocene), Dungan, and Ranikot (Paleocene) Formations. The results showed that the Nammal and Dungan Formation samples had low to moderate TOC content, ranging from 0.21 to 2.04 wt.% and 0.45 to 0.56 wt.%, respectively, while the Ranikot Formation samples had moderate to high TOC content, ranging from 0.48 to 1.63 wt.%. The formations under study were found to have a low potential for generating hydrocarbons, as indicated by their S2 values ranging from 0.21 to 2.04 mg HC\u002Fg rock. The primary type of kerogen present in these formations was type III and mixed type II\u002FIII kerogen, and several plots confirmed the poor generative potential of these formations. The analysis of the Sakesar Formation revealed that it had higher porosity levels at depths of approximately 4163–4197 ft4, with average porosity ranging between 8 and 14% and 68.28% SH and 31.71 Sw, indicating moderate to poor reservoir potential. These findings suggest that the Sakesar Formation could potentially be a moderate-to-good reservoir.",{"EN":1555},"Assessing the potential for hydrocarbon generation in early Eocene and Paleocene sequences of the Punjab Platform Basin, Pakistan, through geochemical and petrophysical analysis",{"VOID":1557},"Ahmed W, Alam S (2007) Organic geochemistry and source rock characteristics of salt range formation, Potwar Basin, Pakistan. Pak J Hydrocarb Res 17:37–59\nAsquith GB, Krygowski D, Gibson CR (2004) Basic well log analysis, vol 16. American Association of Petroleum Geologists, Tulsa\nBordenave ML, Espitalié L, Leplat P, Oudin JL, Vandenbroucke M (1993) Screening techniques for source rock evaluation. In: Bordenave ML (ed) Applied Petroleum Geochemistry. Editions Technip, Paris, pp 217–278\nCharts, Schlumberger (1977) Log Interpretation. Schlumberger limited, New York\nFazeelat T, Jalees MI, Bianchi TS (2010) Source rock potential of Eocene, Paleocene and Jurassic deposits in the subsurface of the Potwar Basin, northern Pakistan. J Pet Geol 33(1):87–96\nHartmann DJ, Beaumont EA (1999) Treatise of petroleum geology\u002Fhandbook of petroleum geology: exploring for oil and gas traps. In: Chapter 9: predicting reservoir system quality and performance, pp 9–1\nHunt JM (1996) Petroleum geochemistry and geology, 2nd edn. W. H. Freeman and Company, New York\nKadri IB (1995) Petroleum geology of Pakistan. Pakistan Petroleum Limited\nKazmi AH, Jan MQ (1997) Geology and tectonics of Pakistan. Graphic publishers\nPeters KE (1986) Guidelines for evaluating petroleum source rock using programmed pyrolysis. AAPG Bull 70(3):318–329\nPeters K, Cassa M (1994) Applied source rock geochemistry. In: Magoon LB, Dow WG (eds) 1994, The petroleum system from source to trap, AAPG Memoir, vol 60, pp 93–117\nPeters KE, Clark ME, Gupta UD, McCaffrey MA, Lee CY (1995) Recognition of an Infracambrian source rock based on biomarkers in the Baghewala-1 oil. India AAPG bull 79(10):1481–1493\nRaza H (1973) Organic geochemistry and sedimentology of petroleum source rocks of Indus Basin: Pakistan. Geological Survey Open-File Report\nRaza HA, Ahmad W, Ali SM, Mujtaba M, Alam S, Shafeeq M et al (2008) Hydrocarbon prospects of Punjab platform Pakistan, with special reference to Bikaner-Nagaur Basin of India. Pak J Hydrocarb Res 18:1–33\nRider MH (1986) The geological interpretation of well logs. Published by Rider-French, 1st edition. Consulting Ltd., Sutherland, Scotland, pp 21–98\nShah SMI (2009) Stratigraphy of Pakistan. Government of Pakistan. Ministry of petroleum and natural resources, geological survey of Pakistan. Memoirs of the geological survey of Pakistan, published by Geological Survey of Pakistan 22(1):73–156\nShah SBA, Abdullah WH (2016) Petrophysical properties and hydrocarbon potentiality of Balkassar well 7 in Balkassar oilfield, Potwar Plateau, Pakistan. Bulletin of the Geological Society of Malaysia 62(1):73–77\nShah SBA, Abdullah WH (2017) Structural interpretation and hydrocarbon potential of Balkassar oil field, eastern Potwar, Pakistan, using seismic 2D data and petrophysical analysis. J Geol Soc India 90(3):323–328\nShah SBA, Abdullah WH, Shuib MK (2019) Petrophysical properties evaluation of Balkassar oilfield, Potwar Plateau, Pakistan: implication for reservoir characterization. Himal Geol 40(1):50–57\nShah SBA (2021) Lockhart formation provides source rocks for Potwar Basin. Oil Gas J 119(8):22–28\nShah SBA (2022) Evaluation of organic matter in Sakesar and Patala formations in southern and northern Potwar Basin. Petroleum Science and Technology, Pakistan. https:\u002F\u002Fdoi.org\u002F10.1080\u002F10916466.2022.2105360\nShah SBA (2023) Evaluation of mixed organic-rich carbonate and shale rocks of Meyal oilfield using an integrated palynofacies, geochemical and petrophysical approaches. Pet Sci Technol. https:\u002F\u002Fdoi.org\u002F10.1080\u002F10916466.2023.2175864\nShah SBA, Shah SHA, Nath M (2023a) 1-D basin modelling, 3-D reservoir mapping and source rock generative potential of Balkassar oilfield. Petroleum Science and Technology, Potwar Basin, Pakistan. https:\u002F\u002Fdoi.org\u002F10.1080\u002F10916466.2023.2175866\nShah SBA, Shah SHA, Jamshed K (2023b) An integrated palynofacies, geochemical and petrophysical analysis for characterizing mixed organic-rich carbonate and shale rocks in Potwar Basin, Pakistan: insights for multisource and reservoir rocks evaluation. J Pet Sci Eng. