ANATEXIS

作品数:22被引量:231H指数:7
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相关领域:天文地球更多>>
相关作者:刘勇胜高山赵磊张西平更多>>
相关机构:中国地质大学朝鲜国家科学院中国地质科学院中国科学院更多>>
相关期刊:《Natural Science》《Acta Geologica Sinica(English Edition)》《Science China Earth Sciences》《Geoscience Frontiers》更多>>
相关基金:国家自然科学基金国家重点基础研究发展计划更多>>
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Early Oligocene anatexis in the Yardoi gneiss dome,southern Tibet and geological implications被引量:69
《Chinese Science Bulletin》2009年第1期104-112,共9页ZENG LingSen LIU Jing GAO LiE XIE KeJia WEN Li 
Supported by National Natural Science Foundation of China (Grant No.40673027);the Outlay Research Fund of Chinese Academy of Geological Sciences (Grant No.20071120101125);the Hundred Talent Program of Chinese Academy of Sciences
The Yardoi gneiss dome is located to the easternmost of the North Himalayan Gneiss Dome (NHGD),southern Tibet. It consists of metapelite,garnet amphibolite,granite and leucogranite,and is a key subject to constrain th...
关键词:地球 渐新世 变泥质岩 地壳深熔作用 喜马拉雅山 
Geological and chronological evidence of Indo-Chinese strike-slip movement in the Altyn Tagh fault zone被引量:20
《Chinese Science Bulletin》2002年第1期27-32,共6页LI Haibing YANG Jingsui XU Zhiqin WU Cailai WAN Yusheng SHI Rendeng Juhn G.Liou P.Tapponnier Trevor R.Ireland 
The work was supported by the National Key Basic Research Project (Grant No. G1998040800) ; Sino-France Collaborative Project of "Altun Shan-Qilianshan" Tectonic Evolution and Lithosphere Shearing.
A set of granitic and amphibole mylonite are exposed in the Altyn Tagh fault zone. The preliminary study shows that these rocks are the product of the syntectonic anatexis in the process of the left-lat- eral strike-s...
关键词:Altyn Tagh fault zone SYNTECTONIC ANATEXIS MYLONITE zircon directional spread U-Pb SHRIMP age AR-AR age. 
Experimental study on dehydration melting of natural biotite-plagioclase gneiss from High Himalayas and implications for Himalayan crust anatexis被引量:29
《Chinese Science Bulletin》2001年第10期867-872,共6页YANG Xiaosong JIN Zhenmin Ernst Huenges Frank R.Schilling Bernd Wunder 
This work was sponsored by the State Key Basic Research and Development Program of China (Grant No. G1998040800); GeoForschungsZentrum in Germany for International Cooperation and the Foundation of the Opened Laboratory of Constitution; Interaction and
Here we present the results of dehydration melting, melt morphology and fluid migration based on the dehydration melting experiments on natural bio-tite-plagioclase gneiss performed at the pressure of 1.0-1.4 GPa, and...
关键词:GNEISS dehydration melting melt topology fluid migration LEUCOGRANITE granulite Himalayas. 
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