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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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Handbook of Earthquake and Engineering Seismology",{"VOID":960},"10.1007\u002Fs10950-005-9000-0","PUBLICATION","Auto Verify","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10950-005-9000-0",[965],{"id":966,"sortIndex":32,"researcher":28,"roles":967,"affiliations":969,"properties":978,"displayName":980,"givenName":28,"familyName":28},"c784d1b5-a6b9-4cd2-bf9d-818a388e18c6",[968],"AUTHOR",[970],{"id":971,"sortIndex":32,"affiliation":972,"properties":28},"18eb0f00-0eee-4b24-b99e-032531e918be",{"id":971,"createTime":28,"updateTime":28,"relativeEntities":973,"slug":28,"properties":974,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":977,"statistic":28},[],{"title":975},{"VI":976},"Institut für Geophysik, Universität Hamburg, Hamburg, Germany",[],{"title":979},{"VI":980},"Carsten 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Fresnel volume ray theory is more suitable for handling real seismic propagation problems because the traveltime depends not only on the velocity distribution along a traditional geometric ray but also on the velocity distribution within a vicinal region (referred to as first Fresnel volume, abbreviated as FFV) which embraces the geometric ray. In this study, we used an exact solution to calculate multi-phase FFV rays for both 2-D and 3-D cases and introduced a normalized coefficient to account for different contributions inside the FFV ray on the traveltimes. Furthermore, we draw a new formula to calculate the partial traveltime derivatives with respective to the velocity variations and depth changes of the reflectors and finally present a simultaneous inversion method for updating both velocity field and reflector geometry by using these multi-phase FFV rays for both in 2-D and 3-D cases. Using synthetic data examples, we compare the reconstructions of the velocity field and the reflector geometry using the FFV ray tomographic methods and the traditional ray tomography approaches. The simulated inversion results for both 2-D and 3-D cases show that the FFV ray tomographic method is advantageous over the traditional ray tomography method, especially when the ray density is relatively low. The other advantage for the FFV ray tomography method is that it can capture the coarse velocity structure and reflector geometry by starting with a low-frequency data set and then map the fine velocity structure and the detailed reflector geometry by using a high-frequency data set.",{"EN":1047},"2D\u002F3D multi-phase Fresnel volume rays and applications to simultaneously update both velocity model and reflector geometry",{"VOID":1049},"Bai CY, Greenhalgh SA (2005) 3-D non-linear travel time tomography: imaging high contrast velocity anomalies. Pure Appl Geophys 162:2029–2049\nBai CY, Huang GJ, Zhao R (2010) 2D\u002F3D irregular shortest-path ray tracing for multiple arrivals and its applications. Geophys J Int 183:1596–1612\nBai CY, Li XL, Tang XP (2011) Seismic wavefront evolution of multiply reflected, transmitted and converted phases in 2D\u002F3D triangular cell model. J Seismol 15:637–652\nBai CY, Li XL, Wang QL, Peng JB (2012) Multiple arrival tracking within irregular triangular or tetrahedron cell model. J Geophys Eng 9:29–38\nBai CY, Wang X, Wang CX (2013) Comparison wavefield simulation between the first- and the second-order separated wave equations through a high-order staggered-grid finite difference method. Earthq Sci 26(2):83–98\nBai CY, Li XW, Huang GJ, Greenhalgh S (2014a) Simultaneous inversion for velocity and reflector geometry using multi-phase Fresnel volume rays. Pure Appl Geophys 171:1089–1105\nBai CY, Huang GJ, Li XW, Greenhalgh S (2014b) 3D simultaneous traveltime inversion for velocity structure, hypocenter locations and reflector geometry using multiple classes of arrivals. Pure Appl Geophys. doi:10.1007\u002Fs00024-014-0945-1\nČervený V, Soares JEP (1992) Fresnel volume ray tracing. Geophysics 57:902–915\nHuang GJ, Bai CY, Zhu DL, Greenhalgh S (2012) 2D\u002F3D seismic simultaneous inversion for velocity model and interface geometry using multiple classes of arrivals. Bull Seismol Soc Am 102:790–801\nHusen S, Kissling E (2001) Local earthquake tomography between rays and waves: fat ray tomography. Phys Earth Planet Inter 123:129–149\nKennett BLN, Sambridge M (1998) Inversion for multiple parameter classes. Geophys J Int 135:304–306\nLuo Y, Schuster GT (1991) Wave-equation traveltime inversion. Geophysics 56:645–653\nPratt RG, Goulty NR (1991) Combining wave-equation imaging with traveltime tomography to form high-resolution images from crosshole data. Geophysics 56:208–224\nSheng J, Leed A, Buddensiek M, Schuster GT (2006) Early arrival waveform tomography on near-surface refraction data. Geophysics 71:47–57\nThurber C, Eberhart-Phillips D (1999) Local earthquake tomography with flexible gridding. Comput Geosci 25:809–818\nVasco DW, Peterson JE, Majer EL (1995) Beyond ray tomography: wave paths and Fresnel volumes. Geophysics 60:1790–1804\nWielandt E., 1987. On the validity of the ray approximation for interpreting delay time. In: Seismic tomography, edited by Nolet G., Redel Publishing Company\nZhou B, Greenhalgh SA, Sinadinovski C (1992) Iterative algorithm for the damped minimum norm, least-squares and constrained problem in seismic tomography. Explor Geophys 23:497–505",{"VOID":1051},"10.1007\u002Fs10950-015-9484-1","http:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs10950-015-9484-1",[1054,1078,1091],{"id":1055,"sortIndex":32,"researcher":28,"roles":1056,"affiliations":1057,"properties":1075,"displayName":1077,"givenName":28,"familyName":28},"e10a4d77-ecbb-48f8-bd27-6a76518bac71",[968],[1058,1066],{"id":1059,"sortIndex":32,"affiliation":1060,"properties":28},"7539968d-a2bd-4dae-863d-64b2151a052d",{"id":1059,"createTime":28,"updateTime":28,"relativeEntities":1061,"slug":28,"properties":1062,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1065,"statistic":28},[],{"title":1063},{"VI":1064},"Department of Geophysics, College of Geology Engineering and Geomatics, Chang’an University, Xi’an, 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School of Earth Sciences and Engineering, Hohai University, Nanjing, China",[],{},{"title":1111},{"VI":1112},"Guo-jiao Huang",{"url":1052,"publisher":1114,"properties":1160},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1115,"slug":872,"properties":1116,"entityType":25,"verifyStatus":880,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1120,"manageAffiliations":1129,"indexDatabases":1140,"url":940,"thumbnailPath":28,"statistic":1155,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1117,"title":1118,"eissn":1119},{"VOID":875},{"EN":877},{"VOID":879},[1121,1125],{"id":883,"createTime":28,"updateTime":28,"relativeEntities":1122,"label":1123,"description":1124,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":886},{},{"id":889,"createTime":28,"updateTime":28,"relativeEntities":1126,"label":1127,"description":1128,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":892},{},[1130,1135],{"id":896,"createTime":28,"updateTime":28,"relativeEntities":1131,"slug":28,"properties":1132,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1134,"statistic":28},[],{"title":1133},{"EN":900},[902],{"id":904,"createTime":28,"updateTime":28,"relativeEntities":1136,"slug":28,"properties":1137,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1139,"statistic":28},[],{"title":1138},{"EN":908},[],[1141,1148],{"id":912,"indexDatabase":1142,"url":924,"indexYears":28,"academicFieldIds":1147,"indexDatabaseRanking":28},{"id":914,"createTime":28,"updateTime":28,"relativeEntities":1143,"label":1144,"description":1145,"key":921,"publicationTags":1146,"standard":28},[],{"EN":917,"VI":917},{"EN":919,"VI":920},[923,813],[926],{"id":928,"indexDatabase":1149,"url":934,"indexYears":935,"academicFieldIds":1154,"indexDatabaseRanking":939},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1150,"label":1151,"description":1152,"key":781,"publicationTags":1153,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[937,938],{"impactFactor":32,"impactFactorByYear":1156,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":279,"totalPublicationByYear":1157,"totalCitation":32,"totalCitationByYear":1158,"totalCitationPerPublication":32,"totalCitationPerPublicationByYear":1159,"hindexLast5Year":32,"hindex":32},{},{"1997":48,"1998":42,"1999":46,"2000":48,"2001":49,"2002":46,"2003":40,"2005":40,"2006":40,"2007":40,"2008":40,"2012":123,"2013":40,"2016":123,"2018":123,"2020":40,"2022":42},{},{},{"pages":1161,"volume":1163},{"VOID":1162},"607-621",{"VOID":1164},"19","2015-02-03",2015,[939,923],{"id":1169,"createTime":1170,"updateTime":1171,"relativeEntities":1172,"slug":1173,"properties":1174,"entityType":961,"verifyStatus":26,"verifyTime":1171,"verifyNote":962,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1183,"fullTextUrl":28,"authors":1184,"publicationType":981,"publisherRelationship":1222,"citationCount":28,"citationInfo":28,"publishDate":1274,"publishYear":1275,"citationAnalyzeStatus":880,"lastCitationAnalyze":28,"indexDatabases":1276,"openAccess":28,"references":28,"isForceReanalyzing":1037},"00c68baa-6902-4833-915f-ff5234bf4427","2024-01-04T12:44:03.566+00:00","2024-12-28T21:13:10.851+00:00",[],"Strength-and-ductility-level-earthquake-design-for-Gulf-of-Suez-oil-platforms",{"abstract":1175,"title":1177,"references":1179,"doi":1181},{"EN":1176},"Gulf