摘要
以野外地质观察和断裂的地质剖面为依据 ,阐述了青岛沧口 -温泉断裂的空间展布和构造特征。并应用区域地貌、地震地质、第四纪地质方法和断裂活动的绝对年龄资料对青岛沧口 -温泉断裂现代活动性进行了研究 ,认为上述断裂自晚更新世以来 ,其活动趋向稳定状态 ,属于晚第四纪不活动断裂。
We describe the plane geometry and structural features of the Cangkou Wenquan fault in Qingdao on the basis of field observations. We study the recent activity of this fault by using geomorphy, geology, and dating data. It is suggested that this fault has been becoming stable since Holocene time and is a nonactive fracture of late Quaternary.
出处
《地震地质》
EI
CSCD
北大核心
2001年第1期63-68,共6页
Seismology and Geology