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.petrol.2022.111236\nTissot BP, Welte DH (1984) Petroleum formation and occurrence, 2nd edn. Springer, New York\nZahid M, Khan A, ur Rashid M, Saboor A, Ahmad S (2014) Structural interpretation of Joya Mair oil field, South Potwar, Upper Indus Basin, Pakistan, using 2D seismic data and petrophysical analysis. J Himalayan Earth Sci 47(1):73–86",{"VOID":1559},"10.1007\u002Fs12517-023-11365-6","https:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs12517-023-11365-6",[1562],{"id":1563,"sortIndex":32,"researcher":28,"roles":1564,"affiliations":1565,"properties":1574,"displayName":1576,"givenName":28,"familyName":28},"c3add0de-66c5-4fe8-9df5-b8413109e33a",[935],[1566],{"id":1567,"sortIndex":32,"affiliation":1568,"properties":28},"af3e5685-94d9-43d0-9f88-06fa9a4b1d87",{"id":1567,"createTime":28,"updateTime":28,"relativeEntities":1569,"slug":28,"properties":1570,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1573,"statistic":28},[],{"title":1571},{"VI":1572},"Department of Geology, University of Malaya, Kuala Lumpur, Malaysia",[],{"title":1575},{"VI":1576},"Syed Bilawal Ali Shah",{"url":1560,"publisher":1578,"properties":1598},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1579,"slug":872,"properties":1580,"entityType":25,"verifyStatus":882,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1584,"manageAffiliations":1585,"indexDatabases":1586,"url":28,"thumbnailPath":28,"statistic":1593,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1581,"title":1582,"eissn":1583},{"VOID":877},{"EN":879},{"VOID":875},[],[],[1587],{"id":887,"indexDatabase":1588,"url":893,"indexYears":894,"academicFieldIds":28,"indexDatabaseRanking":788},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1589,"label":1590,"description":1591,"key":781,"publicationTags":1592,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],{"impactFactor":32,"impactFactorByYear":1594,"i10Index":123,"i10IndexLast5Year":40,"totalPublication":897,"totalPublicationByYear":1595,"totalCitation":567,"totalCitationByYear":1596,"totalCitationPerPublication":513,"totalCitationPerPublicationByYear":1597,"hindexLast5Year":45,"hindex":45},{"2019":513,"2020":513,"2021":32,"2022":32,"2023":32},{"2008":205,"2009":149,"2010":161,"2011":331,"2012":899,"2013":900,"2014":901,"2015":902,"2016":903,"2017":904,"2018":617,"2019":905,"2020":906,"2021":907,"2022":908,"2023":909,"2024":567},{"2018":278,"2019":40,"2020":127,"2021":145},{"2018":105,"2019":32,"2020":107,"2021":513},{"pages":1599,"volume":1601},{"VOID":1600},"1-10",{"VOID":1602},"16","2023-03-27",2023,[],{"id":1607,"createTime":1608,"updateTime":1609,"relativeEntities":1610,"slug":1611,"properties":1612,"entityType":929,"verifyStatus":26,"verifyTime":1609,"verifyNote":1077,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1621,"fullTextUrl":28,"authors":1622,"publicationType":1031,"publisherRelationship":1696,"citationCount":28,"citationInfo":28,"publishDate":1722,"publishYear":1723,"citationAnalyzeStatus":882,"lastCitationAnalyze":28,"indexDatabases":1724,"openAccess":28,"references":28,"isForceReanalyzing":1061},"003a097d-1305-499d-ae3b-44e374bf83cd","2024-01-14T14:08:31.215+00:00","2025-02-15T04:59:15.184+00:00",[],"Regional-integrated-interpretation-of-the-hydrocarbon-prospectivity-of-the-Nile-Delta-Offshore-Egypt",{"abstract":1613,"title":1615,"references":1617,"doi":1619},{"EN":1614},"Interpretation of 2500 km of newly processed 2D seismic and regional potential field data has led to the identification of two new Miocene–Oligocene sedimentary basins in the northern part of offshore Egypt. The western part of the basin is deeper and has thick sedimentary cover. The upper part of the Miocene section is tested in its southern part through two wells, where the eastern subbasin is still virgin and is located at the intersection between Temsah basins and southeastern end of the Levantine basin. The main sedimentary unit of the basin is the Miocene–Oligocene sedimentary section, which was proven by the exploration and production activities in Nile Delta to be one of the hydrocarbon-generating facies. This fact is supported by 1D basin analysis using the average parameter values, which shows a hydrocarbon window, extending from lower Miocene to upper Miocene. The basin dimensions are more than 2000 km2 area and more than 4000 m of thickness, with variable petroleum system parameters’ potentialities, starting from Tortonian–Serravallian to lower Oligocene section.",{"EN":1616},"Regional integrated interpretation of the hydrocarbon prospectivity of the Nile Delta, Offshore Egypt",{"VOID":1618},"Abdel Aal A, Price RJ, Vaitl JD, Shrallow JA (1994) Tectonic evaluation of the Nile Delta, its impact on sedimentation and hydrocarbon potential, E.G.P.C. 12th Exploration and Production Conference, v.1, p 19–34\nAbdel Aal A, Shrallow JA, Nada H, Sharaaway O (1996) Geological evaluation of the Nile Delta, Egypt using regal, regional seismic line interpretation, E.G.P.C. 13th Exploration and Production Conference, v.1, p 224–225\nAbdel Aal A, El Barkooky A, Gerrits M, Meyer H, Schwander M, Zaki H (2000) Tectonic evaluation of the eastern Mediterranean Basin and its significance for hydrocarbon prospectivity of the Nile Delta Ultra-Deep water area, MOC 2000, Alex., Egypt\nAbdel Motaal E, Kusky TM (2003) tectonic evolution of the intraplate S-shaped Syrian arc fold thrust belt of the middle east