Formation of the Moping Dome in the Xuefengshan Orocline, Central China and its Tectonic Significance
Shi Wei1,2; Dong Shuwen3; Li Jianhua1; Tian Mi1,4; Wu Guoli1,5
刊名ACTA GEOLOGICA SINICA-ENGLISH EDITION
2013-06-01
卷号87期号:3页码:720-729
关键词Xuefengshan Orocline Moping Dome Superposed Structure Paleo-stress Field Intracontinental Orogeny
DOI10.1111/1755-6724.12083
文献子类Article
英文摘要Many equiaxial dome-like structures developed in the north segment of the Xuefengshan orocline, Central China are obviously inconcordant with the NE-trending linear structures in this area, which contain important records for understanding the structural framework and evolution of this belt. In this paper, taking one of the typical dome-like structures in the Xuefengshan orcline (e.g. Moping dome-like structure) as an example, based on its structural framework interpratatoin, superposed deformation analysis and paleo-stress fields reconstruction, we propose the Moping dome-like structure is composed of two populations of different-striking thrust-fold structures, similar to E-trending and NE-striking structures, indicative of two-stages shortening, similar to N- and NW-striking, respectively. Together with the geochronological analysis, we suggest the first stage of shortening occurred in Late Triassic to Early Jurassic, due to the Indosinian intercollisional orogeny of the Yangtze Block and the North China Block The second occurred during Late Jurassic-Early Cretaceous owing to Yanshanian intracontinental orogeny, leading to the intensive superposition of the NE-trending structures onto the similar to E-trending structures, and the final ocurrence of the Moping dome. Thus, our study indicates the Xuefengshan arc-shape belt also experienced two-phase deformation, and resulted from the superposition of NE-SW structures onto similar to E-W structures in Late Jurassic-Early Cretaceous, which could provide new structural evidence for probing the Mesozoic tectonic framework and evolution of the Xuefengshan orocline.
WOS关键词SOUTH CHINA ; PALEOMAGNETIC CONSTRAINTS ; YANGTZE BLOCK ; SICHUAN BASIN ; NORTH CHINA ; MIANLUE SUTURE ; HUNAN PROVINCE ; JURASSIC ROCKS ; DABIE OROGEN ; THRUST BELT
WOS研究方向Geology
语种英语
WOS记录号WOS:000321845300009
资助机构National Natural Foundation of China(41172184) ; National Natural Foundation of China(41172184) ; Institute of Geomechanics Foundation(DZLXJK200715) ; Institute of Geomechanics Foundation(DZLXJK200715) ; (SINOPROBE-08-01) ; (SINOPROBE-08-01) ; National Natural Foundation of China(41172184) ; National Natural Foundation of China(41172184) ; Institute of Geomechanics Foundation(DZLXJK200715) ; Institute of Geomechanics Foundation(DZLXJK200715) ; (SINOPROBE-08-01) ; (SINOPROBE-08-01)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/62643]  
专题地质与地球物理研究所_特提斯研究中心
作者单位1.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China
2.Minist Land & Resources, Key Lab Neotecton Movement & Geohazard, Beijing 100081, Peoples R China
3.Chinese Acad Geol Sci, Beijing 100037, Peoples R China
4.SINOPEC, Wuxi Res Inst Petr Geol, Wuxi 214151, Jiangsu, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
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Shi Wei,Dong Shuwen,Li Jianhua,et al. Formation of the Moping Dome in the Xuefengshan Orocline, Central China and its Tectonic Significance[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2013,87(3):720-729.
APA Shi Wei,Dong Shuwen,Li Jianhua,Tian Mi,&Wu Guoli.(2013).Formation of the Moping Dome in the Xuefengshan Orocline, Central China and its Tectonic Significance.ACTA GEOLOGICA SINICA-ENGLISH EDITION,87(3),720-729.
MLA Shi Wei,et al."Formation of the Moping Dome in the Xuefengshan Orocline, Central China and its Tectonic Significance".ACTA GEOLOGICA SINICA-ENGLISH EDITION 87.3(2013):720-729.
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