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《Seismology and Geology》 2006-02
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DEFORMATION PATTERN AND SHORTENING RATES IN THE EAST PART OF KALPIN THRUST SYSTEM IN SOUTHWEST TIANSHAN DURING LATE QUATERNARY

RAN Yong-kang YANG Xiao-ping XU Xi-wei CHENG Jian-wu CHEN Li-chun(Institute of Geology , China Earthquake Administration, Beijing 100029,China)  
Less attention has been paid to the deformation pattern, shortening amount and shortening rate in late Quaternary across Kalpin thrust system. This paper tries to discuss them, mainly in the eastern part of the thrust system by doing field investigation along the faults and folds, measuring geomorphic deformation, excavating trenches in some important sites where young alluvial fans were displaced obviously and dating young deposits of alluvial terrace. There are two types of deformation in surface and near surface for the Kalpin thrust system in late Quaternary i.e. the movement of thrust faults at lower angles and bending of young folds. Both kinds of deformation are shown by shortening and uplifting of young geomorphic surfaces. The surface ages of 3 stages are concluded by dating 20 examples using TL method in the studying area and comparing the results of previous people on deposition and incision times of alluvial terraces in Tianshan mountain area, and they are 100ka, 33~18ka and 6.6~8.2ka, respectively, for large-scale deformed alluvial surfaces: T_ 3 , T_ 2 , and T_ 1 in kalpin region. Then, the 19 shortening amounts and rates are obtained in the 13 sites along 4 rows of anticlines in front of Kalpin thrust system and Piqian fold. The shortening amounts and rates show that there are two sections where deformation is stronger than others. The two sections consist of two arcs that is toward the south. Shortening rates near top of arcs are 1.32mm/a in the west and 1.39mm/a in the east across the thrust system, respectively. Besides, deformation on front rows is stronger than that behind for bifurcate folds.
【Fund】: 中国地震局“新疆巴楚-伽师6.8级地震应急工作专项计划”项目资助
【CateGory Index】: P534.63
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9 ZHANG Pei\|zhen 1,2 , WANG Qi 3, MA Zong\|jin 1,2 (1 Institute of Geology, China Seismological Bureau, Beijing 100029, China; 2 Open Research Center of GPS,China Seismological Bureau,Beijing 100029,China; 3 Institute of Seismology, Chi;GPS VELOCITY FIELD AND ACTIVE CRUSTAL DEFORMATION IN AND AROUND THE QINGHAI-TIBET PLATEAU[J];Earth Science Frontiers;2002-02
10 QU Guo-sheng 1, LI Yi-gang 1, CHEN Jie 1,NING Bao-kun 1,LI Yan-feng 1,LI Jun 2, YIN Jun-ping 3 (1.Institute of Geology, China Seismological Bureau, Beijing 100029,China; 2.Xinjiang Seismological Bureau,rümqi 830011,China; 3.Southwest Tarim Petroleum Company,Zepu 844804,China);GEOMETRY,KINEMATICS AND TECTONIC EVOLUTION OF KEPINGTAGE THRUST SYSTEM[J];Earth Science Frontiers;2003-S1
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