of Suez area which characterized by a moderate seismic activity is consider as a very important area in Egypt. Nearly 75% of the national oil production is covered from this area. Seismic hazard (both probabilistic and deterministic) was carried out to study the possibility of earthquake damage in the area; a new seismic model was used taking into account the seismo-tectonic framework of the region. The hazard calculations utilized at strength and ductility level periods at the whole area of the Gulf of Suez. Fundamentally, the hazard calculations were performed at bedrock conditions, and the spectrum was estimated over the period range of 0.001–12 s. At Abou Zeniama area, where many oil platforms exist, the hazard was calculated at the sea floor, at depth 4.7 m and at depth 26.0 m. The maximum spectral accelerations at strength level earthquakes (SLEs) are found to be 0.260 (g), 0.203 (g), and 0.156 (g) for 90.48% chance, of non-exceedance in 50 years (return period 500 year) at sea floor, at depth 4.7 m and at depth 26 m, respectively. While the ductility level earthquake (DLE) are found to be 0.30 (g), 0.23 (g), and 0.18 (g) for 95.12% chance of non-exceedance in 50 years (return period 1000 year) at sea floor, at depth 4.7 m, and at depth 26 m, respectively. The deterministic hazard calculation was estimated at 50th and 84th percentile levels for the median peak ground acceleration. The study target initiated from the importance of studying the seismic hazard, SLE, and DLE in the area which contain most of the Egyptian oil industry with many off shore platforms.",{"EN":1178},"Strength and ductility level earthquake design for Gulf of Suez oil platforms",{"VOID":1180},"Abd el-aal AK (2010a) Modeling of seismic hazard at the northeastern part of greater Cairo metropolitan area. Egypt. J Geophys Eng 7:75–90. https:\u002F\u002Fdoi.org\u002F10.1088\u002F1742-2132\u002F7\u002F1\u002F007\nAbd el-aal AK (2010b) Ground motion prediction from nearest seismogenic zones in and around greater Cairo area, Egypt. Nat Hazards Earth Syst Sci 10:1495–1511. https:\u002F\u002Fdoi.org\u002F10.5194\u002Fnhess-10-1495-2010\nAbd el-aal AK, Kamal H, Abdelhay M, Elzahaby K (2015) Probabilistic and stochastic seismic hazard assessment for wind turbine tower sites in Zafarana Wind Farm, Gulf of Suez, Egypt. Bull Eng Geol Environ 74:1225–1241. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs10064-015-0717-x\nAbd el-aal AK, Yagi Y, Kamal H, Abdelrahman K (2016) Implementation of integrated multi-channel analysis of surface waves and waveform inversion techniques for seismic hazard estimation. Arab J Geosci 9:322. https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs12517-016-2329-6\nAbdel hafiez HE (2015) Estimating the magnitude of completeness for assessing the quality of earthquake catalogue of the ENSN, Egypt. Arab J Geosci 8(11):9315–9323\nAbou Elenean, K. M., 1997. Seismotectonics of Egypt in relation to the Mediterranean and Red Seas tectonics. Ph. D. thesis Ain Shams Univ., Egypt\nAbou Elenean KM (2007) Focal mechanisms of small and moderate size earthquakes recorded by the Egyptian national seismic network (ensn), Egypt. NRIAG J Geophys 6(1):117 ñn151\nAbrahamson, N. A. 2006. Seismic hazard assessment: problems with current practice and future development, first European conference on earthquake engineering and seismology, Geneva, , 3–8 September 2006,17 pp.\nAbrahamson NA, Silva WJ (1997) Empirical response spectral attenuation relations for shallow crustal earthquakes. Seismol Res Lett 68:94–127\nAmbraseys NN, Melville CP, Adams RD (1994) The seismicity of Egypt, Arabia and the Red Sea, a historical review, King Abdul Aziz City for Science and Technology. Cambridge Univ. Press, Amsterdam, p 137\nAPI (1991), Recommendations for Planning, Designing and Constructing Fixed Offshore Platforms, API Recommended Practice 2A (RP 2A), 19th Edition, August I, American Petroleum Institute\nCampbell KW, Bozorgnia Y (2003) Updated near-source ground motion (attenuation) relations for the horizontal and vertical components of peak ground acceleration and acceleration response spectra. Bull Seismol Soc Am 93(1):314–331\nCornell CA (1968) Engineering seismic risk analysis. Bull Seismol Soc Am 18:1583–1606\nCotton F, Scherbaum F, Mommer JJ, Bungum H (2006) Criteria for selecting and adjusting ground –motion models for specific target application: application to Central Europe and rock sites. J Seismol 10:137–156\nDeif A, Abou Elenean K, El Hadidy M, Tealeb A, Mohamed A (2009) Probabilistic seismic hazard maps for Sinai Peninsula, Egypt. J Geophys Eng 6(3):288–e297\nDeif A, Hamed H, Ibrahim HA, Abou Elenean K, El-Amin E (2011) Seismic hazard assessment in Aswan Egypt. J Geophys Eng 8(2011):531–548\nDomenico Giardini, The global seismic Hazard assessment program (GSHAP) -1992\u002F1999 ANNALI DI GEOFISICA, VOL 42, N. 6, December 1999\nEl-Sayed A, Wahlstroem R, Kulhanek O (1994) Seismic Hazard of Egypt. Nat Hazards 10:247–e259\nFugro Report No: N4490\u002F0.1. (n.d.) Geotechnical data and spudcan penetration assessments, Jack-up Rig Comet Muzhil 1 Exploration Well location Gulf of Suez, Egypt\nGutenberg B, Richter CF (1944) Seismicity and associated phenomena. Princeton University Press, Princeton, NJ, p 310\nKijko A, Graham G (1999) Parametric-historic procedure for probabilistic seismic hazard analysis part ii: assessment of seismic hazard at specified site. Pure Appl Geophys 154(1):1–22\nKijko A (2004) Estimation of the maximum earthquake magnitude, Mmax. Pure Appl Geophys 161:1655–1681\nKijko A, Singh M (2011) Statistical tools for maximum possible earthquake magnitude estimation. Acta Geophys 59:674–700\nMaamoun M, Megahed A, Allam A (1984) Seismicity of Egypt. Bull HIAG 4:109–126\nMc Guire R K 1976 : FORTRAN computer program for seismic risk analysis US Geological Survey Open-File Report 76–67\nMeshref, W. M., (1990): Tectonic framework of global tectonics. In: The Geology of Egypt. (Ed. R. Said, 1990)\nMostafa SI, Abd el-aal AK, El-Eraki M (2018) Multi scenario seismic hazard assessment for Egypt. J Seismol 22(3):669–696\nReiter L (1990) Earthquake hazards analysis: issues and insights. Columbia University Press, New York\nRobson DS, Whitlock JH (1964) Estimation of a truncation point. Biometrika 51:33–39\nRydelek PA, Sacks IS (2003) Comment on “minimum magnitude of completeness in earthquake catalogs: examples from Alaska, the western United States, and Japan”, by Stefan Wiemer and max Wyss. Bull Seismol Soc Am 93(4):1862–1867\nSaid R (1962) The geology of Egypt. Amesterdam, New York 370p\nStepp JC (1972) Analysis of completeness of the earthquake sample in the Puget Sound area and its effect on statistical estimates of earthquake hazard proc. In: 2nd Int Conf on microzonation 897–910\nWiemer S, Wyss M (2000) Minimum magnitude of completeness reporting in earthquake catalogs: examples from Alaska, the Western United States, and Japan. Bull Seismol Soc Am 90(4):859–869\nWiemer S, Wyss M (2003) Reply to “comment on minimum magnitude of completeness in earthquake catalogs: example from Alaska, the western United States, and Japan’, by Stefan Wiemer and max Wyss”, by Paul a Rydelek and IS sacks. 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Thisvalue is significantly larger than expected on thebasis of the usual regressions with magnitude anddistance. A broad-band amplification up to a factor of10 was consistently estimated in previous papers,using both weak and strong motion data recorded at theaccelerograph site during local moderate earthquakes.To study the cause of this amplification we deployedsix seismologic stations across the tectonic contactbetween the Ceno-Mesozoic limestone and the Mesozoicmarly sandstone where the accelerograph is installed.Seismograms of 21 shallow aftershocks in the magnituderange from 2.2 to 4.0 and a subcrustal Mw = 5.3event are analysed. Regardless of epicentre location,waveforms show a large complexity in an approximately200 m wide band adjacent to the tectonic contact. Thisis interpreted as the effect of trapped waves in thehighly fractured, lower velocity materials within thefault zone.",{"EN":1286},"Large amplification of ground motion at rock sites within a fault zone in Nocera Umbra (central Italy)",{"EN":1288},"",{"VOID":1290},"10.1023\u002FA:1026559901378",[31],"https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1023\u002FA:1026559901378",[1294,1309,1322,1335,1348,1361,1374,1387,1400],{"id":1295,"sortIndex":32,"researcher":28,"roles":1296,"affiliations":1297,"properties":1306,"displayName":1308,"givenName":28,"familyName":28},"375af596-7ea5-4e53-b058-0365d7b1fb1d",[],[1298],{"id":1299,"sortIndex":32,"affiliation":1300,"properties":28},"bb4f3656-fc10-45be-8a75-ed5047f282aa",{"id":1299,"createTime":28,"updateTime":28,"relativeEntities":1301,"slug":28,"properties":1302,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1305,"statistic":28},[],{"title":1303},{"VI":1304},"Istituto Nazionale di Geofisica, Roma, Italy",[],{"title":1307},{"EN":1308},"F. 