Anatexis,Deformation and Exhumation Mechanism for UHP Metamorphic Rocks:A Case Study in the North Qaidam and South Altyn UHP Terrane,Western China

Objective In recent years,hydrous silicate melts by dehydrationdriven in situ partial melting constrained from experiments and natural rocks have been increasingly recognized in UHP rocks,indicating partial melting of UHP slab.Partial melting of UHP metamorphic rocks can dramatically affect the rheo...

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Veröffentlicht in:Acta geologica Sinica (Beijing) 2017-02, Vol.91 (1), p.361-362
Hauptverfasser: YU, Shengyao, ZHANG, Jianxin, LI, Sanzhong, PENG, Yinbiao, SUN, Deyou
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container_title Acta geologica Sinica (Beijing)
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creator YU, Shengyao
ZHANG, Jianxin
LI, Sanzhong
PENG, Yinbiao
SUN, Deyou
description Objective In recent years,hydrous silicate melts by dehydrationdriven in situ partial melting constrained from experiments and natural rocks have been increasingly recognized in UHP rocks,indicating partial melting of UHP slab.Partial melting of UHP metamorphic rocks can dramatically affect the rheology of deeply subducted crust and thus play a crucial role in accelerating the exhumation of UHP slabs.
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subjects 中国西部
变形
折返机制
柴达木盆地北缘
深熔作用
超高压变质岩石
超高压地体
阿尔金
title Anatexis,Deformation and Exhumation Mechanism for UHP Metamorphic Rocks:A Case Study in the North Qaidam and South Altyn UHP Terrane,Western China
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