region in the context of plate tectonics, the third international conference on the geology of Africa vol (2), p-p 139–157 (DEC. 2003) Assiut-Egypt\nAndreoletti C, Bienati N, Caponni G, Cibin P (2010) Nile Delta geological model enhancement through geology aided seismic imaging, MOC 2010, Alex., Egypt\nBailey J, Wallace J, Larsen J, Bryant W (1998) Ha’py field appraisal drilling program, E.G.P.C. 14th Exploration and Production Conference, V1. p 212–221\nBarsoum K, Aiolf C, Dalla S, Kamal M (1998) Evaluation and hydrocarbon occurrence in the Plio-Pleistocene succession of the Egyptian Mediterranean Margin. Examples from the Nile Delta basin. E.G.P.C. Exploration seminar, Cairo\nBarsoum K, Della M, Kamal M (2002) Gas chimneys in the Nile Delta slope and gas field occurrence, MOC 2002, Alex., Egypt\nBertello F, Barsoum K, Dalla S, Guesserian S (1998) Temsah discovery: a giant gas field in a deep sea turbidite environment. E.G.P.C. Exploration seminar, Cairo\nBurnham AK (1989) A simple kinetic model of petroleum formation and cracking. Lawrence Livermore National Laboratory, California\nCowan G, Shallow J (1998) The Rosetta P1 field: a fast track development case study Nile Delta Egypt. E.G.P.C. 14th Exploration and Production Conference. V2. P 222–235\nDeibis S, Futyan AR, Ince DM, Morley RJ, Seymour WP, Thompson S (1986) Stratigraphic framework of the Nile Delta and its implications with respect to regions, hydrocarbon potential, E.G.P.C. 8th Exploration Conference\nDobrin MB (1976) Introduction to geophysical prospecting, 4th edn. Mc. Graw. Hill Book Company, New York, p 223\nEl Barkoky A, Helal M (2002) Some Neogene stratigraphic aspects of the Nile Delta, MOC 2002. Alex, Egypt\nEl Heiny I, Enani N (1996) Regional stratigraphic interpretation pattern of Neogene sediments, Northern Nile Delta, Egypt, E.G.P.C. 13th Exploration and Production Conference, v.1, p 270–290\nEl Heiny I, Morsi S (1992) Stratigraphic correlation of the Neogene sediments in the eastern Nile Delta and Gulf of Suez, Egypt, E.G.P.C. 11th Exploration and Production Conference, v1, p 166–192\nEl Sharahan A, Saleh M (1996) Geological setting and hydrocarbon potential of north Sinai, Egypt bulletin of Canadian petroleum geology, V. 44, NO.4 (December 1996), p 615–631\nHelmy M, Fouad O (1994) Prospectivity and play assessment of Abu Qir area, Nile Delta, Egypt, E.G.P.C. 12th Exploration and Production Conference, v.1, p 277–292\nHemdan K, Barasi M (2002) The Oligocene hydrocarbon potential: a challenging opportunity for the exploratory activity in the Eastern Mediterranean Offshore., Egypt. MOC 2002, Alex, Egypt\nKamel H, Eita T, Sarhan M (1998) Nile delta hydrocarbon potentiality, Egypt, E.G.P.C. 14th Exploration and Production Conference, v.2, p 485–503\nKhaled KA, Attia GM, Metwalli FI, Fagelnour MS (2014) Subsurface geology and petroleum system in the eastern offshore area, Nile Delta, Egypt. J Appl Sci Res 10(4):254–270\nMarlow L, Kornpihl K, Kendall CGSC (2011) 2-D basin modeling study of petroleum systems in the Levantine Basin, Eastern Mediterranean. GeoArabia 16(2):17–42\nMoustafa AR, Khalil MH (1990) Structural characteristics and tectonic evolution of north Sinai fold belts. In: Said R (ed) The geology of Egypt. Balkema, Rotterdam, Chapter 20, p 381–389\nNashaat M, Aiolf C, Dalla S, Kamal M (1998) Evaluation and hydrocarbon occurrence in the Plio-Pleistocene succession of the Egyptian Mediterranean Margin. Examples from the Nile Delta basin. E.G.P.C. Exploration seminar, Cairo\nNourEldin N (2002) Nile delta-where is the oil, Egypt, MOC2002, Alex, Egypt\nPointer T, Colnard O, Hemdan S (2008) Pore pressure from seismic velocity prediction in ElManzala offshore, Egypt, MOC 2008, Alex, Egypt\nRizzini A, Vezzani F, Milad G (1978) Stratigraphy and sedimentation of a Neogene Quaternary section in the Nile Delta area. Mar Geol 27:327–348\nSamuel A, Kneller B, Raslan S, Sharp A, Parsons C (2002) Prolific deep-marine slope channels of the Nile Delta, Egypt. AAPG Bull 87(4):541–560\nSelim ESI (2013) Subsurface structural trends of the offshore Nile Delta area, Egypt: evidences from gravity and magnetic data. Environ Earth Sci 68:1015–1032\nSheriff RE (1980) Seismic stratigraphy. IHRDC, Boston\nTari G, Haddou J (2011) Structural analogy between the inverted structures of the moroccan atlas system and the Syrian arc structures of the Eastern Mediterranean, AAPG (April 2011) Search and Discovery paper\nTari G, Hussein H, Novotny B, Hannke K, Kohazy R (2012) Play types of the deep-water Matruh and Herodotus basins, NW Egypt. 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Flotation is the predominant method for the processing of low-grade phosphate ore. The phosphate coarse particles of Kef-Eddur washing plant (southern Tunisia), having a low-grade phosphate, were studied to improve the recovery of phosphate flotation, lost during the washing process. The results of the chemical analysis of phosphate samples showed a grade of 12.51 % P2O5 with a carbonation rate of 2.9 %. Mineralogical study of a sample by X-ray diffraction showed the presence of the following minerals: the carbonate-fluorapatite, calcite, quartz, clinoptilolite (zeolite), and dolomite. Testing of dry grinding showed that the work index is of 10.39 kWh\u002Ft achieving an economical consumption of energy. Milling tests having high values of recovery are accompanied by a raised rate