| 郯庐断裂皖中段的韧性活动特征 |
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| 引用本文： | 许卫,童劲松.郯庐断裂皖中段的韧性活动特征[J].安徽地质,1999(1). |
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| 作者姓名： | 许卫 童劲松 |
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| 作者单位： | 安徽省地质调查院!合肥２３０００１ |
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| 摘 要： | 揭示了皖中浮槎山地区郯庐断裂的韧性活动以产生大规模的韧性剪切带为特征，构造岩为各类糜棱岩，并造成浮槎山的变质变形地质休呈由剪切带围限的透镜状夹块格局，为带逆冲性质的左行平移剪切，形成时代为Ｊ１－２
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| 关 键 词： | 平移 韧性活动 郯庐断裂 |
THE DUCTILE MOBILITY CHARACTERISTICS OF THE TAN-LU FAULT IN THE MIDDLE OF ANHUI |
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| Xu Wei,Tong Jinsong.THE DUCTILE MOBILITY CHARACTERISTICS OF THE TAN-LU FAULT IN THE MIDDLE OF ANHUI[J].Geology of Anhui,1999(1). |
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| Authors: | Xu Wei Tong Jinsong |
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| Abstract: | It has been disclosed that the ductile mobility of the Tan - Lu Fault in the Fuchashan area of middle of Anhui is characterizedby its product of large - scaled ductile shear zones and the tectonites of variety of myonites. As a result, the metamorphosed and deformed geological bodies in the Fuchashan area is in a framework of lenticular horses confined by shear zones typical of left - handed strike - slipshearing that formed in the early to middle Jurassic. |
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| Keywords: | strike - slip Tan - Lu Fault ductile mobility |
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