新疆地震构造带及近期地震活动趋势  

The Seismic Tectonic Belt and the Current Possible Shifting Tendencies of the Earthquakes in Xinjiang

作　　者：杨发义[1] 

机构地区：[1]新疆师范大学地理系

出　　处：《新疆师范大学学报（自然科学版）》1993年第1期66-71,81,共7页Journal of Xinjiang Normal University(Natural Sciences Edition)

摘　　要：本文论述了新疆地震构造带的划分及特征,列举了新疆主要活动断裂的分布。着重分析了新疆地震的时空分布与迁移特征。在此基础上,对新疆近期地震活动趋势作了预测。Based upon a thorough study of the classification as well as the characteristics of the seismic tectonicaone in XingJiang, especially the magnitude, the epicentral region, and the scattering pattern of its main active fissural regions,and a full discussion of the seismic variations in time and space,and its quivering and emigrating features,the author made predictions about the current possible shifting tendencies of the earthquakes in Xinjiang.

关 键 词：地震构造带 活动断裂 迁移特征 强震危险区 

分 类 号：N55[自然科学总论]