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    王小民, 夏木林, J.G.Liou. 1992: 中国东部的含科石英榴辉岩带的发现——郯庐断裂平移作用的证据. 地质通报, (1): 88-91.
    引用本文: 王小民, 夏木林, J.G.Liou. 1992: 中国东部的含科石英榴辉岩带的发现——郯庐断裂平移作用的证据. 地质通报, (1): 88-91.
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    WANG Xiao-min, XIA Mu-lin, J.G.Liou. 1992: THE DISCOVERY OF A COESITE-BEARING ECLOGITE BELT IN EASTERN CHINA. Geological Bulletin of China, (1): 88-91.
    Citation: WANG Xiao-min, XIA Mu-lin, J.G.Liou. 1992: THE DISCOVERY OF A COESITE-BEARING ECLOGITE BELT IN EASTERN CHINA. Geological Bulletin of China, (1): 88-91.
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    中国东部的含科石英榴辉岩带的发现——郯庐断裂平移作用的证据

    THE DISCOVERY OF A COESITE-BEARING ECLOGITE BELT IN EASTERN CHINA

      摘要
    • 摘要: 根据近年来在中朝板块与扬子板块碰撞带上,所发现的科石英或含科石英假象的榴辉岩,推测中国东部的郯庐断裂的左行平移幅度可达550km,活动时代在中生代之后。

       

      Abstract: According to the coesite-and coesite pseudomorph-bearing eclogite belt discovered recently in a collision zone between the Sino-Korean and Yang- tze plates,it is inferred that the amplitude of the sinistral strike-slip dis- placement of the Tancheng-Lujiang fault in eastern China may attain 550 km and that its movement took place after the Mesozoic.

       

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