裴放. 1995: 河南南召地区韧性剪切带及构造变形相. 地质通报, (4).
    引用本文: 裴放. 1995: 河南南召地区韧性剪切带及构造变形相. 地质通报, (4).
    PEI Fang. 1995: DUCTILE SHEAR BELTS AND TECTONIC DEFORMATION FACIES IN THE NANZHAO AREA,HENAN. Geological Bulletin of China, (4).
    Citation: PEI Fang. 1995: DUCTILE SHEAR BELTS AND TECTONIC DEFORMATION FACIES IN THE NANZHAO AREA,HENAN. Geological Bulletin of China, (4).

    河南南召地区韧性剪切带及构造变形相

    DUCTILE SHEAR BELTS AND TECTONIC DEFORMATION FACIES IN THE NANZHAO AREA,HENAN

    • 摘要: 磨坪-维摩寺、下浦池-郭沟和三道岗-小罗沟三条韧性剪切带的形成与活动,影响并决定了它们所分隔的四个构造变形域和变形带的构造变形,导致地壳压缩,最终奠定了复杂的构造格局,并形成脆裂剪切、弯曲滑动、固态流变和柔流或熔融四种构造变形相。

       

      Abstract: The formation and activity of the Moping-Weimosi,Xiapuchi-Guogou and Sandaogang-Xiaoluogou ductile shear belts affected and determined the tectonic deformation of four tec-tonic deformation domains and belts separated by them,thus leading to crustal shortening,fi-nally laying the foundation of the complex tectonic framework and forming four tectonic defor-mation facies,i.e. brittle shear,flexural slope,solid-state rheomorphism and plastic flow or fu-sion.

       

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