Anisotropy of magnetic susceptibility of Eocene and Miocene sediments in the Qaidam Basin, Northwest China: Implication for Cenozoic tectonic transition and depocenter migration

Abstract The Cenozoic evolution of the Qaidam basin, especially its paleostress field, can provide a better understanding of the dynamistic process of the northern Tibetan Plateau. Under certain conditions, Anisotropy of Magnetic Susceptibility (AMS) holds great potential for investigating early tec...

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Bibliographic Details

Published in:	Geochemistry, Geophysics, Geosystems
Main Authors:	Xiangjiang Yu, Baochun Huang, Shuwei Guan, Suotang Fu, Feng Cheng, Xiang Cheng, Tuo Zhang, Zhaojie Guo
Format:	Article
Language:	English
Published:	Wiley 2014-06-01
Subjects:	anisotropy of magnetic susceptibility the Qaidam basin Cenozoic tectonic evolution deposition center migration paleostress field
Online Access:	https://doi.org/10.1002/2014GC005231