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Res. Lett. 25(15), 2861–2864.",{"id":28,"text":1467,"url":28,"identifiers":28},"Bonilla, L.F., Steidl, J.H., Lindley, G.T., Tumarkin, A.G. and Archuleta, R.J., 1997, Site amplification in the San Fernando Valley, California: variability of site-effect estimation using the S-wave, coda and H\u002FV methods, Bull. Seism. Soc. Am. 87, 710–730.",{"id":28,"text":1469,"url":28,"identifiers":28},"Caserta, A., Bellucci, F., Cultrera, G., Donati, S., Marra, F., Mele, G., Palombo, B. and Rovelli, A., 2000, Site effects in the area of Nocera Umbra (central Italy) during the 1997 Umbria-Marche seismic sequence, Journal of Seismology, this volume.",{"id":28,"text":1471,"url":28,"identifiers":28},"Cello, G., Mazzoli, S., Tondi, E. and Turco, E., 1997, Active tectonics in the Central Apennines and possible implication for seismic hazard analysis in peninsular Italy, Tectonophysics 272, 43–60.",{"id":28,"text":1473,"url":28,"identifiers":28},"Cormier, V.F. and Spudich, P., 1984, Amplification of ground motion and waveform complexity in fault zones: examples from the San Andreas and Calaveras Faults, Geophys. J. R. astr. Soc. 79, 135–152.",{"id":28,"text":1475,"url":28,"identifiers":28},"Cranswick, E., 1988, The information content of high-frequency seismograms and the near-surface geologic structure of 'hard rock' recording sites, Pageoph 128, 333–363.",{"id":28,"text":1477,"url":28,"identifiers":28},"Ekstrom, G., Morelli, A., Boschi, E. and Dziewonski, A.M., 1998, Moment tensor analysis of the central Italy earthquake sequence of September-October 1997, Geophys. Res. Lett. 25(11), 1971–1974.",{"id":28,"text":1479,"url":28,"identifiers":28},"Field, E.H. and Jacob, K., 1995, A comparison and test of various site response estimation techniques, including three that are non reference-site dependent, Bull. Seism. Soc. Am. 85, 1127–1143.",{"id":28,"text":1481,"url":28,"identifiers":28},"GNDT, 1999, Nocera Umbra: elementi di microzonazione sismica, GNDT - SSN Report, http:\u002F\u002Fdaphne.irrs.mi.cnr.it\u002Fseism\u002FItal\u002Fhomeum.html.",{"id":28,"text":1483,"url":28,"identifiers":28},"Lachet, C. and Bard, P.-Y., 1994, Numerical and theoretical investigations on the possibilities and limitations of the Nakamura's technique, J. Phys. Earth 42, 377–397.",{"id":28,"text":1485,"url":28,"identifiers":28},"Lermo, J.F. and Chavéz Garcia, F.J., 1993, Site effect evaluation using spectral ratios with only one station, Bull. Seism. Soc. Am. 83, 1574–1594.",{"id":28,"text":1487,"url":28,"identifiers":28},"Li, Y.-G. and Leary, P.C., 1990, Fault zone trapped seismic waves, Bull. Seism. Soc. Am. 80, 1245–1271.",{"id":28,"text":1489,"url":28,"identifiers":28},"Li, Y.-G., Leary, P., Aki, K. and Malin, P., 1990, Seismic trapped modes in the Oroville and San Andreas Fault zones, Science 249, 763–766.",{"id":28,"text":1491,"url":28,"identifiers":28},"Li, Y.-G., Vidale, J.E., Aki, K., Marone, C.J., and Lee, W.H.K., 1994, Fine structure of the Landers fault zone: segmentation and the rupture process, Science 265, 367–370.",{"id":28,"text":1493,"url":28,"identifiers":28},"Li, Y.-G., Vidale, J.E., Aki, K., Xu, F. and Burdette, T., 1998, Evidence of shallow fault zone strengthening after the 1992 M7.5 Landers, California, earthquake, Science 279, 217–219.",{"id":28,"text":1495,"url":28,"identifiers":28},"Nakamura, Y., 1989, A method for dynamic characteristics estimation of subsurface using microtremors on the ground surface, Quarterly Rept. RTRI, Jpn. 30, 25–33.",{"id":28,"text":1497,"url":28,"identifiers":28},"Ohmachi, T., Nakamura, Y. and Toshinawa, T., 1991, Ground Motion Characteristics in the San Francisco Bay Area Detected by Microtremor Measurements, Proceedings of the Second International Conference on Recent Advances in Geotechnical Engineering and Soil Dynamics, March 11- 15, St. Louis, Missouri, pp. 1643–1648.",{"id":28,"text":1499,"url":28,"identifiers":28},"Pino, N.A., Mazza, S., and Boschi, E., 1999, Rupture directivity of the major shocks in the 1997 Umbria Marche (Central Italy) sequence from regional broad band waveforms, Geophys. Res. Lett. 26, 2101–2104.",{"id":28,"text":1501,"url":28,"identifiers":28},"Rovelli, A., Bonamassa, O., Cocco, M., Di Bona, M. and Mazza, S., 1988, Scaling laws and spectral parameters of the ground motion in active extensional areas in Italy, Bull. Seism. Soc. Am. 78, 530–560.",{"id":28,"text":1503,"url":28,"identifiers":28},"Sabetta, F. and Pugliese, A., 1987, Attenuation of peak horizontal acceleration and velocity from Italian strong-motion records, Bull. Seism. Soc. Am. 77, 1491–1513.",{"id":28,"text":1505,"url":28,"identifiers":28},"Tucker, B.E. and King, J.L., 1984, Dependence of sediment-filled valley response on input amplitude and valley properties, Bull. Seism. Soc. Am. 74, 153–165.",{"id":1507,"createTime":1508,"updateTime":1509,"relativeEntities":1510,"slug":1511,"properties":1512,"entityType":961,"verifyStatus":26,"verifyTime":1509,"verifyNote":962,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1521,"fullTextUrl":28,"authors":1522,"publicationType":981,"publisherRelationship":1538,"citationCount":28,"citationInfo":28,"publishDate":1590,"publishYear":1591,"citationAnalyzeStatus":880,"lastCitationAnalyze":28,"indexDatabases":1592,"openAccess":28,"references":28,"isForceReanalyzing":1037},"014885c6-65af-4ca6-9124-22df7caee7d5","2024-01-26T05:51:09.505+00:00","2024-12-28T19:13:25.950+00:00",[],"An-investigation-of-analysis-of-variance-as-a-tool-for-exploring-regional-differences-in-strong-ground-motions",{"abstract":1513,"title":1515,"references":1517,"doi":1519},{"EN":1514},"The statistical technique known as analysis of variance is applied to a large set of European strong-motion data to investigate whether strong ground motions show a regional dependence. This question is important when selecting strong-motion records for the derivation of ground motion prediction equations and also when choosing strong-motion records from one geographical region for design purposes in another. Five regions with much strong-motion data (the Caucasus region, central Italy, Friuli, Greece and south Iceland) are investigated here. For the magnitude and distance range where there are overlapping data from the five areas (2.50≤ Ms≤ 5.50, 0≤ d ≤ 35 km) and consequently analysis of variance can be performed, there is little evidence for a regional dependence of ground motions. There is a lack of data from moderate and large magnitude earthquakes (Ms > 5.5) so analysis of variance cannot be performed there. Since there is uncertainty regarding scaling ground motions from small to large magnitudes whether ground motions from large earthquakes are significantly different in different parts of Europe is not known. Analysis of variance has the ability to complement other techniques for the assessment of regional dependence of ground motions.",{"EN":1516},"An investigation of analysis of variance as a tool for exploring regional differences in strong ground motions",{"VOID":1518},"Ambraseys, N.N. and Bommer, J.J., 1990, Uniform magnitude re-evaluation for the strong-motion database of Europe and adjacent areas, Eur. Earthquake Eng. IV, 3–16.\nAmbraseys, N.N. and Bommer, J.J., 1991, The attenuation of ground accelerations in Europe, Earthquake Eng. Struct. Dyn. 20, 1179–1202.\nAmbraseys, N. and J. Douglas, 2000, Reappraisal of surface wave magnitudes in the Eastern Mediterranean region and the Middle East, Geophys. J. Int. 141, 357–373.\nAmbraseys, N.N., Douglas, J., Sigbjörnsson, R., Berge-Thierry, C., Suhadolc, P., Costa, G. and Smit, P.M., 2004a, Dissemination of European strong-motion data, vol. 2, using Strong-Motion Datascape Navigator. CD-ROM collection. Engineering and Physical Sciences Research Council, United Kingdom.\nAmbraseys, N.N., Simpson, K.A. and Bommer, J.J., 1996, Prediction of horizontal response spectra in Europe, Earthquake Eng. Struct. Dyn. 25, 371–400.\nAmbraseys, N.N., Simpson, K.A. and Bommer, J.J., 1997, Authors’ reply, Earthquake Eng. Struct. Dyn. 26, 295–300.\nAmbraseys, N., Smit, P., Berardi, R., Rinaldis, D., Cotton, F. and Berge, C., 2000, Dissemination of European Strong-Motion Data. CD-ROM collection. European Commission, Directorate-General XII, Environmental and Climate Programme, ENV4-CT97-0397, Brussels, Belgium.\nAmbraseys, N.N., Smit, P., Douglas, J., Margaris, B., Sigbjörnsson, R., ‘Olafsson, S., Suhadolc, P. and Costa, G., in press, Internet site for European strong-motion data, Bollettino Geofisica Teorica Appl.\nAmbraseys, N., Smit, P., Sigbjörnsson, R., Suhadolc, P. and Margaris, B., 2002, Internet-site for European strong-motion data. http:\u002F\u002Fwww.isesd.cv.ic.ac.uk. European Commission, Directorate-General XII, Environmental and Climate Programme, Brussels, Belgium.\nBergerat, F., Gudmundsson, A., Angelier, J. and Rögnvaldsson, S.T., 1998, Seismotectonics of the central part of the south Iceland seismic zone, Tectonophysics 298, 319–335.\nBoore, D.M., 1983. Stochastic simulation of high-frequency ground motions based on seismological models of the radiated spectra, Bull. Seismol. Soc. Am. 73, 1865–1894.\nBoore, D.M., Joyner, W.B. and Fumal, T.E., 1993, Estimation of response spectra and peak accelerations from western North American earthquakes: An interim report. Open-File Report 93-509, U.S. Geological Survey. 70 p.\nCampbell, K.W., 2003, Prediction of strong ground motion using the hybrid empirical method and its use in the development of ground-motion (attenuation) relations in eastern North America, Bull. Seismol. Soc. Am. 93, 1012–1033.\nCello, G., Mazzoli, S., Tondi, E. and Turco, E., 1997, Active tectonics in the central Apennines and possible implications for seismic hazard analysis in central Italy, Tectonophysics 272, 43–68.\nChen, S.-Z. and Atkinson, G.M., 2002, Global comparison of earthquake source spectra, Bull. Seismol. Soc. Am. 92, 885–895.