| 新疆尾亚韧性剪切带的基本特征及其意义 |
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| 引用本文： | 邵铁全,刘云焕,董玉书. 新疆尾亚韧性剪切带的基本特征及其意义[J]. 地球科学与环境学报, 2001, 23(4): 28-32 |
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| 作者姓名： | 邵铁全 刘云焕 董玉书 |
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| 作者单位： | 1. 长安大学
2. 甘肃成县地矿局 |
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| 摘 要： | 尾亚韧性剪切带形成于石炭纪晚期.根据其宏观变形构造、显微变形构造等变形特征,说明其经历了早期的推覆剪切和后期的右行推覆剪切两个主要演化阶段.对该区的构造演化及指导找矿增添了一点新的内容.
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| 关 键 词： | 尾亚韧性剪切带 变形构造 演化阶段 |
| 文章编号： | 1007-9955(2001)04-0028-05 |
| 修稿时间： | 2001-01-11 |
THE BASIC FEATURE OF WEIYA DUCTILE SHEAR ZONE,XINJIANG |
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| SHAO Tie quan ,LIU Yun huan ,DONG Yu shu. THE BASIC FEATURE OF WEIYA DUCTILE SHEAR ZONE,XINJIANG[J]. Journal of Earth Sciences and Environment, 2001, 23(4): 28-32 |
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| Authors: | SHAO Tie quan LIU Yun huan DONG Yu shu |
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| Affiliation: | SHAO Tie quan 1,LIU Yun huan 1,DONG Yu shu 2 |
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| Abstract: | The Weiya ductile shear zone formed in the last stage of Carboniferous Period.According to its macroscopic and microscopic deformation structures,it at least went through two main stages of evolution from the thrusting nappe shearing to dextral nappe shearing. This adds some new contents to researching the history of the structure evolution in the region as well as directing to find deposits. |
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| Keywords: | WeiYa ductile shear zone the deformation structure the evolution stage Xinjiang |
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