中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Tectonic evolution of the Dabieshan orogen: In the view from polyphase deformation of the Beihuaiyang metamorphic zone

文献类型:期刊论文

作者Lin, W; Michel, F; Wang, QC; Nicolas, A
刊名SCIENCE IN CHINA SERIES D-EARTH SCIENCES
出版日期2005-07-01
卷号48期号:7页码:886-899
关键词Beihuaiyang Metamorphic Zone Geometry Kinematic Polyphase Deformation Tectonic Evolution
ISSN号1006-9313
DOI10.1360/03yd0306
文献子类Article
英文摘要The Beihuaiyang metamorphic zone was formed by the Early Mesozoic collision of the North and South China Blocks. It consisted of the Foziling and Luzhenguan complexes and was thought to have never afforded a deep subduction. A similar feature of the deformation in the Dabieshan UHP metamorphic rocks implies that these different tectonic units share the same geodynamic background. The early stage of deformation can be preserved on account of their relatively shallower subduction than that for UHP rocks. On the basis of an analysis of the geological structure and geochronological results, five deformational stages have been recognized: a D(1)-Early compressional deformation which represents the continental subduction; a D(2)-Early exhumation deformation producing a syn-convergence exhumation; a D(3)-Main deformation, represented by an exhumation deformation with Late Triassic age; a D(4)-Doming and its margin extensional gravity collapse deformation and finally a D(5)-regional extensional deformation of Cretaceous that was mostly introduced by the migmatization and plutonism.
WOS关键词CENTRAL CHINA ; EASTERN CHINA ; SOUTH CHINA ; JIANGXI PROVINCE ; COOLING HISTORY ; PRESSURE ROCKS ; SHAN ; NORTH ; GEOCHRONOLOGY ; CONSTRAINTS
WOS研究方向Geology
语种英语
WOS记录号WOS:000230546300004
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/65738]  
专题中国科学院地质与地球物理研究所
通讯作者Lin, W
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, LTE, Beijing 100029, Peoples R China
2.Nagoya Univ, Grad Sch Sci, Dept Earth & Planetary Sci, Nagoya, Aichi, Japan
3.Univ Orleans, CNRS, UMR 6113, ISTO, F-45067 Orleans, France
4.UMR 6524 Magmas & Volcans, F-63000 Clermont Ferrand, France
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Lin, W,Michel, F,Wang, QC,et al. Tectonic evolution of the Dabieshan orogen: In the view from polyphase deformation of the Beihuaiyang metamorphic zone[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2005,48(7):886-899.
APA Lin, W,Michel, F,Wang, QC,&Nicolas, A.(2005).Tectonic evolution of the Dabieshan orogen: In the view from polyphase deformation of the Beihuaiyang metamorphic zone.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,48(7),886-899.
MLA Lin, W,et al."Tectonic evolution of the Dabieshan orogen: In the view from polyphase deformation of the Beihuaiyang metamorphic zone".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 48.7(2005):886-899.

入库方式: OAI收割

来源:地质与地球物理研究所

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