The collision-related structures revealed in the northern Tarim Basin and their geological significance

doi:10.1002/gj.3561

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 岩石圈演化国家重点实验室

	The collision-related structures revealed in the northern Tarim Basin and their geological significance
	Wen, Lei 1; Li, Cheng 2; Li, Hong-Hui 3; Liu, Ya-Lei 1; Li, Yue-Jun 4; Zhao, Yan 5; Sun, Xiang-Can 1; Huang, Tong-Fei 3; Zhao, Tian-Yu 5; Gao, Yan-Yan 5
刊名	GEOLOGICAL JOURNAL
	2019-07-10
页码	16
关键词	Central Asian Orogenic Belt (CAOB) end Permian-Triassic thrust Jurassic-Cretaceous normal fault regional extension structure South Tianshan syn-collision structure
ISSN号	0072-1050
DOI	10.1002/gj.3561
英文摘要	The South Tianshan on the southern margin of the Central Asian Orogenic Belt (CAOB) is a collisional orogenic belt between the Tarim continent and Ili-Central Tianshan volcanic arc. The initial time of the collision remains debated, with proposed timing from Early Devonian to Middle Triassic. Almost all the previous studies on this collision were carried out within the South Tianshan Mountains, few within the related basins. End Permian-Triassic thrusts and Jurassic-Cretaceous normal faults were discovered in the northern Tarim Basin where is the southern piedmont of the South Tianshan Mountains after careful and systematic seismic interpretation. The end Permian-Triassic thrusts are constituted by both basement-involved and thin-skinned thrusts. They are likely seen as the syn-collision compressional structures of the South Tianshan collisional orogen. The syn-collision thrusts constitute the main faults in the study area. Consistent with the Triassic/Permian and Jurassic/Triassic unconformities, two thrusting phases occurred, at end Permian-beginning Triassic and end Triassic-beginning Jurassic, respectively. The Jurassic-Cretaceous normal faults usually arrange into stair-step or graben-horst structures in profile and en echelon normal fault zones horizontally. They are attributed as the results of the regional extensional stage in the CAOB. This regional extension stage provides a good constraint for the ending time of the collision between Tarim and Ili-Central Tianshan blocks. The normal faulting time is revealed by normal fault growth indexes. According to these observed syn-collision compressional and subsequent extension structures, it can be fairly inferred that the collision between Tarim and Ili-Central Tianshan was initiated at end Permian, lasted through the Triassic and ceased at end Triassic, and then evolved into the Jurassic-Cretaceous extensional tectonic stage.
资助项目	China Geological Survey Program[DD20160170] ; China Geological Survey Program[DD20160203] ; China Geological Survey Program[DD20190090] ; PetroChina Science and Technology Major Project[KT2018-02-01] ; National Science and Technology Major Project[2011ZX05028-003]
WOS关键词	CHINESE TIEN-SHAN ; PALEOZOIC TECTONIC EVOLUTION ; FOLD-THRUST BELT ; NW CHINA ; SOUTH TIANSHAN ; EXTENSIONAL STRUCTURES ; RADIOLARIAN FOSSILS ; PRESSURE GRANULITE ; MOUNTAINS ; ACCRETION
WOS研究方向	Geology
语种	英语
出版者	WILEY
WOS记录号	WOS:000477351800001
资助机构	China Geological Survey Program ; China Geological Survey Program ; PetroChina Science and Technology Major Project ; PetroChina Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; China Geological Survey Program ; China Geological Survey Program ; PetroChina Science and Technology Major Project ; PetroChina Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; China Geological Survey Program ; China Geological Survey Program ; PetroChina Science and Technology Major Project ; PetroChina Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project ; China Geological Survey Program ; China Geological Survey Program ; PetroChina Science and Technology Major Project ; PetroChina Science and Technology Major Project ; National Science and Technology Major Project ; National Science and Technology Major Project
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/92947]
专题	地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者	Li, Yue-Jun
作者单位	1.China Geol Survey, Oil & Gas Survey, Beijing, Peoples R China 2.Kyung Hee Univ, Dept Geog, Seoul, South Korea 3.PetroChina, Res Inst Petr Explorat & Dev, Beijing, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 5.Kexin Petr Sci & Technol Serv Co Ltd, Korla, Peoples R China
推荐引用方式 GB/T 7714	Wen, Lei,Li, Cheng,Li, Hong-Hui,et al. The collision-related structures revealed in the northern Tarim Basin and their geological significance[J]. GEOLOGICAL JOURNAL,2019:16.
APA	Wen, Lei.,Li, Cheng.,Li, Hong-Hui.,Liu, Ya-Lei.,Li, Yue-Jun.,...&Shi, Bin.(2019).The collision-related structures revealed in the northern Tarim Basin and their geological significance.GEOLOGICAL JOURNAL,16.
MLA	Wen, Lei,et al."The collision-related structures revealed in the northern Tarim Basin and their geological significance".GEOLOGICAL JOURNAL (2019):16.