| 武当地块中的走滑韧性剪切带初步研究 |
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| 引用本文： | 周小虎,周鼎武.武当地块中的走滑韧性剪切带初步研究[J].西北大学学报,1999,29(3):241-245. |
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| 作者姓名： | 周小虎 周鼎武 |
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| 作者单位： | 西北大学地质学系 |
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| 摘 要： | 从基性岩墙群区域形态差异、韧性剪切带产状特点、构造岩类型与矿物变形特征、区域褶皱样式差异等方面初步论证了走滑韧性剪切带的存在。认为南秦岭武当地区的构造格局不是前人认定的以推覆构造为主，而确实有走滑韧性剪切带存在。
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| 关 键 词： | 走滑韧性剪切带 武当地块 南秦岭 |
| 文章编号： | 1000-274X(1999)03-0241-05 |
| 修稿时间： | 1998年10月9日 |
A Primary research of strike-slip ductile shear zone in Wudang Block |
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| ZHOU Xiao-hu,ZHOU Ding-wu.A Primary research of strike-slip ductile shear zone in Wudang Block[J].Journal of Northwest University(Natural Science Edition),1999,29(3):241-245. |
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| Authors: | ZHOU Xiao-hu ZHOU Ding-wu |
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| Abstract: | A new opinion is demonstrated from those aspects:the different shape of basic dyke in Wudang Area ;the schistosity zone;the mineral deformation feature of the ductile shear zone,the different style of the fold ,etc.The existence of the strike slip ductile zone shows that the forming of the framework in South Qinling is worked by nappe tectonics and strike slip ductile zone together, not worked by nappe tectonics only. |
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| Keywords: | strike slip ductile shear belt Wudang Block South Qinling |
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