\nDouglas, J., 2003a. Earthquake ground motion estimation using strong-motion records: A review of equations for the estimation of peak ground acceleration and response spectral ordinates, Earth-Sci. Rev. 61, 43–104.\nDouglas, J., 2003b, What is a poor quality strong-motion record? Bull. Earthquake Eng. 1, 141–156.\nDouglas, J. and Smit, P.M., 2001, How accurate can strong ground motion attenuation relations be? Bull. Seismol. Soc. Am. 91, 1917–1923.\nDraper, N.R. and Smith, H., 1981, Applied Regression Analysis. 2nd ed., John Wiley & Sons.\nFisher, R.A., 1990, Statistical Methods, Experimental Design, and Scientific Inference, Oxford University Press, Oxford, United Kingdom.\nFree, M.W., 1996, The Attenuation of Earthquake Strong-Motion in Intraplate Regions. Ph.D. Thesis, University of London.\nGreen, J.R. and Margerison, D., 1979, Statistical Treatment of Experimental Data, Physical Sciences Data 2, Second Impression edition, Elsevier Scientific Publishing Company, Amsterdam, The Netherlands.\nHanks, T.C. and Johnston, A.C., 1992, Common features of the excitation and propogation of strong ground motion for north American earthquakes, Bull. Seismol. Soc. Am. 82, 1–23.\nJackson, J., 2001, Living with earthquakes: Know your faults, J. Earthquake Eng. 5, 5–123.\nJoyner, W.B. and Boore, D.M., 1981, Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 Imperial Valley, California, earthquake, Bull. Seismol. Soc. Am. 71, 2011–2038.\nKanamori, H. 1977, The energy release in great earthquakes, J. Geophys. Res. 82, 2981–2987.\nLee, V. W., 1995, Pseudo relative velocity spectra in former Yugoslavia, Eur. Earthquake Eng. IX, 12–22.\nSigbjornsson, R. and Baldvinsson, G.I., 1992, Seismic hazard and recordings of strong ground motion in Iceland, In: Proceedings of Tenth World Conference on Earthquake Engineering, vol. 1, A.A. Balkema, Rotterdam, The Netherlands. Madrid, Spain, 19–24 July, pp. 419–424.\nSlejko, D., Neri, G., Orozova, I., Renner, G., and Wyss, M., 1999, Stress field in Friuli (NE Italy) from fault plane solutions of activity following the 1976 main shock, Bull. Seismol. Soc. Am. 89, 1037–1052.\nSpudich, P., Joyner, W.B., Lindh, A.G., Boore, D.M., Margaris, B.M. and Fletcher, J.B., 1999, SEA99: A revised ground motion prediction relation for use in extensional tectonic regimes, Bull. Seismol. Soc. Am. 89, 1156– 1170.\nSuhadolc, P. and Chiaruttini, C., 1987, A theoretical study of the dependence of the peak ground acceleration on source and structure parameters. In: M. Erdik and Toksöz, M., (eds.), Strong Ground Motion Seismology, D. Reidel Publishing Company pp. 143–183.\nWells, D.L. and Coppersmith, K.J., 1994, New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement, Bull. Seismol. Soc. Am. 84, 974–1002.",{"VOID":1520},"10.1007\u002Fs10950-004-3094-7","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10950-004-3094-7",[1523],{"id":1524,"sortIndex":32,"researcher":28,"roles":1525,"affiliations":1526,"properties":1535,"displayName":1537,"givenName":28,"familyName":28},"b28d8c78-9545-46d1-aec3-8803dcef473c",[968],[1527],{"id":1528,"sortIndex":32,"affiliation":1529,"properties":28},"17cfc4be-e193-4c26-9b0f-914077eeb0fe",{"id":1528,"createTime":28,"updateTime":28,"relativeEntities":1530,"slug":28,"properties":1531,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1534,"statistic":28},[],{"title":1532},{"VI":1533},"Department of Civil & Environmental Engineering, Imperial College London, South Kensington Campus, London, U.K.",[],{"title":1536},{"VI":1537},"John Douglas",{"url":1521,"publisher":1539,"properties":1585},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1540,"slug":872,"properties":1541,"entityType":25,"verifyStatus":880,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1545,"manageAffiliations":1554,"indexDatabases":1565,"url":940,"thumbnailPath":28,"statistic":1580,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1542,"title":1543,"eissn":1544},{"VOID":875},{"EN":877},{"VOID":879},[1546,1550],{"id":883,"createTime":28,"updateTime":28,"relativeEntities":1547,"label":1548,"description":1549,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":886},{},{"id":889,"createTime":28,"updateTime":28,"relativeEntities":1551,"label":1552,"description":1553,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":892},{},[1555,1560],{"id":896,"createTime":28,"updateTime":28,"relativeEntities":1556,"slug":28,"properties":1557,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1559,"statistic":28},[],{"title":1558},{"EN":900},[902],{"id":904,"createTime":28,"updateTime":28,"relativeEntities":1561,"slug":28,"properties":1562,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1564,"statistic":28},[],{"title":1563},{"EN":908},[],[1566,1573],{"id":912,"indexDatabase":1567,"url":924,"indexYears":28,"academicFieldIds":1572,"indexDatabaseRanking":28},{"id":914,"createTime":28,"updateTime":28,"relativeEntities":1568,"label":1569,"description":1570,"key":921,"publicationTags":1571,"standard":28},[],{"EN":917,"VI":917},{"EN":919,"VI":920},[923,813],[926],{"id":928,"indexDatabase":1574,"url":934,"indexYears":935,"academicFieldIds":1579,"indexDatabaseRanking":939},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1575,"label":1576,"description":1577,"key":781,"publicationTags":1578,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[937,938],{"impactFactor":32,"impactFactorByYear":1581,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":279,"totalPublicationByYear":1582,"totalCitation":32,"totalCitationByYear":1583,"totalCitationPerPublication":32,"totalCitationPerPublicationByYear":1584,"hindexLast5Year":32,"hindex":32},{},{"1997":48,"1998":42,"1999":46,"2000":48,"2001":49,"2002":46,"2003":40,"2005":40,"2006":40,"2007":40,"2008":40,"2012":123,"2013":40,"2016":123,"2018":123,"2020":40,"2022":42},{},{},{"pages":1586,"volume":1588},{"VOID":1587},"485-496",{"VOID":1589},"8","2004-10-01",2004,[939,923],{"id":1594,"createTime":1595,"updateTime":1595,"relativeEntities":1596,"slug":1597,"properties":1598,"entityType":961,"verifyStatus":880,"verifyTime":28,"verifyNote":28,"languages":1606,"translateLanguages":28,"viewCount":32,"primaryUrl":1607,"fullTextUrl":28,"authors":1608,"publicationType":981,"publisherRelationship":1686,"citationCount":28,"citationInfo":28,"publishDate":1733,"publishYear":1734,"citationAnalyzeStatus":880,"lastCitationAnalyze":28,"indexDatabases":1735,"openAccess":28,"references":1736,"isForceReanalyzing":1037},"01f9f8aa-259a-4657-bbfb-fca9e78b5b52","2024-04-15T10:03:03.931+00:00",[],"An-attenuation-study-using-earthquakes-from-the-1997-Umbria-Marche-sequence",{"abstract":1599,"title":1601,"keywords":1603,"doi":1604},{"EN":1600},"We studied spatial and temporal characteristics of seismic attenuation inCentral Italy using S- and coda- waves recorded by the MarchesanSeismograph Network from earthquakes located in the epicentral area ofthe 1997 Umbria-Marche sequence. The amplitude decay of the S waveswith distance was defined calculating empirical attenuation functions at 15frequencies between 1 and 25 Hz. We analyzed separately foreshocks andaftershocks and we found the same attenuation functions, suggesting thatthe possible temporal variations could be confined in a small area. Thefrequency dependence of Q\nS was approximated by the equation Q\nS=18 · f\n2.0between 1 and 10 Hz. At higher frequencies (10–25 Hz), the frequencydependence of Q\ns weakens, having an average value of Q\nS=990. We also estimated Q from coda waves (Q\nC) using the single-scattering models of Aki andChouet (1975) and Sato (1977). We found that Q\nC=77 · f\n0.6, (between 2 and 20Hz) at the western side of the mountain chain, using either foreshocks oraftershocks. This relation is consistent with previous estimates of Q\nCreported for the Central Apennines. For a volume sampling the Colfioritobasin, the Apennines and the Marche region we found that Q\nC=55 · f\n0.8,indicating highattenuation below the mountain belt. To detect small temporal changes ofQ, we calculated spectral ratios of 5 temporal doublets located in theepicentral area and recorded at the closest station. We found temporalchanges of Q that vary from 27% to 56%, depending on the locationof the doublets. This variability suggests that the temporal change ofattenuation may depend on the spatial variation of Q and perhaps on thespatial distribution of tectonic stress in the epicentral area.",{"EN":1602},"An attenuation study using earthquakes from the 1997 Umbria-Marche sequence",{"EN":1288},{"VOID":1605},"10.1023\u002FA:1014245406628",[31],"https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1023\u002FA:1014245406628",[1609,1624,1639,1652,1673],{"id":1610,"sortIndex":32,"researcher":28,"roles":1611,"affiliations":1612,"properties":1621,"displayName":1623,"givenName":28,"familyName":28},"d3ab6383-8c43-4213-a797-633b1abc0a34",[],[1613],{"id":1614,"sortIndex":32,"affiliation":1615,"properties":28},"9351a845-f0e0-4aea-8b13-935ad9565e4e",{"id":1614,"createTime":28,"updateTime":28,"relativeEntities":1616,"slug":28,"properties":1617,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1620,"statistic":28},[],{"title":1618},{"EN":1619},"División Ciencias de la Tierra, CICESE, Baja California, México",[],{"title":1622},{"EN":1623},"Raúl R. Castro",{"id":1625,"sortIndex":40,"researcher":28,"roles":1626,"affiliations":1627,"properties":1636,"displayName":1638,"givenName":28,"familyName":28},"04d26309-e457-437c-bab5-023b20f82ed8",[],[1628],{"id":1629,"sortIndex":32,"affiliation":1630,"properties":28},"72191c68-cec9-4709-9bc6-b79c03ffd6b1",{"id":1629,"createTime":28,"updateTime":28,"relativeEntities":1631,"slug":28,"properties":1632,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1635,"statistic":28},[],{"title":1633},{"EN":1634},"Osservatorio