青岛沧口-温泉断裂的空间展布及现代活动性研究

地震地质 ›› 2001, Vol. 23 ›› Issue (1): 61-68.

青岛沧口-温泉断裂的空间展布及现代活动性研究

栾光忠, 张海平

青岛海洋大学, 青岛 266003

收稿日期:2000-07-31 修回日期:2000-09-30 出版日期:2001-03-07 发布日期:2009-10-26

PLANE GEOMETRY AND MORDERN ACTIVITY OF THE QINGDAO CANGKOU-WENQUAN FAULT

Luan Guangzhong, Zhang Haiping

Oceon University of Qingdao, Qingdao 266003

Received:2000-07-31 Revised:2000-09-30 Online:2001-03-07 Published:2009-10-26

摘要/Abstract

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。

关键词: 青岛沧口-温泉断裂, 空间展布, 现代活动性, 环境地质

Abstract: 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.

Key words: Active fault, Recent activity, Qingdao

栾光忠, 张海平. 青岛沧口-温泉断裂的空间展布及现代活动性研究[J]. 地震地质, 2001, 23(1): 61-68.

Luan Guangzhong, Zhang Haiping. PLANE GEOMETRY AND MORDERN ACTIVITY OF THE QINGDAO CANGKOU-WENQUAN FAULT[J]. SEISMOLOGY AND GEOLOGY, 2001, 23(1): 61-68.