新疆阜康-吉木萨尔断裂带的几何特征与活动性研究  

STRUCTURAL GEOMETRY AND ACTIVITIES OF THE FUKANG-JIMSAR FAULT ZONE, XINJIANG

作　　者：尤惠川[1] 任利生[2] 张玉梅[3] 

机构地区：[1]中国地震局地球物理研究所,北京100081 [2]中国地震局,北京100036 [3]中国地震局地质研究所,北京100029

出　　处：《地震地质》2003年第3期375-384,T001-T002,共12页Seismology and Geology

基　　金：地震科学联合基金 ( 1980 6 2 );科技部项目 ( 95110 2 )中国地震局地球物理勘探中心论著编号RECG2 0 0 2 0 1

摘　　要：根据详实的野外资料对新疆阜康 -吉木萨尔断裂带的构造几何特征和活动性进行了分析与研究 ,结果表明 :断裂带由东、西两大段组成 ,西段由 4条次级S倾逆断裂左行斜列组成 ,东段由 3条次级S倾逆断裂右行斜列组成 ,总体上呈向北微凸的近EW向展布 ,长达 14 0km ,控制着东天山北缘的第四纪构造演化和地貌发育 ;组成断裂往往是低角度的逆断层 ,与褶皱共生 ,切割深度 5～ 6km ,第四纪晚期多期 (次 )活动 ,以间歇性稳定滑动为特征 ;断裂带端部段落倾角较大 ,活动量较小 ,全新世平均垂直滑动速率为 0 .10～ 0 4 0mm/a ,中部段落以低倾角的推覆为特征 ,活动强烈 ,全新世平均垂直滑动速率达 0 80～ 1 0 0mm/a以上。Based on detailed field investigations, this paper describes geometrical characteristics and tectonic activities of the Fukang Jimsar Fault zone in eastern Tianshan, Xinjiang, China. This fault zone strikes nearly in east west, dipping to south, and extends over a length of 140km. It is a major geological/geomorphological margin controlling the neotectonic movement in this region. On the southern side of the Fukang Jimsar Fault develop Mesozoic strata, forming low mountains and hills; the northern side of the fault corresponds to a large Quaternary depression plain. The Fukang Jimsar Fault consists of 7 segments of secondary gently dipping reverse faults with lengths of 12～24km, i.e. the Ganquanpu, Sangonghe, Sigonghe, Ganhezi, Quanquanzi, Dalongkou and Dongfeng Muchang Faults. In seismic profiles these faults make up an anticline thrust structure in the range of 5～6km depth, having dip angles of 20°～30° at the lower part and 40°～50° at the upper part(sometimes nearly 60°～80° at the ground). All these fault segments display the evidence of late Quaternary activities such as fault scarps, offset terraces and young sedimentary deposits etc. The steep dipping distal segments of the fault experienced 7 times of activities in Holocene (with an occurrence interval of 1500yr), and have relatively small vertical slip rate (0.10～0.40mm/yr); while the gently dipping middle segments are characterized mainly by strong thrusting, and have relatively high vertical slip rate in Holocene (0 40～1 43mm/yr).

关 键 词：断裂带 几何特征 活动性 新疆 构造演化 地貌发育 褶皱: 

分 类 号：P542.3[天文地球—构造地质学]