Geofísico Sperimentale di Macerata, Macerata, Italia",[],{"title":1637},{"EN":1638},"Giancarlo Monachesi",{"id":1640,"sortIndex":123,"researcher":28,"roles":1641,"affiliations":1642,"properties":1649,"displayName":1651,"givenName":28,"familyName":28},"fee1e2c2-b61c-4f5b-8e61-78684ec0be62",[],[1643],{"id":1629,"sortIndex":32,"affiliation":1644,"properties":28},{"id":1629,"createTime":28,"updateTime":28,"relativeEntities":1645,"slug":28,"properties":1646,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1648,"statistic":28},[],{"title":1647},{"EN":1634},[],{"title":1650},{"EN":1651},"Luca Trojani",{"id":1653,"sortIndex":42,"researcher":28,"roles":1654,"affiliations":1655,"properties":1670,"displayName":1672,"givenName":28,"familyName":28},"8e40aa2f-5949-41a3-b36a-7576a24af227",[],[1656,1662],{"id":1629,"sortIndex":32,"affiliation":1657,"properties":28},{"id":1629,"createTime":28,"updateTime":28,"relativeEntities":1658,"slug":28,"properties":1659,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1661,"statistic":28},[],{"title":1660},{"EN":1634},[],{"id":1663,"sortIndex":32,"affiliation":1664,"properties":28},"de946122-5cc7-41c8-a84a-7b136b4f6a26",{"id":1663,"createTime":28,"updateTime":28,"relativeEntities":1665,"slug":28,"properties":1666,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1669,"statistic":28},[],{"title":1667},{"EN":1668},"Universita della Basilicata, Potenza, Italia",[],{"title":1671},{"EN":1672},"Marco Mucciarelli",{"id":1674,"sortIndex":45,"researcher":28,"roles":1675,"affiliations":1676,"properties":1683,"displayName":1685,"givenName":28,"familyName":28},"acdb828b-a859-4d4d-bcd7-3cb7a66bc4da",[],[1677],{"id":1629,"sortIndex":32,"affiliation":1678,"properties":28},{"id":1629,"createTime":28,"updateTime":28,"relativeEntities":1679,"slug":28,"properties":1680,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1682,"statistic":28},[],{"title":1681},{"EN":1634},[],{"title":1684},{"EN":1685},"Massimo Frapiccini",{"url":28,"publisher":1687,"properties":28},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1688,"slug":872,"properties":1689,"entityType":25,"verifyStatus":880,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1693,"manageAffiliations":1702,"indexDatabases":1713,"url":940,"thumbnailPath":28,"statistic":1728,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1690,"title":1691,"eissn":1692},{"VOID":875},{"EN":877},{"VOID":879},[1694,1698],{"id":883,"createTime":28,"updateTime":28,"relativeEntities":1695,"label":1696,"description":1697,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":886},{},{"id":889,"createTime":28,"updateTime":28,"relativeEntities":1699,"label":1700,"description":1701,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":892},{},[1703,1708],{"id":896,"createTime":28,"updateTime":28,"relativeEntities":1704,"slug":28,"properties":1705,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1707,"statistic":28},[],{"title":1706},{"EN":900},[902],{"id":904,"createTime":28,"updateTime":28,"relativeEntities":1709,"slug":28,"properties":1710,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1712,"statistic":28},[],{"title":1711},{"EN":908},[],[1714,1721],{"id":912,"indexDatabase":1715,"url":924,"indexYears":28,"academicFieldIds":1720,"indexDatabaseRanking":28},{"id":914,"createTime":28,"updateTime":28,"relativeEntities":1716,"label":1717,"description":1718,"key":921,"publicationTags":1719,"standard":28},[],{"EN":917,"VI":917},{"EN":919,"VI":920},[923,813],[926],{"id":928,"indexDatabase":1722,"url":934,"indexYears":935,"academicFieldIds":1727,"indexDatabaseRanking":939},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1723,"label":1724,"description":1725,"key":781,"publicationTags":1726,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[937,938],{"impactFactor":32,"impactFactorByYear":1729,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":279,"totalPublicationByYear":1730,"totalCitation":32,"totalCitationByYear":1731,"totalCitationPerPublication":32,"totalCitationPerPublicationByYear":1732,"hindexLast5Year":32,"hindex":32},{},{"1997":48,"1998":42,"1999":46,"2000":48,"2001":49,"2002":46,"2003":40,"2005":40,"2006":40,"2007":40,"2008":40,"2012":123,"2013":40,"2016":123,"2018":123,"2020":40,"2022":42},{},{},"2002-01-01",2002,[939,923],[1737,1739,1741,1743,1745,1747,1749,1751,1753,1755,1757,1759,1761,1763,1765,1767,1769,1771,1773,1775,1777,1779,1781,1783,1785,1787,1789,1791,1793,1795,1797,1799,1801,1803,1805,1807,1809,1811,1813,1815,1817,1819],{"id":28,"text":1738,"url":28,"identifiers":28},"Abercrombie, R.E., 1995, Earthquake source scaling relationships from-1 to 5 ML using seismograms recorded at 2.5 km depth, J. Geophys. Res. 100, 24,015–24,036.",{"id":28,"text":1740,"url":28,"identifiers":28},"Aki, K. and Chouet, B., 1975, Origin of coda waves: Source, attenuation, and scattering effects. J. Geophys. Res. 80, 3322–3342.",{"id":28,"text":1742,"url":28,"identifiers":28},"Aki, K., 1980, Scattering and attenuation of shear waves in the lithosphere, J. Geophys. Res. 85, 6496–6504.",{"id":28,"text":1744,"url":28,"identifiers":28},"Anderson, J.G. and Quaas, R., 1988, The Mexico earthquake of September 19, 1985: effect of magnitude on the character of strong ground motion: an example from the Guerrero, Mexico strong motion network, Earthquake Spectra 4, 635–646.",{"id":28,"text":1746,"url":28,"identifiers":28},"Anderson, J.G. and Lei, Y., 1994, Nonparametric description of peak acceleration as a function of magnitude, distance and site in Guerrero, Mexico, Bull. Seism. Soc. 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Res. 3, 519–543.",{"id":1822,"createTime":1823,"updateTime":1824,"relativeEntities":1825,"slug":1826,"properties":1827,"entityType":961,"verifyStatus":26,"verifyTime":1824,"verifyNote":962,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1836,"fullTextUrl":28,"authors":1837,"publicationType":981,"publisherRelationship":1853,"citationCount":28,"citationInfo":28,"publishDate":1904,"publishYear":1166,"citationAnalyzeStatus":880,"lastCitationAnalyze":28,"indexDatabases":1905,"openAccess":28,"references":28,"isForceReanalyzing":1037},"0208c9e2-4116-4bf9-9308-bb1cb31ba9da","2024-01-24T15:24:26.217+00:00","2024-12-31T19:17:58.073+00:00",[],"Intermediate-term-variations-in-200-years-seismicity-at-the-north-of-Iran",{"abstract":1828,"title":1830,"references":1832,"doi":1834},{"EN":1829},"In this paper, significant variations in rate of moderate-large earthquake occurrence during the last two centuries at the north of Persia (Alborz, Azarbaijan, and Kopeh Dagh seismotectonic provinces) were chronically investigated. Depths of some historical and instrumental earthquakes were reasonably estimated using macroseismic data. Also, empirical relationships were developed between the maximum intensity and magnitude of the earthquakes in the north of Persia. Two centuries of earthquake data (M ≥5.0) reliably demonstrates that quite periods with durations of about a few years to two decades have happened and have been subsequently followed by active periods with durations of about 10 to 70 years. The time variation of seismic hazards (achieved by the macroseismic maximum intensity, I0 ≥IV) almost displays a similar behavior at the study area. According to both patterns of the time variations of seismicity and the seismic hazards, it may conclude that we are within a low rate of seismic period, and we may expect a higher rate of seismicity at the Alborz in the next decades. Finally, in both the Azarbaijan and Kopeh Dagh areas, we discovered considerable migrations of the seismicity from the east to the west.",{"EN":1831},"Intermediate-term variations in 200 years seismicity at the north of Iran",{"VOID":1833},"Akasheh B, Eshghi I (1979) The Iran earthquake of Dec. 19 1977 (Bab-Tangal), Northwestern Kerman. Iran. J. Earth and Space Phys 8\nAmbraseys NN (1974) Historical seismicity of north-Central Iran. Geol Surv Iran Rep 29:47–95\nAmbraseys NN (1981) On the long term seismicity of the Hellenic arc. Boll Geofis Teor Appl 23:355–359\nAmbraseys N, Bilham R (2003) Earthquakes in Afghanistan. Seismol Res Lett 74:107–123\nAmbraseys N, Melville C (1982) A history of Persian earthquakes. Cambridge University Press, Cambridge, p 219\nAmbraseys N, Moinfar A, Tchalenko J (1971) The Karnaveh (Northeast Iran) earthquake of 30 July 1970. Ann Geophys 24:475–495\nAshtari M, Hatzfeld D, Kamalian N (2005) Microseismicity in the region of Tehran. 