of carbonation, non-tolerable to enter the flotation circuits, dictated an intermediate determination of parameters simultaneously providing considerable recovery while having a tolerable rate of carbonation. Optimizing the operating parameters of flotation (3 scavengers, 320 g\u002Ft ester and 340 g\u002Ft amine), specifications of the best flow-sheet obtained are as follows: crushing 10 mm and ball milling (T = 5.5 min, Cs = 45 %, Rc = 3\u002F1, Vbr = 60 tr\u002Fmin). Attrition released during the first 10 min, second attrition of the same fraction for 20 min and reverse flotation render a grade of 26.80 % P2O5. The results of Kef-Eddur enrichment tests present an increase of 12.51 to 26.80 % P2O5. Application of flotation process is an alternative for this phosphate type.",{"EN":1735},"Enrichment of low-grade phosphate coarse particles by froth-flotation process, at the Kef-Eddur washing plant, Tunisia",{"VOID":1737},"Abdel-Khalek NA (2000) Evaluation of flotation strategies for sedimentary phosphates with siliceous and carbonates gangue. Miner Eng 13(7):789–793\nAbouzied AZM, Negm AT, Elgillani DA (2009) Upgrading of calcareous phosphate ores by flotation: effect of ore characteristics. Int J Miner Process 90:81–89\nAbramov, Al, Onal, G., Atak, S., Celik, M.S., 1993. Mechanism of reverse flotation calcareous phosphate ores. In: El-Shall, H., Moudgil, B.M., Wiegel, R. (Eds.), Beneficiation of phosphate: theory and practice. SME, pp. 281–288.\nAkçaözoğlua K, Fenerb M, Akçaözoğluc S, Öca R (2014) Microstructural examination of the effect of elevated temperature on the concrete containing clinoptilolite. Constr Build Mater 72(15):316–325\nAl-Fariss, T. 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Met & Exp., Inc., Littleton, Colorado, pp. 225–230\nHouot R, Joussement R, Tracez J, Brouard R (1985) Selective flotation of phosphatic ores having a siliceous and\u002For a carbonated gangue. Int J Miner Process 14:245–266\nHsieh SS, Lehr JR (1985) Beneficiation of dolomitic Idaho phosphate rock by the TVA diphosphonic acid depressant process. SME Min Metall Process 2(1):10–13\nKocsis L, Ounis A, Chaabani F, Mohamed-Salah N (2013) Paleoenvironmental conditions and strontium isotope stratigraphy in the Paleogene Gafsa Basin (Tunisia) deduced from geochemical analyses of phosphatic fossils. Int J Earth Sci (Geologische Rundschau) 102:1111–1129\nKocsis L, Ounis A, Baumgartner C, Pirkenseer C, Harding IC, Adatte T, Chaabani F, Mohamd-Neili S (2014) Paleocene–Eocene palaeoenvironmental conditions of the main phosphorite deposits (Chouabine Formation) in the Gafsa Basin, Tunisia. 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A (2003) Characterization of intermetallic Fe–Mn–Si powders produced by casting and mechanical ball milling. Powder Technol 137:139–147\nZheng X, Smith RW (2000) Dolomite depressants in the flotation of apatite and collophane from dolomite. 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Babbou-Abdelmalek",{"id":1771,"sortIndex":123,"researcher":28,"roles":1772,"affiliations":1773,"properties":1780,"displayName":1782,"givenName":28,"familyName":28},"bda15bab-1ef8-4a77-8c3f-787c7133d7ec",[935],[1774],{"id":1747,"sortIndex":32,"affiliation":1775,"properties":28},{"id":1747,"createTime":28,"updateTime":28,"relativeEntities":1776,"slug":28,"properties":1777,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1779,"statistic":28},[],{"title":1778},{"VI":1752},[],{"title":1781},{"VI":1782},"Fredj Chaabani",{"id":1784,"sortIndex":42,"researcher":28,"roles":1785,"affiliations":1786,"properties":1795,"displayName":1797,"givenName":28,"familyName":28},"fbd8fb03-6780-4fa7-9039-4babf2975a3d",[935],[1787],{"id":1788,"sortIndex":32,"affiliation":1789,"properties":28},"f7dc6b94-c1a1-44cc-8da5-73428563dccf",{"id":1788,"createTime":28,"updateTime":28,"relativeEntities":1790,"slug":28,"properties":1791,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1794,"statistic":28},[],{"title":1792},{"VI":1793},"Gafsa Phosphate Company (GPC), Gafsa, Tunisia",[],{"title":1796},{"VI":1797},"Laila Abbassi",{"url":1740,"publisher":1799,"properties":1819},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1800,"slug":872,"properties":1801,"entityType":25,"verifyStatus":882,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1805,"manageAffiliations":1806,"indexDatabases":1807,"url":28,"thumbnailPath":28,"statistic":1814,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1802,"title":1803,"eissn":1804},{"VOID":877},{"EN":879},{"VOID":875},[],[],[1808],{"id":887,"indexDatabase":1809,"url":893,"indexYears":894,"academicFieldIds":28,"indexDatabaseRanking":788},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1810,"label":1811,"description":1812,"key":781,"publicationTags":1813,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],{"impactFactor":32,"impactFactorByYear":1815,"i10Index":123,"i10IndexLast5Year":40,"totalPublication":897,"totalPublicationByYear":1816,"totalCitation":567,"totalCitationByYear":1817,"totalCitationPerPublication":513,"totalCitationPerPublicationByYear":1818,"hindexLast5Year":45,"hindex":45},{"2019":513,"2020":513,"2021":32,"2022":32,"2023":32},{"2008":205,"2009":149,"2010":161,"2011":331,"2012":899,"2013":900,"2014":901,"2015":902,"2016":903,"2017":904,"2018":617,"2019":905,"2020":906,"2021":907,"2022":908,"2023":909,"2024":567},{"2018":278,"2019":40,"2020":127,"2021":145},{"2018":105