ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
中国桐柏大别构造带变质演化的岩石学证迹
  
关键词:Tongbai-Dabie tectonic belt  metamorphic and deformational history  PTt path  post orogenic uplift  reequilibrium texture
基金项目:本文是国家自然科学基金重大项目49290100和面上项目49172090和国家计委国土司30届国际地质大会96-30-07专项成果之一,成文过程中与索书田、韩郁善、桑隆康、钟增球等进行了有益交流
作者单位
游振东 中国地质大学武汉 
陈能松 中国地质大学武汉 
张泽明 中国地质大学武汉 
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摘要:
The Petrology Evidence of Metamorphic Evolution in Tongbai-Dabie Tectonic Belt
      Tongbai-Dabie tectonic belt, eastern extension of Qinling orogenic belt, experi-enced multistage evolutions under different tectonic regimes. The present Tongbai-Dabie area is composed of a collage of metamorphic terranes. The faults of ductile shear zones delimit these metamorphic terranes. Although each terrane has its own metamorphic and deformational history and unique PTt path, All terrane undergo common postorogenic up-lift in collison orogenic belt. The paper presents the features of retrogressive metamorphism reeguilibrinm textures from coesite eclogite, kyanite gedrite schist and hypersthene garnet biotite gneiss in Suixi-an Group, Hongan Guroup and Dabie complex. Recent zircon U-Pb dating of the granulitic rock is 1699±128Ma Reequilbrium textures in above rocks suggest a prominant post orogenic uplift in the Tongbai-Dabie tectonic-metamorphic belt.
You Zhendong,Chen Nengsong,Zhang Zeming.1996.The Petrology Evidence of Metamorphic Evolution in Tongbai-Dabie Tectonic Belt[J].Acta Geoscientica Sinica,17(z1):16-22.
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