Formation of the Moping Dome in the Xuefengshan Orocline, Central China;and its Tectonic Significance

doi:10.1111/1755-6724.12083

CORC > 中国地质调查局 > 中国地质调查局 > 中国地质科学院地质力学研究所

	Formation of the Moping Dome in the Xuefengshan Orocline, Central China;and its Tectonic Significance
	Shi Wei 1; Dong Shuwen 2; Li Jianhua ; Tian Mi 3; Wu Guoli 4
刊名	ACTA GEOLOGICA SINICA-ENGLISH EDITION
	2013
卷号	87 期号:3 页码:720-729
关键词	Xuefengshan orocline Moping dome superposed structure paleo-stress field intracontinental orogeny
ISSN号	1000-9515;EI 1755-6724
DOI	10.1111/1755-6724.12083
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.
学科主题	构造地质学
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
出版者	WILEY-BLACKWELL
WOS记录号	WOS:000321845300009
内容类型	期刊论文
源URL	[http://119.78.100.197/handle/2HKVOGP0/40209]
专题	中国地质科学院地质力学研究所
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 GB/T 7714	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.