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C., pp 153–172",{"VOID":1835},"10.1007\u002Fs10950-015-9483-2","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10950-015-9483-2",[1838],{"id":1839,"sortIndex":32,"researcher":28,"roles":1840,"affiliations":1841,"properties":1850,"displayName":1852,"givenName":28,"familyName":28},"15c659bf-6e01-4ce0-a39a-f27e9cdee3d5",[968],[1842],{"id":1843,"sortIndex":32,"affiliation":1844,"properties":28},"01e17f6e-1143-4355-97ee-20ad79ed286d",{"id":1843,"createTime":28,"updateTime":28,"relativeEntities":1845,"slug":28,"properties":1846,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1849,"statistic":28},[],{"title":1847},{"VI":1848},"Department of Geology, Faculty of Science and Earthquake Research Center of Shahid Bahonar University of Kerman, Kerman, Iran",[],{"title":1851},{"VI":1852},"Majid Nemati",{"url":1836,"publisher":1854,"properties":1900},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1855,"slug":872,"properties":1856,"entityType":25,"verifyStatus":880,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1860,"manageAffiliations":1869,"indexDatabases":1880,"url":940,"thumbnailPath":28,"statistic":1895,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1857,"title":1858,"eissn":1859},{"VOID":875},{"EN":877},{"VOID":879},[1861,1865],{"id":883,"createTime":28,"updateTime":28,"relativeEntities":1862,"label":1863,"description":1864,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":886},{},{"id":889,"createTime":28,"updateTime":28,"relativeEntities":1866,"label":1867,"description":1868,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":892},{},[1870,1875],{"id":896,"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},{"EN":900},[902],{"id":904,"createTime":28,"updateTime":28,"relativeEntities":1876,"slug":28,"properties":1877,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1879,"statistic":28},[],{"title":1878},{"EN":908},[],[1881,1888],{"id":912,"indexDatabase":1882,"url":924,"indexYears":28,"academicFieldIds":1887,"indexDatabaseRanking":28},{"id":914,"createTime":28,"updateTime":28,"relativeEntities":1883,"label":1884,"description":1885,"key":921,"publicationTags":1886,"standard":28},[],{"EN":917,"VI":917},{"EN":919,"VI":920},[923,813],[926],{"id":928,"indexDatabase":1889,"url":934,"indexYears":935,"academicFieldIds":1894,"indexDatabaseRanking":939},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1890,"label":1891,"description":1892,"key":781,"publicationTags":1893,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[937,938],{"impactFactor":32,"impactFactorByYear":1896,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":279,"totalPublicationByYear":1897,"totalCitation":32,"totalCitationByYear":1898,"totalCitationPerPublication":32,"totalCitationPerPublicationByYear":1899,"hindexLast5Year":32,"hindex":32},{},{"1997":48,"1998":42,"1999":46,"2000":48,"2001":49,"2002":46,"2003":40,"2005":40,"2006":40,"2007":40,"2008":40,"2012":123,"2013":40,"2016":123,"2018":123,"2020":40,"2022":42},{},{},{"pages":1901,"volume":1903},{"VOID":1902},"585-605",{"VOID":1164},"2015-02-10",[939,923],{"id":1907,"createTime":1908,"updateTime":1909,"relativeEntities":1910,"slug":1911,"properties":1912,"entityType":961,"verifyStatus":26,"verifyTime":1909,"verifyNote":962,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":1921,"fullTextUrl":28,"authors":1922,"publicationType":981,"publisherRelationship":1973,"citationCount":28,"citationInfo":28,"publishDate":2025,"publishYear":2026,"citationAnalyzeStatus":880,"lastCitationAnalyze":28,"indexDatabases":2027,"openAccess":28,"references":28,"isForceReanalyzing":1037},"0261bfc1-ef7e-4490-ab8f-0ada2685f32d","2024-02-07T18:35:18.703+00:00","2025-02-10T20:33:50.559+00:00",[],"Active-folding-in-the-Tenes-region-Tell-Atlas-Algeria-modelling-the-1922-earthquake-fault-related-fold-Mw-6-2-",{"abstract":1913,"title":1915,"references":1917,"doi":1919},{"EN":1914},"We study the Tenes Abou El Hassan (TAEH) fault-related fold of the Tell Atlas (the site of the 1922 Mw 6.2 earthquake) using field investigations combined with satellite image processing. The 1922 earthquake is also revisited through previous reports, publications and contemporaneous newspapers in order to locate the area of maximum ground motion and its relation to the active TAEH fault-related fold. The analysis of high-resolution (0.5 m) satellite imagery (panchromatic Pleiades tri-stereo images) allows the accurate study in tectonic geomorphology and the characterization of active and seismogenic deformation. High-resolution DEMs obtained from Pleiades images highlight alluvial and marine terraces with cumulative uplift during the Upper Pleistocene–Holocene period and allowed the identification of geomorphological markers along the active fold with recognition of complex tectonic structures. The fault-related fold is modelled using both elastic (Okada 1992) and kinematic (Trishear) approaches using balanced cross-sections that reveal 1.2 mm\u002Fyear shortening rate during the Upper Pleistocene–Holocene. Uplift rate calculated using marine and alluvial terrace altitudes is ~0.3 mm\u002Fyear during the Upper Pleistocene along the Allalah Quaternary basin and the coastal zone reaching ~1 mm\u002Fyear during the Holocene. The earthquake geology and correlation between surface deformation and seismotectonic modelling provides additional constraints on the 1922 earthquake fault parameters and related seismic hazard assessment in the Tell Atlas of Algeria.",{"EN":1916},"Active folding in the Tenes region (Tell Atlas, Algeria): modelling the 1922 earthquake fault-related fold (Mw 6.2)",{"VOID":1918},"Allmendinger R W (1999) Propagation-to-slip ratio and fold style in fault-propagation folds: perspectives gleaned from trishear modeling. Geological Society of America Abstracts with Programs\nAmbraseys N (1981) The El Asnam, Algeria, earthquake of 10th October 1980. Quart Jl Eng Geol 14:143–148\nAmbraseys N (1988) Magnitude-fault length relationships for earthquakes in the Middle East. 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Geophys J Int 99:761–788",{"VOID":1920},"10.1007\u002Fs10950-021-10005-4","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10950-021-10005-4",[1923,1947,1960],{"id":1924,"sortIndex":32,"researcher":28,"roles":1925,"affiliations":1926,"properties":1944,"displayName":1946,"givenName":28,"familyName":28},"ecd00ff2-c07c-46f4-8167-03df58ecdfc1",[968],[1927,1935],{"id":1928,"sortIndex":32,"affiliation":1929,"properties":28},"16446d7d-459d-4f9e-9c12-55ec9b852ed6",{"id":1928,"createTime":28,"updateTime":28,"relativeEntities":1930,"slug":28,"properties":1931,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1934,"statistic":28},[],{"title":1932},{"VI":1933},"Institut Terre et Environnement de Strasbourg, Université de Strasbourg, Strasbourg, 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Bagdi-Issaad",{"id":1948,"sortIndex":40,"researcher":28,"roles":1949,"affiliations":1950,"properties":1957,"displayName":1959,"givenName":28,"familyName":28},"f14798c3-563f-40a6-89d3-abf8e348e36a",[968],[1951],{"id":1928,"sortIndex":32,"affiliation":1952,"properties":28},{"id":1928,"createTime":28,"updateTime":28,"relativeEntities":1953,"slug":28,"properties":1954,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1956,"statistic":28},[],{"title":1955},{"VI":1933},[],{"title":1958},{"VI":1959},"Mustapha Meghraoui",{"id":1961,"sortIndex":123,"researcher":28,"roles":1962,"affiliations":1963,"properties":1970,"displayName":1972,"givenName":28,"familyName":28},"001e8266-6b98-40e1-91cc-dab06ab00d5c",[968],[1964],{"id":1936,"sortIndex":32,"affiliation":1965,"properties":28},{"id":1936,"createTime":28,"updateTime":28,"relativeEntities":1966,"slug":28,"properties":1967,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1969,"statistic":28},[],{"title":1968},{"VI":1941},[],{"title":1971},{"VI":1972},"Ahmed Nedjari",{"url":1921,"publisher":1974,"properties":2020},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1975,"slug":872,"properties":1976,"entityType":25,"verifyStatus":880,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1980,"manageAffiliations":1989,"indexDatabases":2000,"url":940,"thumbnailPath":28,"statistic":2015,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1977,"title":1978,"eissn":1979},{"VOID":875},{"EN":877},{"VOID":879},[1981,1985],{"id":883,"createTime":28,"updateTime":28,"relativeEntities":1982,"label":1983,"description":1984,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":886},{},{"id":889,"createTime":28,"updateTime":28,"relativeEntities":1986,"label":1987,"description":1988,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":892},{},[1990,1995],{"id":896,"createTime":28,"updateTime":28,"relativeEntities":1991,"slug":28,"properties":1992,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1994,"statistic":28},[],{"title":1993},{"EN":900},[902],{"id":904,"createTime":28,"updateTime":28,"relativeEntities":1996,"slug":28,"properties":1997,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1999,"statistic":28},[],{"title":1998},{"EN":908},[],[2001,2008],{"id":912,"indexDatabase":2002,"url":924,"indexYears":28,"academicFieldIds":2007,"indexDatabaseRanking":28},{"id":914,"createTime":28,"updateTime":28,"relativeEntities":2003,"label":2004,"description":2005,"key":921,"publicationTags":2006,"standard":28},[],{"EN":917,"VI":917},{"EN":919,"VI":920},[923,813],[926],{"id":928,"indexDatabase":2009,"url":934,"indexYears":935,"academicFieldIds":2014,"indexDatabaseRanking":939},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":2010,"label":2011,"description":2012,"key":781,"publicationTags":2013,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[937,938],{"impactFactor":32,"impactFactorByYear":2016,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":279,"totalPublicationByYear":2017,"totalCitation":32,"totalCitationByYear":2018,"totalCitationPerPublication":32,"totalCitationPerPublicationByYear":2019,"hindexLast5Year":32,"hindex":32},{},{"1997":48,"1998":42,"1999":46,"2000":48,"2001":49,"2002":46,"2003":40,"2005":40,"2006":40,"2007":40,"2008":40,"2012":123,"2013":40,"2016":123,"2018":123,"2020":40,"2022":42},{},{},{"pages":2021,"volume":2023},{"VOID":2022},"783-801",{"VOID":2024},"25","2021-04-10",2021,[939,923],{"id":2029,"createTime":2030,"updateTime":2031,"relativeEntities":2032,"slug":2033,"properties":2034,"entityType":961,"verifyStatus":26,"verifyTime":2031,"verifyNote":962,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":2043,"fullTextUrl":28,"authors":2044,"publicationType":981,"publisherRelationship":2075,"citationCount":28,"citationInfo":28,"publishDate":2126,"publishYear":2026,"citationAnalyzeStatus":880,"lastCitationAnalyze":28,"indexDatabases":2127,"openAccess":28,"references":28,"isForceReanalyzing":1037},"026c0c1a-fe24-4729-9641-b73fbaebf0ed","2024-01-05T03:31:35.632+00:00","2025-01-06T04:46:49.452+00:00",[],"Paleo-earthquake-evidence-and-earthquake-recurrence-for-D%C3%BCzce-fault-Turkey",{"abstract":2035,"title":2037,"references":2039,"doi":2041},{"EN":2036},"Paleoseismological