Is the Jurassic (Yanshanian) intraplate tectonics of North China due to westward indentation of the North China block?

doi:10.1111/ter.12002

	Is the Jurassic (Yanshanian) intraplate tectonics of North China due to westward indentation of the North China block?
	Faure, Michel 1; Lin, Wei 2; Chen, Yan 1
刊名	TERRA NOVA
	2012-12-01
卷号	24 期号:6 页码:456-466
ISSN号	0954-4879
DOI	10.1111/ter.12002
文献子类	Article
英文摘要	The northern mountains of Beijing are the type locality of the Mesozoic Yanshanian orogen. Our structural study emphasizes the importance of dextral strike-slip for the formation of this intracontinental belt. The South- and North-directed thrusts are positive flower structures rooted in strike-slip faults. This transpressional tectonics developed from Late Triassic to Late Jurassic-Early Cretaceous through three deformation phases coeval with syntectonic sedimentation, separated by two transtensional episodes coeval with magmatism. The Late JurassicEarly Cretaceous tectonic event is also recognized in several places of North China. Strike-slip faulting controls the deformation of the northern border of the North China block in the Yanshan-Yinshan belt. Simultaneously, East-directed thrusts and folds develop along N-S elongated ranges in Helanshan, Shanxi highlands and Taihangshan. The Jurassic tectonics of the North China Block is interpreted in a unitary way as the result of the westward underthrusting of the North China block below the Alashan block.
WOS关键词	LU FAULT ZONE ; METAMORPHIC CORE COMPLEX ; MESOZOIC EXTENSIONAL TECTONICS ; INNER-MONGOLIA ; THRUST BELT ; DAQING SHAN ; HENGSHAN-WUTAISHAN ; ANHUI PROVINCE ; YINSHAN BELT ; EASTERN ASIA
WOS研究方向	Geology
语种	英语
出版者	WILEY-BLACKWELL
WOS记录号	WOS:000310791400004
资助机构	NSFC(40872142) ; NSFC(40872142) ; Chinese National 973 Project(2009CB825008) ; Chinese National 973 Project(2009CB825008) ; NSFC(40872142) ; NSFC(40872142) ; Chinese National 973 Project(2009CB825008) ; Chinese National 973 Project(2009CB825008) ; NSFC(40872142) ; NSFC(40872142) ; Chinese National 973 Project(2009CB825008) ; Chinese National 973 Project(2009CB825008) ; NSFC(40872142) ; NSFC(40872142) ; Chinese National 973 Project(2009CB825008) ; Chinese National 973 Project(2009CB825008)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/84372]
专题	中国科学院地质与地球物理研究所
通讯作者	Faure, Michel
作者单位	1.Univ Orleans, Inst Sci Terre Orleans, UMR 7327, F-45071 Orleans 2, France 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Faure, Michel,Lin, Wei,Chen, Yan. Is the Jurassic (Yanshanian) intraplate tectonics of North China due to westward indentation of the North China block?[J]. TERRA NOVA,2012,24(6):456-466.
APA	Faure, Michel,Lin, Wei,&Chen, Yan.(2012).Is the Jurassic (Yanshanian) intraplate tectonics of North China due to westward indentation of the North China block?.TERRA NOVA,24(6),456-466.
MLA	Faure, Michel,et al."Is the Jurassic (Yanshanian) intraplate tectonics of North China due to westward indentation of the North China block?".TERRA NOVA 24.6(2012):456-466.