ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
海南戈枕韧性剪切带微观构造研究
  
关键词:Gezhen shear zone mylonites  microstructure kinematics  dynamics
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作者单位
余凤鸣 宜昌地质矿产研究所 
刘国庆 宜昌地质矿产研究所 
何龙清 宜昌地质矿产研究所 
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摘要:
The Microstructore Study of the Gezhen Ductile Shear Zone, Hainan
      The Gezhen shear zone extends in NE-direction , occurring in the Middie Proterozoic Baoban Group. It was formed in the Hercynian-Indsinian, It was discovered by qualitative- quantitative inmicrocopic analysis, Its tectonics show complex zoning in composition beth in strike and dip. Themanner of movement is a reverse one in section but a sinistral shear one in plane, Totle shift isabout one kilometer. Deformations are devided into pure shear style in the Hongpumenling part andflaser style from Baoban to Beiniu and from Gongai to Bumo, Stress strain and lithofacies studieshave obviously showed the deformation of the Gezhen shear zone becomes much stronger from mar-gin to center and from the SW part to the NE part.
YU Feng-ming,LI Guo-qing,HE Long-qing.1995.The Microstructore Study of the Gezhen Ductile Shear Zone, Hainan[J].Acta Geoscientica Sinica,16(3):261-275.
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