trenching was performed along the Düzce fault providing some preliminary insight about its seismogenic behavior. Dating was based on radiocarbon analysis of peat samples collected from the trenches and suggested seven earthquakes have occurred since 1740 BC. Integrating date constraints of events exposed in the trenches suggests a periodical earthquake recurrence model. According to a linear sequential event serial that has minimum misfit determined by considering the probability curve limits of the sample dates, the earthquake recurrence interval is between 384 and 460 years (or possibly between AD 394 and 400). A probability curve was also calculated for the date of the last earthquake (1999 Düzce earthquake) considering the probability distributions of sample dates based on the same event serial. This probability-distribution-based method, similarly, predicted that the 1999 Düzce earthquake occurred between 1933 and 2005 (±36 years) with a 68% probability. After this verification, using this method, it was estimated that the next earthquake along the Düzce fault has a 68% probability of occurring between 2328 and 2392. According to this calculation, the earthquake recurrence interval is about 391 ± 34 years with a 68% probability and the AD 967 historical earthquake likely ruptured the Düzce fault. Assuming an average slip of 350 cm (the average slip of the 1999 earthquake), the slip rate was estimated to be between 8.7 and 11.2 mm\u002Fa.",{"EN":2038},"Paleo-earthquake evidence and earthquake recurrence for Düzce fault, Turkey",{"VOID":2040},"Ambraseys N (2002) The seismic activity of the Marmara sea region over the last 2000 years. Bull Seismol Soc Am 92:1–18. https:\u002F\u002Fdoi.org\u002F10.1785\u002F0120000843\nAmbraseys NN, Finkel CF (1995) The seismicity of Turkey and adjacent areas: a historical review. 1500-1800. Eren Yayıncılık ve Kitapçılık ltd. Şti., İstanbul. ISBN: 975-7622-38-9\nAmbraseys NN, Jackson JA (1998) Faulting associated with historical and recent earthquakes in the eastern Mediterranean region. Geophys J Int 133:390–406. https:\u002F\u002Fdoi.org\u002F10.1046\u002Fj.1365-246X.1998.00508.x\nBakır M (2002) Impact and consequences of earthquakes in byzantine Constantinople and its vicinity, a.D.342-1454. Dissertation, Boğaziçi University\nBronk Ramsey C (1995) Radiocarbon calibration and analysis of stratigraphy: the OxCal program. Radiocarbon 37:425–430. https:\u002F\u002Fdoi.org\u002F10.1017\u002FS0033822200030903\nBronk Ramsey C (2001) Development of the radiocarbon program. OxCal Radiocarb 43:355–363. https:\u002F\u002Fdoi.org\u002F10.1017\u002FS0033822200038212\nBronk Ramsey C (2004) Online version of the OxCal program, Ver. 3.9. Oxford radiocarbon accelerator unit, http:\u002F\u002Fwww.rlaha.ox.ac.uk\u002Forau\u002Findex.html. Accessed 11 Aug 2004\nEmre Ö, Duman TY, Toda S, Okuno M, Dogan A, Özalp S, Tsutsumi H, Tokay F, Haraguchi T, Kondo H, Sugito N, Nakamura T (2002) Paleoseismicity of Düzce fault in the last millennium, North Anatolian Fault zone (NAFZ), Turkey. 1st international symposium of the Faculty of Mines (İTÜ) on earth sciences and engineering 16-18 May 2002, İstanbul, Turkey, 59\nEmre O, Toda S, Doğan A, Awata Y, Tokay F, Ozalp S (2004) Paleoseismic behaviour of the Karadere fault between İzmit and Düzce ruptures in 1999, North Anatolian Fault, Turkey. 32nd IGC, Florence 2004 - abstracts\nHitchcock C, Altunel E, Barka A, Bachhuber J, Lettis W, Kozacı Ö, Helms J, Lindvall S (2003) Timing of Late Holocene earthquakes on the eastern Düzce fault and implications for slip transfer between the southern and northern strands of the North Anatolian Fault system, Bolu, Turkey. Turk J Earth Sci 12:119–136\nKarabacak V, Ring U, Uysal IT (2020) The off-fault deformation on the North Anatolian Fault zone and assessment of slip rate from carbonate veins. Tectonophysics 795:228633. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.tecto.2020.228633\nKing GCP, Hubert-Ferrari A, Nalbant SS, Meyer B, Armijo R, Bowman D (2001) Coulomb interactions and the 17 august 1999 Izmit, Turkey earthquake. C R Acad Sci IIA 333(9):557–569. https:\u002F\u002Fdoi.org\u002F10.1016\u002FS1251-8050(01)01676-7\nKonukçu E (1984) Düzce Tarihi (İlk Devirlerden Cumhuriyete). Türkiye İmar Turizm ve Sanayi Mecmuası 18:12–23\nPantosti D, Pucci S, Palyvos N, De Martini PM, D’Addezio G, Collins PEF, Zabci C (2008) Paleoearthquakes of the Duzce fault (North Anatolian Fault zone): insights for large surface faulting earthquake recurrence. J Geophys Res 113:B1. https:\u002F\u002Fdoi.org\u002F10.1029\u002F2006JB004679\nPucci S, De Martini PM, Pantosti D (2008) Preliminary slip rate estimates for the Düzce segment of the North Anatolian Fault Zone from offset geomorphic markers. Geomorphology 97:538–554. https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.geomorph.2007.09.002\nŞaroğlu F, Emre Ö, Kuşçu İ (1992) Active fault map of Turkey. General Directorate of Mineral Research and exploration (M.T.a), Ankara\nStuvier M, Reimer PJ, Bard E, Beck JW, Burr GS, Hughen KA, Kromer B, McCormac FG, van der Plicht J, Spurk M (1998) INTCAL98 Radiocarbon age calibration, 24,000-0 cal BP. Radiocarbon 40:1041–1083. https:\u002F\u002Fdoi.org\u002F10.1017\u002FS0033822200019123\nWallace RE (1987) Grouping and migration of surface faulting and variations in slip rates on faults in the Great Basin province. Bull Seismol Soc Am 77:868–876",{"VOID":2042},"10.1007\u002Fs10950-021-10002-7","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002Fs10950-021-10002-7",[2045,2060],{"id":2046,"sortIndex":32,"researcher":28,"roles":2047,"affiliations":2048,"properties":2057,"displayName":2059,"givenName":28,"familyName":28},"afdeb7a4-e997-4d4d-ac36-12f59029a460",[968],[2049],{"id":2050,"sortIndex":32,"affiliation":2051,"properties":28},"67b523d2-2d8d-479b-9867-3a354548c7de",{"id":2050,"createTime":28,"updateTime":28,"relativeEntities":2052,"slug":28,"properties":2053,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2056,"statistic":28},[],{"title":2054},{"VI":2055},"Geophysical Engineering, Faculty of Engineering, Çanakkale Onsekiz Mart University, Çanakkale, Turkey",[],{"title":2058},{"VI":2059},"Tolga Komut",{"id":2061,"sortIndex":40,"researcher":28,"roles":2062,"affiliations":2063,"properties":2072,"displayName":2074,"givenName":28,"familyName":28},"8cdbccda-3929-4c4c-b117-db831a4d51f9",[968],[2064],{"id":2065,"sortIndex":32,"affiliation":2066,"properties":28},"0ebabe08-b0c7-4521-8203-29810e89a0a1",{"id":2065,"createTime":28,"updateTime":28,"relativeEntities":2067,"slug":28,"properties":2068,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2071,"statistic":28},[],{"title":2069},{"VI":2070},"İzmir, Turkey",[],{"title":2073},{"VI":2074},"Ersin Karabudak",{"url":2043,"publisher":2076,"properties":2122},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":2077,"slug":872,"properties":2078,"entityType":25,"verifyStatus":880,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":2082,"manageAffiliations":2091,"indexDatabases":2102,"url":940,"thumbnailPath":28,"statistic":2117,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":2079,"title":2080,"eissn":2081},{"VOID":875},{"EN":877},{"VOID":879},[2083,2087],{"id":883,"createTime":28,"updateTime":28,"relativeEntities":2084,"label":2085,"description":2086,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":886},{},{"id":889,"createTime":28,"updateTime":28,"relativeEntities":2088,"label":2089,"description":2090,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":892},{},[2092,2097],{"id":896,"createTime":28,"updateTime":28,"relativeEntities":2093,"slug":28,"properties":2094,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2096,"statistic":28},[],{"title":2095},{"EN":900},[902],{"id":904,"createTime":28,"updateTime":28,"relativeEntities":2098,"slug":28,"properties":2099,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2101,"statistic":28},[],{"title":2100},{"EN":908},[],[2103,2110],{"id":912,"indexDatabase":2104,"url":924,"indexYears":28,"academicFieldIds":2109,"indexDatabaseRanking":28},{"id":914,"createTime":28,"updateTime":28,"relativeEntities":2105,"label":2106,"description":2107,"key":921,"publicationTags":2108,"standard":28},[],{"EN":917,"VI":917},{"EN":919,"VI":920},[923,813],[926],{"id":928,"indexDatabase":2111,"url":934,"indexYears":935,"academicFieldIds":2116,"indexDatabaseRanking":939},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":2112,"label":2113,"description":2114,"key":781,"publicationTags":2115,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[937,938],{"impactFactor":32,"impactFactorByYear":2118,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":279,"totalPublicationByYear":2119,"totalCitation":32,"totalCitationByYear":2120,"totalCitationPerPublication":32,"totalCitationPerPublicationByYear":2121,"hindexLast5Year":32,"hindex":32},{},{"1997":48,"1998":42,"1999":46,"2000":48,"2001":49,"2002":46,"2003":40,"2005":40,"2006":40,"2007":40,"2008":40,"2012":123,"2013":40,"2016":123,"2018":123,"2020":40,"2022":42},{},{},{"pages":2123,"volume":2125},{"VOID":2124},"803-823",{"VOID":2024},"2021-03-25",[939,923],{"id":2129,"createTime":2130,"updateTime":2131,"relativeEntities":2132,"slug":2133,"properties":2134,"entityType":961,"verifyStatus":26,"verifyTime":2143,"verifyNote":962,"languages":28,"translateLanguages":28,"viewCount":32,"primaryUrl":2144,"fullTextUrl":28,"authors":2145,"publicationType":981,"publisherRelationship":2216,"citationCount":28,"citationInfo":28,"publishDate":2268,"publishYear":2269,"citationAnalyzeStatus":880,"lastCitationAnalyze":28,"indexDatabases":2270,"openAccess":28,"references":28,"isForceReanalyzing":1037},"02f5e25a-f811-4ab4-b3f6-570ecd012498","2023-12-09T20:17:28.645+00:00","2025-02-24T20:17:17.912+00:00",[],"Characteristics-of-the-low-energy-seismicity-of-central-Apulia-southern-Italy-and-hazard-implications",{"abstract":2135,"title":2137,"references":2139,"doi":2141},{"EN":2136},"The