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《Journal of Jilin University(Earth Science Edition)》 2009-04
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Evolution of Deformation and Metamorphism During the Tectono Emplacement of the Granulite in the Middle Himalaya Orogen

LIU De-min,LI De-wei,FAN Xu-guang,LIAO Qun-anFacutty of Earth Sciences,China University of Geosciences,Wuhan 430074,China  
In the middle section of the Himalaya belt,lenticular or pudding granulites are exposed intermittently in some weak strained areas,while the country rocks have been strongly deformed,as indicated by their mylonite foliations and schistosity.Due to the strongly ductile shear deformation and obviously controlled by the ductile shear zone,some mylonite occurs with the characteristics as shear lens shaped,stripy distributing and local concentrating.The granulite can be sorted into four types according to the mineral assemblage,and among which,the primary minerals such as orthopyroxene,clinopyroxene,plagioclase,hornblende and garnet show the characteristics of kinked,flatten,elongating,subgrain,marginal dynamic recrystallization and other strongly plastic deformation micro-structures.The study make it clear that the output of here granulite has relationship with the intrusion of the remelting granite and the movement of the STDS.So it can be considered that during the continental dynamic course of Absolutely-temperature and dropping-pressure when Himalaya orogenic belt fast uplifting and orogen,the lower crust basic granulite quickly move up to the earth's surface,as the same time,the lower crust laminar flow and the action of orogenic belt uplifting-detachment-orogen leads to the granulite facies metamorphism.
【Fund】: 国家自然科学基金项目(40572113);; 国家重点基础研究发展计划“973”项目前期研究专项(2005CCA05600);; 中国地调局区域地质调查项目(20001300009231);; 中国地质大学优秀青年教师资助计划项目(CUGQL0612)
【CateGory Index】: P542.2
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