| 库车坳陷深浅构造变形与地震关系浅析 |
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| 引用本文： | 刘洁,曲国胜,童晓光,宋惠珍,周庆,张宁.库车坳陷深浅构造变形与地震关系浅析[J].地震地质,2004,26(2):236-247. |
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| 作者姓名： | 刘洁 曲国胜 童晓光 宋惠珍 周庆 张宁 |
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| 作者单位： | 中国地震局地质研究所,北京,100029;中国石油国际合作司,北京,100724 |
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| 基金项目： | 国家重点基础研究发展规划项目 (G19990 4 330 5 )资助 |
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| 摘 要： | 通过研究库车地区的地震活动性 ,由地震分布的规律性推断可能的基底断裂 ,并分析了基底活动断裂与地表构造的对应关系、盖层变形和基底变形特征的差异及成因。结果表明 :1)地震震中分布揭示库车坳陷内对应东、西秋里塔格背斜带位置上 ,基底中发育东秋里塔格深断裂和南、北秋里塔格深断裂 ;另外 ,依奇克里克背斜和亚肯背斜位置上也存在对应的深断裂 ,这表明地表构造的形成受深部构造的控制。 2 )依奇克里克构造西端至东秋 5井连线位置上发育 1条NE向走滑断裂 ,在拜城西侧发 1条NW走向的活动断裂 ,这 2条切穿构造走向的活动断裂是库车坳陷构造分段的主因。 3)基底和盖层变形特征的差异主要源于二者之间介质特性的差异。盆地基底岩石圈强度非常高 ,决定了其变形以脆性破裂———地震活动为主 ;而盖层中沉积岩层强度较弱 ,且存在煤和膏盐等极软弱的薄层 ,在构造挤压作用下 ,可以产生黏性或塑性流动大变形及顺层无震滑脱
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| 关 键 词： | 地震活动性 地表构造 基底断裂 变形特征 库车坳陷 |
| 文章编号： | 0253-4967(2004)02-0236-12 |
| 修稿时间： | 2003年6月9日 |
A PRELIMINARY STUDY ON THE RELATIONSHIP BETWEEN BASEMENT-COVER TECTONIC DEFORMATION AND SEISMICITY IN KUQA DEPRESSION |
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| LIU Jie QU Guo-sheng TONG Xiao-guang SONG Hui-zhen ZHOU Qing ZHANG Ning Institute of Geology,China Earthquake Administration,Beijing ,China International Cooperation.A PRELIMINARY STUDY ON THE RELATIONSHIP BETWEEN BASEMENT-COVER TECTONIC DEFORMATION AND SEISMICITY IN KUQA DEPRESSION[J].Seismology and Geology,2004,26(2):236-247. |
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| Authors: | LIU Jie QU Guo-sheng TONG Xiao-guang SONG Hui-zhen ZHOU Qing ZHANG Ning Institute of Geology China Earthquake Administration Beijing China International Cooperation |
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| Affiliation: | LIU Jie 1) QU Guo-sheng 1) TONG Xiao-guang 2) SONG Hui-zhen 1) ZHOU Qing 1) ZHANG Ning 1) 1)Institute of Geology,China Earthquake Administration,Beijing 100029,China 2)International Cooperation Department,Petro China,Beijing 100724,China |
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| Abstract: | By analyzing the seismicity in Kuqa depression,north Tarim Basin,some active basement faults are inferred from the distribution of earthquake epicenters in several profiles.The different deformation charac-teristics between the cover and the basement,as well as their reasons are investigated by comparing the lo-cations of surface structures and basement faults,combined with some other results of deformation and kinematic research in this region.The following conclusions can be drawn from the present study: (1)The distribution of earthquake epicenters indicates that active basement faults exist along the tec-tonic grain corresponding to that of the surface structures of the Qiulitage-Yaken tectonic belt in Kuqa de-pression.In the basement beneath the East and West Qiulitage anticlines,there exist the East,North and South Qiulitage deep faults.Moreover,in the basement beneath the Yiqikelike anticline and Yaken anti-cline there exist the Yiqikelike and Yaken deep faults.These facts may imply that the development of sur-face structures was controlled by the deep structures. (2)It is revealed that a NE-trending deep strike slip fault is developed along the line from the west end of the Yiqikelike anticline to the Dongqiu No.5well,and a NW-trending deep fault is developed on the west side of Baicheng.These two active deep faults cut the tectonic grain of the region,and might be responsible for the segmentation of tectonics in Kuqa depression,probably has led to the greater contraction at the middle segment of Kuqa depression(Kuqa-Baicheng)and smaller contraction at east and west seg-ments.(3)The different characteristics of media result in the different deformation between the cover and the basement.The strength of the lithosphere at the basement of Kuqa depression is extremely high,so that deformation of the basement here is dominated by brittle fracturing and the generation of earthquake.The strength of the sedimentary rocks in the cover is much weaker,which may cause the plastic flow of the rocks under the action of long-period intense compression from the orogenic belt.And especially with the existence of coal or salt layers of extremely weak strength in the cover,a large scale aseismic detachment may occur along these weak layers. |
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| Keywords: | seismicity surface structure basement fault deformation characteristic Kuqa depression |
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