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Oroclinal bending and block rotations in South China since the Mesozoic——Geological and paleomagnetic evidence

Oroclinal bending and block rotations in South China since the Mesozoic——Geological and paleomagnetic evidence

作     者:LI Zhengxiang, FANG Dajun, Christopher McA. Powell and LOU Gang1. Department of Geology and Geophysics, The University of Western Australia, Nedlands WA 6907, Australia 2. Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China 

作者机构:Department of Geology and Geophysics The University of Western Australia Nedlands Australia Department of Earth Sciences Zhejiang University Hangzhou China 

出 版 物:《Chinese Science Bulletin》 (科学通报(英文版))

年 卷 期:1997年第42卷第2期

页      面:132-136页

核心收录:

学科分类:070903[理学-古生物学与地层学(含:古人类学)] 0709[理学-地质学] 07[理学] 

主  题:Mesozoic paleomagnetism block rotation. 

摘      要:THE South China Block exhibits a complex structural pattern in its Neoproterozoic-Mesozoic sedimentary cover. The lack of knowledge about the formation of this pattern hinders our understanding of the regional tectonic evolution and paleogeography, and the reconstruction of Phanerozoic apparent polar wander path(s). In this note we present a synthesis based on a paleomagnetic and tectonic analysis, which suggests that (i) the structural pattern over

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