Zircon SHRIMP U-Pb Dating and Neoproterozoic Metamorphism of Kangding and Yuanmou Intrusive Complexes,Sichuan and Yunnan

被引：0

作者：

李大鹏 ^{[1
]}

陈岳龙 ^{[1
]}

罗照华 ^{[1
]}

赵俊香 ^{[2
]}

机构：

[1] School of the Earth Sciences and Resources, China University of Geosciences

[2] Institute of Crustal Dynamics, China Earthquake Administration

来源：

Journal of Earth Science | 2009年 / 20卷 / 06期

基金：

中国国家自然科学基金;

关键词：

Yangtze craton; Kangding-Yuanmou complex; SHRIMP; metamorphic history;

D O I：

暂无

中图分类号：

P597.3 [];

学科分类号：

070902 ;

摘要：

To clarify the relationship of the metamorphic intrusions along the west margin of the Yangtze craton and their metamorphic history after crystallization, the petrochemical and trace element geochemical characters, zircon SHRIMP U-Pb dating, and the chemical compositions of coexisting hornblendes and plagioclases from Neoproterozoic metamorphic intrusions in Kangding (康定), Sichuan (四川) Province, and Yuanmou (元谋), Yunnan (云南) Province, were studied. Combined with the former published data, it is indicated that the Kangding granitic plutons and Yuanmou complex in the west margin of the Yangtze craton generally formed at the same period. Metamorphic event at ~700 Ma existed extensively, at least covering from Kangding area in Sichuan to the Eshan (峨山) area in Central Yunnan. Moreover, amphibolite facies may represent the peak regional metamorphic condition.

引用

页码：897 / 908

页数：12

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