东昆仑活动断裂带的强震构造条件及未来强震危险区分析  

TECTONIC CONDITION OF STRONG EARTHQUAKE OF THE EASTERN KUNLUN ACTIVE FAULT ZONE AND RISK AREA ANALYSIS OF FUTURE STRONG EARTHQUAKE

作　　者：张瑞斌[1] 赵培林[1] 陈玉华[1] 

机构地区：[1]青海省地震局

出　　处：《高原地震》1996年第3期12-21,共10页Plateau Earthquake Research

摘　　要：通过对东昆仑活动断裂带强震构造条件的研究发现，这条断裂带的强震构造条件不仅与所处的区域地壳运动状况有关，而且与该活动断裂带的规模、形态，断裂带的构造组合及断裂带的运动条件等密切相关。在研究了东昆仑活动断裂带强震构造条件的基础上，还沿断裂带划出了三个未来强震危险区。Based on the study of the tectonic condition of strong earthquake of the Eastern Kuniun active fault zone,the authors put forward that it relates to not only crustal motion regionly but also the scale and of shape this active fault zone. combination of fault zone structure and motion condition of fault zone. Three risk areas of future strong earthquake along this zone were determined therefrom.

关 键 词：东昆仑活动断裂带 强震构造带 危险区 

分 类 号：P56[天文地球—构造地质学]