,"2019":32,"2020":107,"2021":513},{"pages":1820,"volume":1821},{"VOID":1220},{"VOID":1721},"2016-05-21",[783],{"id":1825,"createTime":1826,"updateTime":1827,"relativeEntities":1828,"slug":1829,"properties":1830,"entityType":929,"verifyStatus":26,"verifyTime":1827,"verifyNote":1077,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1839,"fullTextUrl":28,"authors":1840,"publicationType":1031,"publisherRelationship":1934,"citationCount":28,"citationInfo":28,"publishDate":1959,"publishYear":1224,"citationAnalyzeStatus":882,"lastCitationAnalyze":28,"indexDatabases":1960,"openAccess":28,"references":28,"isForceReanalyzing":1061},"0054a58d-ae5c-4135-9a2c-fb0f81119173","2024-01-17T08:57:15.567+00:00","2025-01-12T19:30:32.477+00:00",[],"Investigation-of-natural-background-radiation-of-sediments-in-Rameswaram-Island-Tamil-Nadu-India",{"abstract":1831,"title":1833,"references":1835,"doi":1837},{"EN":1832},"The aim of the study is to assess the natural background radiation in and around Rameswaram Island. In this context, samples were collected to measure the gamma radiations of 238U, 232Th, and 40K using NaI(Tl) detector-based gamma ray spectrometer. The average activity concentrations of 238U, 232Th, and 40K are noted to be well below the world average values. The calculated absorbed dose rate, radium equivalent activity, and hazard index values were below the prescribed limit. The grain size of the sediment was analyzed following Trefethen’s nomenclature, and its correlation with the natural background radioactivity was studied. The sample that contained clay show elevated activity of 40K. The percentage of heavy minerals shows concomitant variation in natural radioactivity, especially in the activity of 238U and 232Th.",{"EN":1834},"Investigation of natural background radiation of sediments in Rameswaram Island, Tamil Nadu, India",{"VOID":1836},"Alappat L, Frechen M, Ramesh R, Tsukamoto S, Srinivasalu S (2011) Evolution of late Holocene coastal dunes in the Cauvery delta region of Tamil Nadu, India. J Asian Earth Sci 42:381–397\nBabu N, Vasumathi N, Bhima Rao R (2009) Recovery of ilmenite and other heavy minerals from Teri Sands (Red Sands) of Tamil Nadu, India. J Miner Mater Charact Eng 8:149–159\nBarnett MO, Jardine PM, Brooks SC (2002) U(VI) adsorption to heterogeneous subsurface media: application of a surface complexation model. Environ Sci Technol 36:937–942\nBaskar K, Sridhar SGD, Sivakumar T, Hussain SM, Maniyarasan S (2015) Temporal variation of physico-chemical parameters and ostracoda population, off Rameswaram, gulf of Mannar, southeast coast of Tamil Nadu, India. J Geol Soc India 86:663–670\nBeretka J, Mathew PJ (1985) Natural radioactivity of Australian building materials, industrial wastes and by-products. Health Phys 48:87–95\nBoboye OA, Nwosu OR (2014) Petrography and geochemical indices of the Lagos lagoon coastal sediments, Dahomey Basin (southwestern Nigeria): sea level change implications. Quat Int 338:14–27\nCharro E, Pardo R, Peña V (2013) Statistical analysis of the spatial distribution of radionuclides in soils around a coal-fired power plant in Spain. J Environ Radioact 124:84–92\nĆujić M, Dragović S, Đorđević M, Dragović R, Gajić B, Miljanić Š (2015) Radionuclides in the soil around the largest coal-fired power plant in Serbia: radiological hazard, relationship with soil characteristics and spatial distribution. Environ Sci Pollut Res 22:10317–10330\nCurrie LA (1968) Limits for qualitative detection and quantitative determination. Application to radiochemistry. Anal Chem 40:586–593\nDalai TK, Rengarajan R, Patel PP (2004) Sediment geochemistry of the Yamuna River system in the Himalaya: implications to weathering and transport. Geochem J 38:441–453\nDalvi AA, Kumar SD, Reddy AVR (2014) A site-specific study on the measurement of sorption coefficients for radionuclides. Int J Environ Sci Technol 11:617–622\nDerin M, Vijayagopal P, Venkatraman B, Chaubey RC, Gopinathan A (2012) Radionuclides and radiation indices of high background radiation area in Chavara-Neendakara placer deposits (Kerala, India). PLoS One 7:e50468\nEchevarria G, Sheppard MI, Morel J (2001) Effect of pH on the sorption of uranium in soils. J Environ Radioact 53:257–264\nEl-Arabi AM, Abbady AGE, Hussein AS (2006) Gamma-ray measurements of natural radioactivity in sedimentary rocks from Egypt. Nucl Sci Tech 17:123–128\nEl-Gamal A, Nasr S, El-Taher A (2007) Study of the spatial distribution of natural radioactivity in the upper Egypt Nile River sediments. Radiat Meas 42:457–465\nErnst WG (2012) Overview of naturally occurring earth materials and human health concerns. J Asian Earth Sci 59:108–126\nFox PM, Davis JA, Zachara JM (2006) The effect of calcium on aqueous uranium(VI) speciation and adsorption to ferrihydrite and quartz. Geochim Cosmochim Acta 70:1379–1387\nGowthaman R, Kumar VS, Dwarakish GS, Mohan SS, Singh J, Kumar KA (2013) Waves in gulf of Mannar and Palk Bay around Dhanushkodi, Tamil Nadu. Curr Sci 104:1431–1435\nGSI (2006) Geological Survey of India Miscellaneous publication no. 30 (Part IV, Tamil Nadu and Pondicherry), in: http:\u002F\u002Fwww.portal.gsi.gov.in\u002FgsiImages\u002Finformation\u002Fmisc_pub_30_tamilnadu_2006_wm.pdf\nGuagliardi I, Buttafuoco G, Apollaro C, Bloise A, De Rosa R, Cicchella D (2013) Using gamma-ray spectrometry and Geostatistics for assessing geochemical behaviour of radioactive