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《Quaternary Sciences》 2006-01
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PRELIMINARY ANALYSIS ON AN EARLY QUATERNARY NEW FAULT TRACE IN NORTH OF TIBETAN PLATEAU

Tian Qinjian Ding Guoyu(Institute of Earthquake Science,China Earthquake Administration,Beijing100036)  
Haiyuan Fault Zone and(Kekexili-East) Kunlun Fault Zone are main regional strike slip fault zones in Northern Tibetan Plateau.There is a series of pull-apart basins developed in different periods in the Haiyuan Fault Zone.The Laolongwan Basin developed in Neocene is the largest one.At northeast of the Laolongwan Basin,a series of smaller pull-apart basins are existing.By analyzing the strata and morphostructures at edges of these latest pull-apart basins,we believe that the latest pull-apart basins in the Haiyuan Fault Zone were generated later than 1.6MaB.P.,indicating a new tectonic period when a new fault was generated.The direction of the newly generated fault had a counterclockwise angle with the original fault.A series of strong earthquakes occurred along the(Kekexili-East) Kunlun Fault Zone in Central Tibetan Plateau.Surface rupture of earthquakes indicated a new fault in that zone.Through the study of the new fault trace and morphostructures by earthquake surface rupture investigation and satellite image interpretation,we suggest that the Kekexili-East Kunlun Fault Zone is a zone with many new generated faults,which were generated between 1.1MaB.P.and 0.65MaB.P.,and also have counterclockwise angles with the original faults. Beside the Haiyuan Fault Zone and the Kekexili-East Kunlun Fault Zone,many other fault zones in Northeastern Tibet Plateau can be found to have new fault traces.Most of these new fault traces have counterclockwise angle with the original faults.This is consistent with the clockwise rotation of the Tibetan Block.We thus presume that a tectonic event might occur at middle to late Early Pleistocene in Northeast of Tibetan Plateau.In this paper we have attempted to discover the fault activities in order to reveal the characteristics of the regional tectonic event along with the uplifting of the Tibetan Plateau in Early Quaternary,and to accumulate data for study style and distribution of each tectonic event.
【Fund】: 科学技术部社会公益研究专项项目(批准号:2004DIA3J010)资助
【CateGory Index】: P542.3
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7 ZHENG Hong-bo 1,2 BUTCHER Katherine3 POWELL Chris3 1(Laboratory of Marine Geology, Tongji University, Shanghai 200092) 2(Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710054) 3(Tectonic Special Research Centre, The University of Western Australia, Perth);Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau——Ⅱ Facies Analysis[J];Acta Sedimentologica Sinica;2003-01
8 Cao Xingshan (No.2 Geol. Team of Hydrogeol. Engine., Bureau of Geol. and Miner. Res. of Gansu Prov., Zhangyi, 734004);The magnetostratigraphy of the Q y1 Drill Hole of Jiuquan, Gansu[J];JOURNAL OF STRATIGRAPHY;1997-04
9 Li Li; Zhang Guomin (Center for Analysis and Prediction, SSB, Beijing 100036, China)Shi Yaolin (Graduated School, USTC, Beijing 100039, China);A DYNAMIC MODEL FOR CONTINENTAL EARTHQUAKES[J];EARTHQUAKE;1997-02
10 Qiao Xuejun\+\{1)\},Wang Qi\+\{1)\}, Du Ruilin\+\{1)\}, Chen Zongshi\+\{2)\} You Xinzhao\+\{3)\} and Tan Kai\+\{1)\}\;1) Institute of Seismology, CSB, Wuhan\ 430071 2) No.2 Crustal Deformation Monitoring Center,CSB,Xi'an\ 710054 3) Center for Analysis and Predication,CSB,Beijing\ 100036;CHARACTERISTICS OF CRUSTAL DEFORMATION RELATING TO Ms8.1 KUNLUNSHAN EARTHQUAKE[J];Crustal Deformation and Earthquake;2002-04
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