东昆仑断裂带西大滩段全新世古地震研究  

RESEARCH ON HOLOCENE PALEOEARTHQUAKES ON THE XIDATAN SEGMENT OF THE EAST KUNLUN FAULT ZONE IN NORTHERN TIBET

作　　者：胡道功[1] 叶培盛[1] 吴珍汉[1] 吴中海[1] 赵希涛[2] 刘琦胜[1] 

机构地区：[1]中国地质科学院地质力学研究所,北京100081 [2]中国科学院地质与地球物理研究所,北京100029

出　　处：《第四纪研究》2006年第6期1012-1020,共9页Quaternary Sciences

基　　金：中国地质调查局国土资源大调查项目(批准号:1212010541403)资助

摘　　要：对东昆仑断裂带西大滩段进行了断错地貌填图和古地震探槽揭露，共揭露出6次古地震事件，它们的年龄分别为10302±651aB．P．，8650±500aB．P．，7160±506aB．P．，2830±170aB．P．，1985±121aB．P．和1540±92aB．P．；古地震重复间隔分别为1652±820a，1490±711a，4330±534a，845±209a和445±152a。研究发现，西大滩段全新世古地震活动具有丛集现象和重复间隔时间的分段性，第1丛集期在10300—7100aB．P．期间，平均重复间隔1571±543a，第2丛集期在2800—1500aB．P．期间，重复间隔400—800a左右，平均重复间隔645±129a，两个丛集期间隔4300a。西大滩段全新世地震活动规律对昆仑山地区未来地震危险性评估具有重要意义。The East Kunlun Fault zone in Northern Tibetan Plateau is a typical active fault zone, characterized by sinistral strike-slip faults. The field investigation has reveals a lot of relics along the fault traces of the Xidatan- Dongdatan segment of the Kunlun Fault, including push-up and pull-apart basins, sag pond, and earthquake fault scarps. They imply that the Xidatan-Dongdatan segment of the Kunlun Fault is a seismogenic fault in which surface- rupturing earthquakes often occured in regular or irregular intervals. To determine the chronology of Holocene surface ruptures of this part of the Kunlun Fault, four trenches were excavated across the Xidatan-Dongdatan segment at Xiaonanchuan near Xidatan Town and Jingxian Valley near Kunlun Pass, respectively. All sediment samples collected from the trenches were dated by using thermoluminescence （TL） and optically stimulated luminescence （OSL） methods. Paleoseismic evidence, combined with the optically stimulated luminescence （OSL） and thermoluminescence （TL） dating of sediments and collapse units from the trenches, shows that the Xidatan segment of the Kunlun Fault zone has generated at least 6 earthquakes during the Holocene, whose ages are 10302 ± 651aB. P., 8650 ± 500aB. P., 7160 ± 506aB. P., 2830 ± 170aB. P., 1985 ± 12laB. P., and 1540 ± 92aB. P. respectively. The recurrence interval between two adjacent events is 1652 ± 820a, 1490 ± 711 a,4330 ±534a,845 ± 209a, and 445 ± 152a respectively. It shows that the recurrence is not uniform with time, that is, the distribution of paleoearthquakes on the Xidatan segment of the Kunlun Fault is characterized by clustering. The Holocene is divided into two subperiods in terms of paleoseismic evidence, the Early Holocene characterized by a recurrence interval of 1571 ± 543a, and the Late Holocene characterized by a higher frequency of tectonic events and a recurrence interval of 645 ± 129a. This result suggests that the Xidatan segment of the fault had displayed a timedependent seismic behavior.

关 键 词：古地震历史 地震复发间隔 全新世断层活动 东昆仑断裂 

分 类 号：P315.2[天文地球—地震学] P534.632[天文地球—固体地球物理学]