elements in the lese catchment (southern Italy). Int J Environ Res 7:645–658\nGuagliardi I, Rovella N, Apollaro C, Bloise A, De Rosa R, Scarciglia F, Buttafuoco G (2016a) Effects of source rocks, soil features and climate on natural gamma radioactivity in the Crati valley (Calabria, southern Italy). Chemosphere 150:97–108\nGuagliardi I, Rovella N, Apollaro C, Bloise A, Rosa RD, Scarciglia F, Buttafuoco G (2016b) Modelling seasonal variations of natural radioactivity in soils: a case study in southern Italy. J Earth Syst Sci 125:1569–1578\nHejl AM, Ottmar RD, Timothy Jannik G, Eddy TP, Rathbun SL, Commodore AA, Pearce JL, Naeher LP (2013) Radionuclide activity concentrations in forest surface fuels at the Savannah River site. J Environ Manag 115:217–226\nICRP (1991) Annals of ICRP 1990 Recommendations of the International Commission on Radiological Protection. ICRP Publication, Pergamon: UK No. 60\nJolyon HH, Steven LS, Andrzej W, Mehdi S, Werner B, Elisabeth C, Dominique L, Margot T, Isamu H (2009) Human exposure to high natural background radiation: what can it teach us about radiation risks? J Radiol Prot 29:A29\nKrishna Kumar S, Chandrasekar N, Seralathan P, Godson P, Magesh NS (2012) Hydrogeochemical study of shallow carbonate aquifers, Rameswaram Island, India. Environ Monit Assess 184:4127–4138\nKrishnamoorthy N, Mullainathan S, Mehra R, Chaparro MAE, Chaparro MAE (2013) Radiation impact assessment of naturally occurring radionuclides and magnetic mineral studies of Bharathapuzha river sediments, South India. Environ Earth Sci 71:3593–3604\nKrishnamoorthy N, Mullainathan S, Mehra R, Chaparro MAE, Chaparro MAE (2014) Radiation impact assessment of naturally occurring radionuclides and magnetic mineral studies of Bharathapuzha river sediments, South India. Environ Earth Sci 71:3593–3604\nKücükömeroglu B, Kurnaz A, Keser R, Korkmaz F, Okumusoglu NT, Karahan G, Sen C, Cevik U (2008) Radioactivity in sediments and gross alpha–beta activities in surface water of Fırtına River, Turkey. Environ Geol 55:1483–1491\nLigero RA, Ramos-Lerate I, Barrera M, Casas-Ruiz M (2001) Relationships between sea-bed radionuclide activities and some sedimentological variables. J Environ Radioact 57:7–19\nLivshits TS (2009) Stability of artificial ferrite garnets with actinides and lanthanoids in water solutions. Geol Ore Deposits 50:470–481\nMc Laughlin JP (2015) Some characteristics and effects of natural radiation. Radiat Prot Dosim 167:2–7\nMelson Nathan H, Haliena Brian P, Kaplan Daniel I, Barnett Mark O (2012) Adsorption of tetravalent thorium by geomedia. Radiochim Acta 100:827–832\nMurphy RJ, Lenhart JJ, Honeyman BD (1999) The sorption of thorium (IV) and uranium (VI) to hematite in the presence of natural organic matter. Colloids Surf A Physicochem Eng Asp 157:47–62\nNatesan U (2009) Shoreline Dynamics of Dhanushkodi, Rameswaram Using Gis. In: Advances in Water Resources and Hydraulic Engineering: Proceedings of 16th IAHR-APD Congress and 3rd Symposium of IAHR-ISHS. Springer Berlin Heidelberg, Berlin, Heidelberg, pp 1294–1298\nÖrgün Y, Altınsoy N, Şahin SY, Güngör Y, Gültekin AH, Karahan G, Karacık Z (2007) Natural and anthropogenic radionuclides in rocks and beach sands from Ezine region (Çanakkale), Western Anatolia, Turkey. Appl Radiat Isot 65:739–747\nRahman SU, Matiullah, Malik F, Rafique M, Anwar J, Ziafat M, Jabbar A (2011) Measurement of naturally occurring\u002Ffallout radioactive elements and assessment of annual effective dose in soil samples collected from four districts of the Punjab Province, Pakistan. J Radioanal Nucl Chem 287:647–655\nRamasamy V, Dheenathayalu M, Ravisankar R, Ponnusamy V, Rajamanickkam GV, Sahayam D, Meenakshisundram V, Gajendran V (2004) Natural radioactivity measurements in beach-rock samples of south-east coast of Tamilnadu, India. Radiat Prot Dosim 111:229–235\nRamasamy V, Suresh G, Meenakshisundaram V, Ponnusamy V (2011) Horizontal and vertical characterization of radionuclides and minerals in river sediments. Appl Radiat Isot 69:184–195\nRamasamy V, Sundarrajan M, Paramasivam K, Meenakshisundaram V, Suresh G (2013) Assessment of spatial distribution and radiological hazardous nature of radionuclides in high background radiation area, Kerala, India. Appl Radiat Isot 73:21–31\nRamasamy V, Sundarrajan M, Suresh G, Paramasivam K, Meenakshisundaram V (2014) Role of light and heavy minerals on natural radioactivity level of high background radiation area, Kerala, India. Appl Radiat Isot 85:1–10\nRamesh R, Nammalwar P, Gowri VS (2008) Database on Coastal Information Of Tamilnadu. Institute for Ocean Management, Anna University, Chennai - 600 025, Environmental Information System (Envis) Centre, Department Of Environment, Government of Tamilnadu, Chennai – 600 015, in: http:\u002F\u002Ftnenvis.nic.in\u002Ftnenvis_old\u002Fcoastal%20data.pdf\nRodríguez-Barroso MR, García-Morales JL, Coello Oviedo MD, Quiroga Alonso JM (2010) An assessment of heavy metal contamination in surface sediment using statistical analysis. Environ Monit Assess 163:489–501\nRojo I, Seco F, Rovira M, Giménez J, Cervantes G, Martí V, de Pablo J (2009) Thorium sorption onto magnetite and ferrihydrite in acidic conditions. J Nucl Mater 385:474–478\nSartandel SJ, Bara SV, Chinnaesakki S, Tripathi RM, Puranik VD (2012) Measurement of naturally occurring radioactive materials (NORM) in beach sand minerals using HPGe based gamma-ray