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天山南缘北轮台断裂库尔楚段晚第四纪的最新活动和滑动速率
引用本文:邓起东 Molhar,P 等.天山南缘北轮台断裂库尔楚段晚第四纪的最新活动和滑动速率[J].内陆地震,2001,15(4):289-298.
作者姓名:邓起东 Molhar  P
作者单位:[1]中国地震局地质研究所,北京100029 [2]美国麻省理工学院地球、大气和行星科学系,麻萨诸塞州剑桥市02139
摘    要:使用全站仪实测了天山南麓北轮台逆断裂库尔楚段阿克艾肯-喀腊萨喀腊阿塔木冲洪积扇断层崖地形地貌,采用^10Be测年方法测定了该冲洪积扇的形成年龄,得到该断裂段垂直位移滑动速率为0.48mm/a、0.85-1.0mm/a和1.52mm/a,并对该断裂段的水平缩短速率和天山第四纪水平缩短量进行了讨论。

关 键 词:天山  北轮台断裂  晚第四纪活动  滑动速率  全站仪测量  铍10测年

LATEST ACTIVITY AND SLIP RATE OF KUERCHU SEGMENTOF BEILUNTAI FAULT IN SOUTH EDGE OF TIANSHAN,CHINA SINCE LATE PLEISTOCENE
DENG Qi-dong,P.Molnar,E.T.Brown,LI Jun,B.C.Burchfiel,FENG Xian-yue,YANG Xiao-ping,SHEN Jun.LATEST ACTIVITY AND SLIP RATE OF KUERCHU SEGMENTOF BEILUNTAI FAULT IN SOUTH EDGE OF TIANSHAN,CHINA SINCE LATE PLEISTOCENE[J].Inland Earthquake,2001,15(4):289-298.
Authors:DENG Qi-dong  PMolnar  ETBrown  LI Jun  BCBurchfiel  FENG Xian-yue  YANG Xiao-ping  SHEN Jun
Institution:DENG Qi-dong+1,P.Molnar+2,E.T.Brown+3,LI Jun+4,B.C.Burchfiel+2,FENG Xian-yue+4,YANG Xiao-ping+1,SHEN Jun+1
Abstract:Beiluntai fault zone is the boundary line between Tarim basin and south Tianshan Mts. Akeaiken-Kalasakalaatamu alluvial and diluvial fan is lied in Kuerchu segment of Beiluntai fault in the south edge of Tianshan.The topographic and geomorphic survey of the fan was made using Total Station,and the age of the fan was measured through 10Be dating.The vertical slip rate of the segment is calculated to be 0.48 mm/a,0.85-1.0 mm/a and 1.52 mm/a,and the horizontal shortening rate of the segment and the horizontal shortening amount of Tianshan since Quaternary were calculated,too.
Keywords:Tianshan  Beiluntai fault  Late Quaternary  Slip rate  Total Station survey  10Be dating
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