摘要
评述腾冲火山断裂构造特征、断裂活动性及其与火山活动关系，论述本区地质构造格架、断裂活动与大区域构造的关系和构造演化历史。从中看出，腾冲地区的断裂构造、火山活动均受地壳运动、块体聚散的控制，并具有继承性和延拓性。
In this paper, features of fault structures, fault activity and its relation with volcano have been evaluated, and geological structural outline, fault activity and its relation with regional tectonics, and evolution history have been discussed. From studies, the fault structure and volcano activity in Tengchong area are controlled by crustal movement and block gathering and dispersing, having inheritance and extensibility.
出处
《地震研究》
CSCD
北大核心
1998年第4期330-336,共7页
Journal of Seismological Research