central part of the Apulia region, in southern Italy, has been generally considered practically free from significant level of seismicity, but historical documentation, geological indicators and recent instrumental observations suggest that the activity of local minor tectonic structures could have been “masked” (and partly also induced) by that of major seismogenic structures located in the neighbouring regions. A revision of the central Apulia seismicity characteristics was conducted considering its space and time distribution, energy release rate and focal mechanisms, in view of possible hazard implications. To better constrain the seismicity rates inferable from the set of available historical data, special attention was paid to the declustering of a catalogue of low energy events (magnitude \u003C 3.5) instrumentally detected in about 20 years: a new declustering procedure, useful for cases like to the one at hand, was purposely devised taking into account the peculiarity of local seismicity characteristics and the limitations of the available database. The results obtained by combining instrumental and historical data show that this area is affected by a rather sporadic seismicity, likely associated to a general tensional regime and possibly stimulated by the interaction with Apenninic and northern Apulia seismogenic activity. Even though less energetic, the local seismicity contributes to increase the moderately damaging shaking probability due to the activity of seismic sources located in the near areas, so to justify the adoption of at least a minimum level of caution in relation to the local definition of seismic protection measures.",{"EN":2138},"Characteristics of the low energy seismicity of central Apulia (southern Italy) and hazard implications",{"VOID":2140},"Anderson, H. and Jackson, J., 1987, Active tectonics of the Adriatic region, Geophys. Journ. R.A.S. 91, 937–983.\nBaratta, M., 1901, I Terremoti d’Italia. Saggio di Storia, Geografia e Bibliografia Sismica Italiana, Bocca, Torino (anastatic reprint: Arnaldo Forni Editore, Sala Bolognese, 1979).\nBaratta, M., 1936, I Terremoti in Italia, Pubblicazione della Commissione Italiana per lo studio delle grandi calamità, Le Monnier, Firenze.\nBender, B., 1983, Maximum likelihood estimation of b values for magnitude grouped data, Bull. Seism. Soc. Am. 73, 831–851.\nBender, B. and Perkins, D.M., 1987, SEISRISK III: A computer program for seismic hazard estimation, U.S. Geological Survey, Bulletin 1772, pp. 48.\nBonito, M., 1691, Terra Tremante, o Vero Continuatione de’ Terremoti Dalla Creatione del Mondo Sino al Tempo Presente, Napoli. (anastatic reprint: Arnaldo Forni Editore, Sala Bolognese, 1980).\nBoschi, E., Ferrari, G., Gasperini, P., Guidoboni, E., Smriglio, G. and Valensise, G., 1995, Catalogo dei forti terremoti in Italia dal 461 a.C. al 1980. ING\u002FSGA, Bologna, p. 973 and a CD-ROM.\nBoschi, E., Guidoboni, E., Ferrari, G., Valensise, G. and Gasperini, P., 1997, Catalogo dei forti terremoti in Italia dal 461 a.C. al 1990. ING\u002FSGA, Bologna, p. 644 and a CD-ROM.\nBoschi, E., Guidoboni, E., Ferrari, G., Valensise, G., Mariotti, D. and Gasperini, P., 2000, Catalogue of strong Italian earthquakes from 461 B.C. to 1997, Ann. Geofis. 43, 609–868 and a CD-ROM.\nCalcagnile, G. and Panza, G.F., 1980, Upper mantle structure of the Apulian plate from Rayleigh waves, Pageoph. 119, 866–879.\nCamassi, R. and Stucchi, M., 1998, NT4.1, A parametric catalogue of damaging earthquakes in the Italian area. GNDT, Milano, Version NT4.1.1, marzo 1998, http:\u002F\u002Femidius.mi.ingv.it\u002FNT.\nChannel, J.E.T., D’Argenio, B. and Horvath, F., 1979, Adria, the African promontory, in Mesozoic Mediterranean Palaeogeography, Earth Sci. Rev. 15, 213–292.\nCiaranfi, N., Cinque, A., Lambiase, S., Pieri, P., Rapisardi, L., Ricchetti, G., Sgrosso, I. and Tortorici, L., 1981, Proposta di zonazione sismotettonica dell’Italia meridionale, Rend. Soc. Geol. It. 4, 493–496.\nCornell, C.A., 1968, Engineering seismic risk analysis, Bull. Seism. Soc. Am. 58, 1583–1606.\nCPTI Working Group (ING; GNDT; SGA; SSN), 1999, Catalogo parametrico dei terremoti italiani, Editrice Compositori, Bologna, p. 88 also available on http:\u002F\u002Femidius.itim.mi.cnr.it\u002FCPTI\u002Fhome.html.\nDel Gaudio, V., Iurilli, V., Pierri, P., Ruina, G., Calcagnile, G., Canziani, R., Moretti, M., Pieri, P. and Tropeano, M., 1996, Sismicità di bassa energia e caratteristiche strutturali delle Murge Nord-occidentali (Puglia-Italia meridionale). In: Atti 15° Convegno G.N.G.T.S., Roma, 11–13 November 1996, pp. 325–330.\nDel Gaudio, V., Festa, V., Ripa, R.R., Iurilli, V., Pierri, P., Calcagnile, G., Moretti, M., Pieri, P. and Tropeano, M., 2001, Evidence of Apulian crustal structures related to low energy seismicity (Murge–southern Italy), Ann. Geofis. 44, 1049–1066.\nDoglioni, C., Mongelli, F. and Pieri, P., 1994, The Puglia (SE Italy) uplift: an anomaly in the foreland of the Apenninic subduction due to buckling of a thick continental lithosphere, Tectonics 13, 1309–1321.\nFavali, P., Funiciello, R., Mattietti, G., Mele, G. and Salvini, F., 1993, An active margin across the Adriatic Sea (central Mediterranean Sea), Tectonophysics 219, 109–117.\nFilippo da Secinara, 1652, Trattato universale di tutti li terremoti occorsi e noti nel mondo con li casi infausti ed infelici pressagiti da tali terremoti, Aquila.\nFrepoli, A. and Amato, A., 2000, Fault plane solutions of crustal earthquakes in southern Italy (1988–1995): seismotectonic implications, Ann. Geofis. 43, 437–467.\nFrohlich, C. and Davis, S.D., 1990, Single-link cluster analysis as a method to evaluate spatial and temporal properties of earthquake catalogues, Geophys. J. Int. 100, 19–32.\nGasperini, P., 2002, Local magnitude revaluation for recent Italian earthquakes (1981–1996), J. Seismol. 6, 503–524.\nGiardini D., 1999, The Global Seismic Hazard Assessment Program (GSHAP) – 1992\u002F1999, Ann. Geofis. 42, 957–974.\nGodano, C., Tosi, P., De Rubeis, V. and Augliera, P., 1999, Scaling properties of the spatio-temporal distribution of earthquakes: a multifractal approach applied to a Californian catalogue, Geophys. J. Int. 136, 99–108.\nGutenberg, B. and Richter, C.F., 1942, Earthquake intensity, energy and acceleration, Bull. Seism. Soc. Am. 32, 163–191.\nGutenberg, B. and Richter, C.F., 1944, Frequency of earthquakes in California, Bull. Seism. Soc. Am. 34, 185–188.\nInstrumental Catalog Working Group, 2001, Catalogo strumentale dei terremoti italiani dal 1981 al 1996, Version 1.0 CD-ROM, Clueb, Bologna.\nKagan, Y.Y. and Jackson D.D., 1991, Long-term earthquake clustering, Geophys. J. Int. 104, 117–133.\nLahr, J.C., 1989, HYPOELLIPSE – Version 2.0: A computer program for determining local earthquakes hypocentral parameters, magnitude, and first-motion pattern, U.S. Geological Survey Open-File Report 89–116, 92 pp.\nMagri, G. and Molin, D., 1979, Attività macrosismica in Basilicata, Campania e Puglia dal 1847 al 1861, Technical Report, C.N.E.N., RT\u002FAMB (79) 5.\nMeletti, C., Patacca, E. and Scandone, P., 2000, Construction of a seismotectonic model: the case of Italy, Pure Appl. Geophys. 157, 11–35.\nMonachesi, G. and Stucchi, M., 1997, DOM4.1, An intensity database of damaging earthquakes in the Italian Area, C.N.R. – G.N.D.T., aggiornamento Web 2000, http:\u002F\u002Femidius.mi.ingv.it\u002FDOM.\nMoretti, M., Pieri, P., Tropeano, M. and Walsh, N., 1995, Tyrrhenian seismites in Bari area (Murge – Apulian Foreland). In: Atti del Convegno “Terremoti in Italia – Previsione e Prevenzione dei Danni,” Accademia Nazionale dei Lincei, Roma, 1–2 December 1994, 211–216.\nOgata, Y., 1989, Statistical model for standard seismicity and detection of anomalies by residual analysis, Tectonophysics 169, 159–174.\nOgata, Y., 1992, Detection of precursory relative quiescence before great earthquakes through a statistical model, J. Geophys. Res. 97, 19845–19871.\nPeresan, A., Panza, G.F. and Costa, G., 2000, CN algorithm and long-lasting changes in reported magnitudes: the case of Italy, Geophys. J. Int. 141, 425–437.\nPeterschmitt, E., 1956, Quelques donnes nouvelles sur les séismes profonds de la mer Tyrrhénienne, Ann. Geofis. 9, 305–334.\nPieri, P., Festa, V., Moretti, M. and Tropeano, M., 1997, Quaternary tectonic activity of the Murge area (Apulian foreland – southern Italy), Ann. Geofis. 40, 1395–1404.\nPostpischl, D. (ed.), 1985, Catalogo dei terremoti italiani dall’anno 1000 al 1980. 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