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CHARACTERISTICS OF METAMORPHIC ROCKS AND DUCTILE SHEAR DEFORMATION IN WEIXI COUNTY,YUNNAN PROVINCE

Ma Guang

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Abstract

The original rock of Xuelongshan metamorphic rock series was formed in pre-Sinian Period and moderately-intensely metamorphosed.It is the crystalline basement of Lanping-Simao block.In the study area occur primary mylonite,mylonite and ultra-mylonite.The metamorphic belt can be divided into four ductile deformation phases,i.e.Jinning,Indosinian-Early Yanshanian,Late Yanshanian and Himalayan phases.

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What this paper is about

The original rock of Xuelongshan metamorphic rock series was formed in pre-Sinian Period and moderately-intensely metamorphosed.It is the crystalline basement of Lanping-Simao block.In the study area occur primary mylonite,mylonite and ultra-mylonite.The metamorphic belt can be divided into four ductile deformation phases,i.e.Jinning,Indosinian-Early Yanshanian,Late Yanshanian and Himalayan phases.

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Available abstract

The original rock of Xuelongshan metamorphic rock series was formed in pre-Sinian Period and moderately-intensely metamorphosed.It is the crystalline basement of Lanping-Simao block.In the study area occur primary mylonite,mylonite and ultra-mylonite.The metamorphic belt can be divided into four ductile deformation phases,i.e.Jinning,Indosinian-Early Yanshanian,Late Yanshanian and Himalayan phases.

Key concepts: Mylonite, Metamorphic rock, Geology, Shear zone, Basement, Deformation (meteorology), Shear (geology), Geochemistry

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CHARACTERISTICS OF METAMORPHIC ROCKS AND DUCTILE SHEAR DEFORMATION IN WEIXI COUNTY,YUNNAN PROVINCE — Research Paper | ScholarLens