Magnetic Petrology of Archean High-Grade Terrains: Window into Deep Crustal Structure and Geodynamic Processes  

Magnetic Petrology of Archean High Grade Terrains: Window into Deep Crustal Structure and Geodynamic Processes *

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作  者:Liu Qingsheng Department of Applied Geophysics, China University of Geosciences, Wuhan 430074 Gao Shan Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074 

出  处:《Journal of Earth Science》1998年第1期83-87,共5页地球科学学刊(英文版)

摘  要:The major results about magnetic petrology of Archearn high grade terrains in the world are reviewed in this article, focusing on the relationship between rock magnetism and deformation, and metamorphism and intensity of magnetization of the lower continental crust. The important problems about the magnetic study of rocks for high grade terrains are advanced.The major results about magnetic petrology of Archearn high grade terrains in the world are reviewed in this article, focusing on the relationship between rock magnetism and deformation, and metamorphism and intensity of magnetization of the lower continental crust. The important problems about the magnetic study of rocks for high grade terrains are advanced.

关 键 词:lower continental crust granulite facies terrain magnetic petrology. 

分 类 号:P584[天文地球—岩石学]

 

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