中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Rejuvenation of fossil sutures and related mesozoic intracontinental orogenies in South China

文献类型:期刊论文

作者Wu, GY
刊名ACTA GEOLOGICA SINICA-ENGLISH EDITION
出版日期2000
卷号74期号:2页码:194-200
关键词intracontinental orogeny rejuvenation of fossil sutures Yanshanides Indosinides South China
ISSN号1000-9515
英文摘要The Huanan (South China) subcontinent was created by amalgamation of the Yangtze, Xianggan, Cathaysia and Zhemin microcontinents by the Guangxi orogeny in the Early Palaeozoic. The closure of the Tethyan Ocean and subsequent collision event outside the amalgamated continent reactivated fossil sutures and resulted in intracontinental (ensialic) orogenies in the Mesozoic. Based on evidence from deformation, molasse and granitoids, the Sichuan-Guizhou-Hunan-southem Hubei and Hunan-Jiangxi-Fujian Yanshanian fold-thrust systems and the Lower Yangtze-northwestern Fujian Indosinian fold-thrust system are thought to be intracontinental orogens. Their main features are as follows: intracontinental orogenies occurred areally, thrusting propagated towards the interior of the continental, they extend parallelly to the strikes of the fossil sutures, and the details of the temporal-spatial evolution of the orogens depend on subduction-collision events.
语种英语
WOS记录号WOS:000088935900013
出版者GEOLOGICAL SOC CHINA
源URL[http://ir.iggcas.ac.cn/handle/132A11/75895]  
专题中国科学院地质与地球物理研究所
通讯作者Wu, GY
作者单位Chinese Acad Sci, Inst Geol, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Wu, GY. Rejuvenation of fossil sutures and related mesozoic intracontinental orogenies in South China[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2000,74(2):194-200.
APA Wu, GY.(2000).Rejuvenation of fossil sutures and related mesozoic intracontinental orogenies in South China.ACTA GEOLOGICA SINICA-ENGLISH EDITION,74(2),194-200.
MLA Wu, GY."Rejuvenation of fossil sutures and related mesozoic intracontinental orogenies in South China".ACTA GEOLOGICA SINICA-ENGLISH EDITION 74.2(2000):194-200.

入库方式: OAI收割

来源:地质与地球物理研究所

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