The Bogeda Shan uplifting: Evidence from multiple phases of deformation

doi:10.1016/j.jseaes.2014.12.006

	The Bogeda Shan uplifting: Evidence from multiple phases of deformation
	Chen, Ke 1; Lin, Wei 2; Wang, Qingchen 2
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2015-03-01
卷号	99 页码:1-12
关键词	The Bogeda Shan Fold-and-thrust belt Multiple phases of deformation Compressional tectonics Structural analysis
ISSN号	1367-9120
DOI	10.1016/j.jseaes.2014.12.006
文献子类	Article
英文摘要	The current topography of Central Asia is considered to have resulted from crustal shortening related to the ongoing India-Asia collision that started in the Early Tertiary period. The Bogeda Shan, a northeastern branch of the Tian Shan located in northwest China, has several summits higher than 5000 m. The northern piedmont of the Bogeda Shan exhibits remarkable deformation features that remain poorly studied. This study documents three phases of tectonic deformation in the Bogeda Shan that are related to the far-field effects of collisions along the southern Eurasian margin. Detailed field observations show that the intensively folded Upper Permian strata are covered by a subhorizontal Lower Jurassic layer, thus indicating a Triassic tectonic event that is probably related to the onset of the uplift in the Bogeda Shan during a Cimmerian orogenic episode (D-1). A seismic profile suggests that this deformation episode was followed by the Late Jurassic-Early Cretaceous deformation (D-2), which is characterized by wide wavelength folds overlaid by undeformed Cretaceous layers. Cenozoic thrusts were also observed in the northern piedmont of the Bogeda Shan (D-3). This study demonstrates that the onset of uplift in the Bogeda Shan began in the Early Mesozoic and separated the Turfan-Hami Basin from the Junggar Basin. A new tectonic evolution model of the Bogeda Shan was reconstructed by these three tectonic phases. This work indicates that the current topography of the Bogeda Shan and its surrounding area was the result of multiple phases of deformation related to successive collisions at the southern Eurasian margin. (C) 2014 Elsevier Ltd. All rights reserved.
WOS关键词	CHINESE TIEN-SHAN ; FISSION-TRACK THERMOCHRONOLOGY ; CENOZOIC TECTONIC EVOLUTION ; EASTERN TIBETAN PLATEAU ; SOUTHWEST TARIM BASIN ; MONGOL-OKHOTSK OCEAN ; INDIA-ASIA COLLISION ; TURPAN-HAMI BASIN ; NORTHWEST CHINA ; TIAN-SHAN
WOS研究方向	Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000349880800001
资助机构	NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; 41472193) ; 41472193) ; 41472193) ; 41472193) ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; 41472193) ; 41472193) ; 41472193) ; 41472193) ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; 41472193) ; 41472193) ; 41472193) ; 41472193) ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; NSFC(41225009 ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; Major State Basic Research Development Program of China(2009CB825008) ; 41472193) ; 41472193) ; 41472193) ; 41472193)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/86904]
专题	中国科学院地质与地球物理研究所
通讯作者	Lin, Wei
作者单位	1.China Geol Survey, Oil & Gas Survey, Beijing 100029, Peoples R China 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	Chen, Ke,Lin, Wei,Wang, Qingchen. The Bogeda Shan uplifting: Evidence from multiple phases of deformation[J]. JOURNAL OF ASIAN EARTH SCIENCES,2015,99:1-12.
APA	Chen, Ke,Lin, Wei,&Wang, Qingchen.(2015).The Bogeda Shan uplifting: Evidence from multiple phases of deformation.JOURNAL OF ASIAN EARTH SCIENCES,99,1-12.
MLA	Chen, Ke,et al."The Bogeda Shan uplifting: Evidence from multiple phases of deformation".JOURNAL OF ASIAN EARTH SCIENCES 99(2015):1-12.