BASIN EVOLUTION WITHIN AND ADJACENT TO THE TIEN-SHAN RANGE, NW CHINA

	BASIN EVOLUTION WITHIN AND ADJACENT TO THE TIEN-SHAN RANGE, NW CHINA
	ALLEN, MB ; WINDLEY, BF ; ZHANG, C ; ZHAO, ZY ; WANG, GR
刊名	JOURNAL OF THE GEOLOGICAL SOCIETY
	1991-03-01
卷号	148 页码:369-378
ISSN号	0016-7649
文献子类	Article
英文摘要	Two late Palaeozoic collisions produced the ancestral Tien Shan Range. Extension following the younger collision, preceded a phase of thermal subsidence associated with fluvial and lacustrine sedimentation throughout the Jurassic, Cretaceous and early Tertiary. This thermal subsidence was interrupted by renewed movement on Palaeozoic reverse faults, caused by the Mesozoic collisions at the southern margin of Asia. The India/Asia collision in the early Tertiary has produced widespread thrusting in the Tien Shan, which in turn is responsible for the formation of active foreland basins at the southern and northern margins of the range and similar basins within the range itself. This compression produced uplift and relief, and consequent erosion gave rise to alluvial fans, braidplains and ephemeral lakes in an extremely arid environment.
WOS关键词	GRAVITY-ANOMALIES ; NORTHWEST CHINA ; CENTRAL-ASIA ; TECTONIC EVOLUTION ; TARIM BASIN ; REGION ; TIBET ; PLATE ; EARTHQUAKES ; ACCRETION
WOS研究方向	Geology
语种	英语
出版者	GEOLOGICAL SOC PUBL HOUSE
WOS记录号	WOS:A1991HJ39100017
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/81404]
专题	中国科学院地质与地球物理研究所
作者单位	1.UNIV LEICESTER,DEPT GEOL,LEICESTER LE1 7RH,ENGLAND 2.CHINESE ACAD SCI,INST GEOL,BEIJING,PEOPLES R CHINA
推荐引用方式 GB/T 7714	ALLEN, MB,WINDLEY, BF,ZHANG, C,et al. BASIN EVOLUTION WITHIN AND ADJACENT TO THE TIEN-SHAN RANGE, NW CHINA[J]. JOURNAL OF THE GEOLOGICAL SOCIETY,1991,148:369-378.
APA	ALLEN, MB,WINDLEY, BF,ZHANG, C,ZHAO, ZY,&WANG, GR.(1991).BASIN EVOLUTION WITHIN AND ADJACENT TO THE TIEN-SHAN RANGE, NW CHINA.JOURNAL OF THE GEOLOGICAL SOCIETY,148,369-378.
MLA	ALLEN, MB,et al."BASIN EVOLUTION WITHIN AND ADJACENT TO THE TIEN-SHAN RANGE, NW CHINA".JOURNAL OF THE GEOLOGICAL SOCIETY 148(1991):369-378.