• 责任者：Wang Mingming (Key Laboratory of Active Tectonics and Volcano ; Institute of Geology ; China Earthquake Administration ; Beijing 100029 ; China) ; Zhou Bengang
• 刊名：Seismology and Geology
• 出版年：2013
• 卷期：35(4)
• 关键词：活动断层 ; active faults ; 汉中盆地 ; Hanzhong Basin
• 页码：p.778-792
• 图表：15 illus., 12 refs.
• 分类号：0300
• issnNo：ISSN0253-4967
• isbnNo：CN11-2192/P

     Since the Wenchuan earthquake,the seismic hazard of the northeastern segment of the Longmenshan Fault zone as well as the Hanzhong Basin has drawn more and more concerns.However,the essential data needed for further analysis on the seismic hazard in this region is scarce at present time,hence there is an urgent need for an in-depth study on the activities of faults around the basin.The faults around the Hanzhong Basin include five main faults,namely,the northern margin fault of Hanzhong Basin,the southern margin fault of Hanzhong Basin,the Qingchuan Fault,the ChabaLin＇ansi Fault and the southern margin fault of Liangshan.Based on several detailed field investigations on the geometric distribution,movement nature and active ages of the five faults,and with consideration of previous work,our study shows that the late-Quaternary tectonic activity in the basin is relatively intense in west and weak in east.The west section of the north-margin fault of the Hanzhong Basin（east of Baohe）was active in early late Pleistocene,while its eastern section（west of Baohe）was active in middle Pleistocene.The south-margin fault of the basin was also active in middle Pleistocene.And the three faults in the southwest of the basin were all active in late Pleistocene.This activity pattern of high in the west and low in the east is also demonstrated by the difference in thickness of Quaternary system and the distribution of small earthquakes.