spectrometry. J Radioanal Nucl Chem 294:447–451\nSelvasekarapandian S, Sivakumar R, Manikandan NM, Meenakshisundaram V, Raghunath VM, Gajendran V (2000) Natural radionuclide distribution in soils of Gudalore, India. Appl Radiat Isot 52:299–306\nSingh HN, Shanker D, Neelakandan VN, Singh VP (2007) Distribution patterns of natural radioactivity and delineation of anomalous radioactive zones using in situ radiation observations in southern Tamil Nadu, India. J Hazard Mater 141:264–272\nSulieman M, Ibrahim I, Elfaki J, Dafa-Allah M (2015) Origin and distribution of heavy minerals in the surficial and subsurficial sediments of the alluvial Nile River terraces. Open J Soil Sci 5:299–310\nSuresh G, Ramasamy V, Meenakshisundaram V, Venkatachalapathy R, Ponnusamy V (2011) A relationship between the natural radioactivity and mineralogical composition of the Ponnaiyar river sediments, India. J Environ Radioact 102:370–377\nTrefethen JM (1950) Classification of sediments. Am J Sci 248:55–62\nUNSCEAR (2000) United Nations Scientific Committee on the Effect of Atomic Radiation, United Nations, New York http:\u002F\u002Fwww.unscear.org\u002Fdocs\u002Fpublications\u002F2000\u002FUNSCEAR_2000_Annex-B.pdf\nUNSCEAR (2008) United Nations Scientific Committee on the Effect of Atomic Radiation, United Nations, New York http:\u002F\u002Fwww.unscear.org\u002Fdocs\u002Fpublications\u002F2008\u002FUNSCEAR_2008_Annex-B-CORR.pdf\nXinwei L, Xiaolan Z (2006) Measurement of natural radioactivity in sand samples collected from the Baoji Weihe Sands park, China. Environ Geol 50:977–982",{"VOID":1838},"10.1007\u002Fs12517-018-4125-y","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs12517-018-4125-y",[1841,1865,1878,1891,1906,1921],{"id":1842,"sortIndex":32,"researcher":28,"roles":1843,"affiliations":1844,"properties":1862,"displayName":1864,"givenName":28,"familyName":28},"bd7568b3-665d-499e-b495-8185d92025a0",[935],[1845,1853],{"id":1846,"sortIndex":32,"affiliation":1847,"properties":28},"55e6b693-262d-43e2-9755-e6684d368aa7",{"id":1846,"createTime":28,"updateTime":28,"relativeEntities":1848,"slug":28,"properties":1849,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1852,"statistic":28},[],{"title":1850},{"VI":1851},"Department of Nuclear Physics, Guindy Campus, University of Madras, Chennai, India",[],{"id":1854,"sortIndex":40,"affiliation":1855,"properties":1861},"25fe4331-ce20-4239-a4ba-19fb973c66c8",{"id":1854,"createTime":28,"updateTime":28,"relativeEntities":1856,"slug":28,"properties":1857,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1860,"statistic":28},[],{"title":1858},{"VI":1859},"Health, Safety and Environment Group, Indira Gandhi Centre for Atomic Research, Kalpakkam, India",[],{},{"title":1863},{"VI":1864},"I. Inigo Valan",{"id":1866,"sortIndex":40,"researcher":28,"roles":1867,"affiliations":1868,"properties":1875,"displayName":1877,"givenName":28,"familyName":28},"cf01249c-12e5-476f-bac9-7c9dc98a1a53",[935],[1869],{"id":1854,"sortIndex":32,"affiliation":1870,"properties":28},{"id":1854,"createTime":28,"updateTime":28,"relativeEntities":1871,"slug":28,"properties":1872,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1874,"statistic":28},[],{"title":1873},{"VI":1859},[],{"title":1876},{"VI":1877},"I. Vijayalakshmi",{"id":1879,"sortIndex":123,"researcher":28,"roles":1880,"affiliations":1881,"properties":1888,"displayName":1890,"givenName":28,"familyName":28},"b5d3ccc2-465d-497a-b9c9-6e42ed186c26",[935],[1882],{"id":1854,"sortIndex":32,"affiliation":1883,"properties":28},{"id":1854,"createTime":28,"updateTime":28,"relativeEntities":1884,"slug":28,"properties":1885,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1887,"statistic":28},[],{"title":1886},{"VI":1859},[],{"title":1889},{"VI":1890},"R. Mathiyarasu",{"id":1892,"sortIndex":42,"researcher":28,"roles":1893,"affiliations":1894,"properties":1903,"displayName":1905,"givenName":28,"familyName":28},"930bc0a1-85da-4484-9104-07ff2e524af6",[935],[1895],{"id":1896,"sortIndex":32,"affiliation":1897,"properties":28},"d885491e-04f6-4303-828f-8f98b7a3a940",{"id":1896,"createTime":28,"updateTime":28,"relativeEntities":1898,"slug":28,"properties":1899,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1902,"statistic":28},[],{"title":1900},{"VI":1901},"Department of Applied Geology, Guindy Campus, University of Madras, Chennai, India",[],{"title":1904},{"VI":1905},"S. G. D. Sridhar",{"id":1907,"sortIndex":45,"researcher":28,"roles":1908,"affiliations":1909,"properties":1918,"displayName":1920,"givenName":28,"familyName":28},"783a14c1-0902-4734-9240-c446f4507f85",[935],[1910],{"id":1911,"sortIndex":32,"affiliation":1912,"properties":28},"de91032f-01f1-4aa8-9295-b8fb959a180a",{"id":1911,"createTime":28,"updateTime":28,"relativeEntities":1913,"slug":28,"properties":1914,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1917,"statistic":28},[],{"title":1915},{"VI":1916},"Department of Inorganic Chemistry, Guindy Campus, University of