| 吐哈盆地南缘大草滩韧性剪切带的变形特征及演化 |
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| 引用本文： | 白明洲.吐哈盆地南缘大草滩韧性剪切带的变形特征及演化[J].新疆工学院学报,1997,18(3):231-234. |
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| 作者姓名： | 白明洲 |
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| 作者单位： | 新疆工学院地质系!乌鲁木齐，830008 |
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| 摘 要： | 大草滩韧性剪切带岩石变形特征明显，有从强到弱三个程度不同的变形带，它是从晚石炭世初至晚石炭世末期发展起来的，是准噶尔板块和塔里木板块相互作用的结果．
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| 关 键 词： | 大草滩韧性剪切带 岩石变形 构造演化 |
DEFORMATION CHARACTER AND EVOLUTION OF DACAOTAN DUCTILE SHEAR ZONE ON THE SOUTH MARGIN OF TUHA BASIN |
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| Authors: | Bai Mingzhou |
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| Affiliation: | Dept. of Geology Urumqi 830008 |
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| Abstract: | The character of the rock deformation in Dacaotan ductile shear zone is obvious. Thereare three deformation zones. Dacootan ductile shear zone developed during the late Carbonif-erous period and it's the result of the mutual action between Tarim plate and Junggar plate. |
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| Keywords: | Ductile shear zone Rock deformation Structural evolution |
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