| 新疆觉罗塔格V型构造的厘定及其有序性 |
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| 引用本文： | 方茂龙,蔡文伯,孙文鹏,徐道一.新疆觉罗塔格V型构造的厘定及其有序性[J].铀矿地质,2005,21(6):331-337. |
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| 作者姓名： | 方茂龙 蔡文伯 孙文鹏 徐道一 |
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| 作者单位： | 1. 核工业北京地质研究院,北京,100029
2. 中国地震局地质研究所,北京,100029 |
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| 基金项目： | 国家自然科学基金(49672167)资助 |
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| 摘 要： | 本文通过对新疆觉罗塔格地区的卫星遥感图片判读和野外验证,认为该区近东西向弧形断裂带是在前中生代北西西和北东东向断裂格局基础上经有序演化而形成。近东西向、北西西和北东东向3组断裂构成V型构造,它是中生代以来近北西向构造应力作用的产物,并在新第三纪以后有强烈活动。该V型构造的形成,在时间上表现为有序过程,空间上表现为排列方式和演化方向等的有序性,是信息有序系列特性在断裂构造演化过程中的表征。
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| 关 键 词： | 觉罗塔格 V型构造 有序性 |
| 文章编号： | 1000-0658(2005)06-0331-07 |
| 收稿时间： | 02 10 2005 12:00AM |
| 修稿时间： | 2005年2月10日 |
The indentification of Jueluotage V- type structure in Xinjiang and its orderness |
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| FANG Mao-long,CAI Wen-bo,SUN Wen-peng,XU Dao-yi.The indentification of Jueluotage V- type structure in Xinjiang and its orderness[J].Uranium Geology,2005,21(6):331-337. |
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| Authors: | FANG Mao-long CAI Wen-bo SUN Wen-peng XU Dao-yi |
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| Institution: | 1. Beijing Research Institute of Uranium Geology, Beijing 100029, China; 2. Institute of Geology, CSB, Beijing 100029, China |
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| Abstract: | Based on the interpretation of satellite image and field checking in Jueluotage area,Xinjiang,it is thought that the sublatitudinal arc fault zones have been formed since Mesozoic through the evolution of the NWWtrending and NEEtrending faults occurring in preMesozoic time.These three sets of faults comprise the Jueluotage "Vtype structure" formed by the NWtrending structural stress field and drastically activated since Neocene.The Jueluotage Vtype structure is expressed in time as an ordered process,and in space as an ordered arrangement and an ordered evolution direction,and characterizes the Information Ordered Series(IOS) of the evolution process of fault structure. |
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| Keywords: | Jueluotage Vtype structure orderness |
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