ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
豫南熊店高压变质岩的pttD轨迹
  
关键词:high-pressure metamorphic rocks  pttD path  Dabie Mountains
基金项目:国家自然科学基金
作者单位
张泽明 中国地质科学院地质研究所 
韦必则 中国地质大学地球科学学院 
韩郁菁 中国地质大学地球科学学院 
游振东 中国地质大学地球科学学院 
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摘要:
The pttD Path of High-Pressure Metamorphic Rocks of Xiongdian, Southern Henan
      The high-pressure metamorphic rock block of Xiongdian,Southern Henan,have been experienced 6 stages of deformation and metamorphism.They are from the ductile shear deformation and eclogite facies metamorphism under the compression dynamic mechanism at the lower crustal level,through the thrust nappe and epidote amphibolite facies metamorphism under a continuous compression mechanism at the medium crustal level,and the brittle_ductile deformation and greenschist facies metamorphism under the extension condition at the upper crust,to the brittle deformation and dynamic metamorphic rocks and their exhumation towards the upper crust derived from the ductile deformation under a continuous compression mechanism,whereas the expose of these rocks at surface fesulted from the extension and faulting.
ZHANG Ze-ming,WEI Bi-ze,HAN Yu-jing,YOU Zhen-dong.1998.The pttD Path of High-Pressure Metamorphic Rocks of Xiongdian, Southern Henan[J].Acta Geoscientica Sinica,19(3):233-237.
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