| 西南天山前缘乌拉根背斜南翼逆断层的发现及其地质意义 |
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| 引用本文： | 李涛,陈杰,肖伟鹏,Burbank D W,Thompson J,杨晓东.西南天山前缘乌拉根背斜南翼逆断层的发现及其地质意义[J].地震地质,2011,33(2):277-288. |
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| 作者姓名： | 李涛 陈杰 肖伟鹏 Burbank D W Thompson J 杨晓东 |
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| 作者单位： | 中国地震局地质研究所地震动力学国家重点实验室;中国矿业大学(北京)地球科学与测绘工程学院;Department of Earth Science;University of California;Santa Barbara;CA 93106; |
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| 基金项目： | 科技部国际科技合作计划项目(2008DFA20860); 地震动力学国家重点实验室自主研究课题(LED2010A04); 我国地震重点监视防御区活动断层地震危险性评价项目共同资助 |
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| 摘 要： | 塔里木盆地新疆喀什以西部分是西南天山和帕米尔两大对冲构造系统的会聚带,关于两者变形前缘和分界的确切位置存在不同认识.在乌恰县以南的玛依卡克盆地南缘,清晰可见属于帕米尔构造带、向N或NNE逆冲的帕米尔前缘逆冲推覆体(PFT).最近野外调查在盆地北部发现了西南天山前缘的最新变形带:向南逆冲的乌拉根背斜南翼断层.断层总体近E...
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| 关 键 词： | 天山 帕米尔 塔里木盆地 乌拉根背斜南翼断层 弯滑断层 阶地变形 |
| 收稿时间： | 2011-04-07 |
| 修稿时间： | 2011-06-18 |
THE DISCORVERY AND GEOLOGIC SIGNIFICANCE OF THE THRUST AT SOUTH LIMB OF THE WULAGEN ANTICLINE,SOUTH MARGIN OF THE SOUTHWESTERN TIANSHAN |
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| LI Tao,CHEN Jie,XIAO Wei-peng,Burbank D W,Thompson J,YANG Xiao-dong.THE DISCORVERY AND GEOLOGIC SIGNIFICANCE OF THE THRUST AT SOUTH LIMB OF THE WULAGEN ANTICLINE,SOUTH MARGIN OF THE SOUTHWESTERN TIANSHAN[J].Seismology and Geology,2011,33(2):277-288. |
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| Authors: | LI Tao CHEN Jie XIAO Wei-peng Burbank D W Thompson J YANG Xiao-dong |
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| Institution: | LI Tao1) CHEN Jie1) XIAO Wei-peng1,2) Burbank D W3)Thompson J3) YANG Xiao-dong1)1)State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China2)College of Geoscience and Surveying Engineering,China University of Mining and Technology,Beijing 100083,China3)Department of Geological Sciences,University of California,Santa Barbara,CA 93106,USA |
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| Abstract: | The western Tarim Basin is a convergent zone of the Southwestern Tianshan and the Pamir,and there have been big debates about its exact boundary.However,in the Mayikake Basin,the boundaries of two tectonic systems are very clear: the north-vergent Pamir Front Thrust is the leading edge of the Pamir,and south-vergent thrust at south limb of the Wulagen anticline,which was discovered in recent field study,is the south margin of the Southwestern Tianshan.The thrust created 7.5～17.6m high scarps on the Tk3(the high terrace of the Kezilesu river)and Tb3(the high terrace of the Bieertuokuoyi river),with an occurrence of 6°∠15°.To the west,the thrust cuts all terraces of the Bieertuokuoyi river and the underlying youngest alluvial fans ultimately.The total length of thrust trace is about 12km.As activity of the thrust,lots of subparallel flexural-slip scarps are formed on terrace surfaces,which make terrace surfaces obviously differential back-tilted(tilted to south),and the locations of tilted degrees changed are corresponding to locations of flexural-slip faults.Shortening at south limb of the Wulagen anticline is absorbed by the thrust and flexural-slip faults,which is about ～71.4m since abandonment of the high terrace.Regional correlation indicates the high terrace is the same surface as the T2 located at north limb of the Mushi anticline with the age of～16ka,which indicates the average shortening rate of south limb of the anticline in late Quaternary is～4.5mm/a. |
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| Keywords: | Tianshan Pamir Tarim Basin thrust at south limb of the Wulagen anticline flexural-slip fault terrace deformation |
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