中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Meso-Cenozoic tectonic evolution of the Dangyang Basin, north-central Yangtze craton, central China

文献类型:期刊论文

作者Shi, Wei1,3; Dong, Shu-Wen2; Ratschbacher, Lothar3; Tian, Mi1,4; Li, Jian-Hua1; Wu, Guo-Li1,5
刊名INTERNATIONAL GEOLOGY REVIEW
出版日期2013
卷号55期号:3页码:382-396
关键词Dangyang Basin Yangtze craton palaeo-stress field tectonic evolution Meso-Cenozoic graben intracontinental orogeny
ISSN号0020-6814
DOI10.1080/00206814.2012.715732
文献子类Article
英文摘要Based on detailed structural data and available tectonic chronological data from the Dangyang Basin, the authors propose that the north-central Yangtze craton experienced three stages of tectonic evolution since Late Triassic time. In the Late Triassic to Early Jurassic (T-3-J(1)), due to the Indosinian orogeny, nearly N-S compression and shortening occurred, which initiated the Dangyang Basin as a foreland basin of the Qinling-Dabie orogen. During the Late Jurassic-Early Cretaceous (J(3)-K-1) period, the Yanshanian intracontinental orogeny caused contemporaneous NE-SW and NW-SE shortening, which resulted in intense folding of the foreland basin; contraction formed a brush structure diverging in a SE direction and strongly converging in a NWdirection around the Huangling anticline. In the Late Cretaceous to Palaeogene, the Yuan'an and Hanshui grabens were separated from other parts of the Dangyang Basin due to post-orogenic ENE-WSW extension. Finally, at the end of the Palaeogene, ENE-WSW shortening led to inversion and deformation of the grabens.
WOS关键词JIANGHAN BASIN ; EASTERN CHINA ; QINLING OROGEN ; FISSION-TRACK ; DABIE OROGEN ; DEFORMATION ; CONSTRAINTS ; ROCKS ; BELT ; GEOCHRONOLOGY
WOS研究方向Geology
语种英语
WOS记录号WOS:000311786500008
出版者TAYLOR & FRANCIS INC
资助机构National Natural Foundation of China(41172184) ; National Natural Foundation of China(41172184) ; German Academic Exchange Service (DAAD) ; German Academic Exchange Service (DAAD) ; DFG(RA 442/25) ; DFG(RA 442/25) ; (SINOPROBE-08-01) ; (SINOPROBE-08-01) ; National Natural Foundation of China(41172184) ; National Natural Foundation of China(41172184) ; German Academic Exchange Service (DAAD) ; German Academic Exchange Service (DAAD) ; DFG(RA 442/25) ; DFG(RA 442/25) ; (SINOPROBE-08-01) ; (SINOPROBE-08-01) ; National Natural Foundation of China(41172184) ; National Natural Foundation of China(41172184) ; German Academic Exchange Service (DAAD) ; German Academic Exchange Service (DAAD) ; DFG(RA 442/25) ; DFG(RA 442/25) ; (SINOPROBE-08-01) ; (SINOPROBE-08-01) ; National Natural Foundation of China(41172184) ; National Natural Foundation of China(41172184) ; German Academic Exchange Service (DAAD) ; German Academic Exchange Service (DAAD) ; DFG(RA 442/25) ; DFG(RA 442/25) ; (SINOPROBE-08-01) ; (SINOPROBE-08-01)
源URL[http://ir.iggcas.ac.cn/handle/132A11/87883]  
专题中国科学院地质与地球物理研究所
通讯作者Shi, Wei
作者单位1.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China
2.Chinese Acad Geol Sci, Beijing 100037, Peoples R China
3.Tech Univ Bergakad Freiberg, D-09599 Freiberg, Germany
4.Wuxi Res Inst Petr Geol, Wuxi 214151, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
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GB/T 7714
Shi, Wei,Dong, Shu-Wen,Ratschbacher, Lothar,et al. Meso-Cenozoic tectonic evolution of the Dangyang Basin, north-central Yangtze craton, central China[J]. INTERNATIONAL GEOLOGY REVIEW,2013,55(3):382-396.
APA Shi, Wei,Dong, Shu-Wen,Ratschbacher, Lothar,Tian, Mi,Li, Jian-Hua,&Wu, Guo-Li.(2013).Meso-Cenozoic tectonic evolution of the Dangyang Basin, north-central Yangtze craton, central China.INTERNATIONAL GEOLOGY REVIEW,55(3),382-396.
MLA Shi, Wei,et al."Meso-Cenozoic tectonic evolution of the Dangyang Basin, north-central Yangtze craton, central China".INTERNATIONAL GEOLOGY REVIEW 55.3(2013):382-396.

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来源:地质与地球物理研究所

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