Madras, Chennai, India",[],{"title":1919},{"VI":1920},"V. Narayanan",{"id":1922,"sortIndex":46,"researcher":28,"roles":1923,"affiliations":1924,"properties":1931,"displayName":1933,"givenName":28,"familyName":28},"c6f051aa-baf9-49e3-86af-af1ffcbc09fb",[935],[1925],{"id":1846,"sortIndex":32,"affiliation":1926,"properties":28},{"id":1846,"createTime":28,"updateTime":28,"relativeEntities":1927,"slug":28,"properties":1928,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1930,"statistic":28},[],{"title":1929},{"VI":1851},[],{"title":1932},{"VI":1933},"A. Stephen",{"url":1839,"publisher":1935,"properties":1955},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1936,"slug":872,"properties":1937,"entityType":25,"verifyStatus":882,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1941,"manageAffiliations":1942,"indexDatabases":1943,"url":28,"thumbnailPath":28,"statistic":1950,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1938,"title":1939,"eissn":1940},{"VOID":877},{"EN":879},{"VOID":875},[],[],[1944],{"id":887,"indexDatabase":1945,"url":893,"indexYears":894,"academicFieldIds":28,"indexDatabaseRanking":788},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1946,"label":1947,"description":1948,"key":781,"publicationTags":1949,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],{"impactFactor":32,"impactFactorByYear":1951,"i10Index":123,"i10IndexLast5Year":40,"totalPublication":897,"totalPublicationByYear":1952,"totalCitation":567,"totalCitationByYear":1953,"totalCitationPerPublication":513,"totalCitationPerPublicationByYear":1954,"hindexLast5Year":45,"hindex":45},{"2019":513,"2020":513,"2021":32,"2022":32,"2023":32},{"2008":205,"2009":149,"2010":161,"2011":331,"2012":899,"2013":900,"2014":901,"2015":902,"2016":903,"2017":904,"2018":617,"2019":905,"2020":906,"2021":907,"2022":908,"2023":909,"2024":567},{"2018":278,"2019":40,"2020":127,"2021":145},{"2018":105,"2019":32,"2020":107,"2021":513},{"pages":1956,"volume":1958},{"VOID":1957},"1-13",{"VOID":1222},"2018-12-08",[783],{"id":1962,"createTime":1963,"updateTime":1964,"relativeEntities":1965,"slug":1966,"properties":1967,"entityType":929,"verifyStatus":26,"verifyTime":1964,"verifyNote":1077,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1976,"fullTextUrl":28,"authors":1977,"publicationType":1031,"publisherRelationship":2028,"citationCount":28,"citationInfo":28,"publishDate":2052,"publishYear":1456,"citationAnalyzeStatus":882,"lastCitationAnalyze":28,"indexDatabases":2053,"openAccess":28,"references":28,"isForceReanalyzing":1061},"007c2caf-e75e-438d-a784-f1a4ac9e4c83","2024-01-15T18:23:52.023+00:00","2025-02-04T02:21:06.815+00:00",[],"Land-cover-classification-and-analysis-of-change-using-machine-learning-classifiers-and-multi-temporal-remote-sensing-imagery",{"abstract":1968,"title":1970,"references":1972,"doi":1974},{"EN":1969},"Frequent human activity and rapid urbanization have led to an assortment of environmental issues. Monitoring land-cover change is critical to efficient environmental management and urban planning. The current study had two objectives. The first was to compare pixel-based random forest (RF) and decision tree (DT) classifier methods and a support vector machine (SVM) algorithm both in pixel-based and object-based approaches for classification of land-cover in a heterogeneous landscape for 2010. The second was to examine spatio-temporal land-cover change over the last two decades (1990–2010) using Landsat data. This study found that the object-based SVM classifier is the most accurate with an overall classification accuracy of 93.54% and a kappa value of 0.88. A post-classification change detection algorithm was used to determine the trend of change between land-cover classes. The most significant change from 1990 to 2010 was caused by the expansion of built-up areas. In addition to the net changes, the rate of annual change for each phenomenon was calculated to obtain a better understanding of the process of change. Between 1990 and 2010, an average of 4.53% of lands turned to the built-up annually and there was an annual decrease of about 0.81% in natural land. If the current trend of change continues, regardless of the actions of sustainable development, drastic declines in natural areas will ensue. The results of this study can be a valuable baseline for land-cover managers in the region to better understand the current situation and adopt appropriate strategies for management of land-cover.",{"EN":1971},"Land-cover classification and analysis of change using machine-learning classifiers and multi-temporal remote sensing imagery",{"VOID":1973},"Adam E, Mutanga O, Abdel-Rahman EM, Ismail R (2014) Estimating standing biomass in papyrus (Cyperus papyrus L.) swamp: exploratory of in situ hyperspectral indices and random forest regression. Int J Remote Sens 35:693–714. doi:10.1080\u002F01431161.2013.870676\nAngell DL, McClaran MP (2001) Long-term influences of livestock management and a non-native grass on grass dynamics in the desert grassland. J Arid Environ 49:507–520. doi:10.1006\u002Fjare.2001.0811\nBajocco S, Angelis A, Perini L, Ferrara A, Salvati L (2012) The impact of land use\u002Fland cover changes on land degradation dynamics. A Mediterranean Case Study Environmental Management 49:980–989. doi:10.1007\u002Fs00267-012-9831-8\nBenz UC, Hofmann P, Willhauck G, Lingenfelder I, Heynen M (2004) Multi-resolution, object-oriented fuzzy analysis of remote sensing data for GIS-ready information ISPRS. Journal of Photogrammetry and Remote Sensing 58:239–258. doi:10.1016\u002Fj.isprsjprs.2003.10.002\nBlaschke T (2010) Object based image analysis for remote sensing ISPRS. Journal of Photogrammetry and Remote Sensing 65:2–16. doi:10.1016\u002Fj.isprsjprs.2009.06.004\nBreiman L (2001) Random Forests. 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