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青岛劈石口断裂的构造特征和现代活动性研究
引用本文:栾光忠,赵淑娟,王庆帅,景春雷,丁文洁,谢汝吉.青岛劈石口断裂的构造特征和现代活动性研究[J].中国海洋大学学报(自然科学版),2009,39(2).
作者姓名:栾光忠  赵淑娟  王庆帅  景春雷  丁文洁  谢汝吉
作者单位:中国海洋大学海底科学与探测技术教育部重点实验室,海洋地球科学学院,山东,青岛,266100
基金项目:中国海洋大学本科训练项目,山东省自然科学基金 
摘    要:通过野外地质观察和断裂平、剖面图的绘制,阐述了青岛劈石口断裂的空间展布、构造特征和构造作用.并应用地貌学、第四纪地质学、地震地质学和构造年代方法对劈石口断裂的现代活动性进行了研究,认为上述断裂自晚更新世以来,其活动性趋向稳定状态,属于晚第四纪不活动断裂.

关 键 词:劈石口断裂  空间展布  现代活动  环境地质

The Study of Structural Characteristic and Modern Activity of the Qingdao Pishkou Fault Zone
LUAN Guang-Zhong,ZHAO Shu-Juan,WANG Qing-Shuai,JING Chun-Lei,DING Wen-Jie,XIE Ru-Ji.The Study of Structural Characteristic and Modern Activity of the Qingdao Pishkou Fault Zone[J].Periodical of Ocean University of China,2009,39(2).
Authors:LUAN Guang-Zhong  ZHAO Shu-Juan  WANG Qing-Shuai  JING Chun-Lei  DING Wen-Jie  XIE Ru-Ji
Institution:College of Marine Geo-Science;Ocean University of China;Qingdao 266100;China
Abstract:The space distribution, structureal charccteristic and the structure effects of the Pishikou fault in Qingdao were studied by the way of field observations and paining the profile pictures of the fault. Modern activity of the Pishikou fault in Qingdao was studied by the way of physiognomy, seism geology, Quaternary,and the structure chronology. The conclusion was got that the Pishikou fault tend to become steady since the late Pleistocene, and it's a inactive fault in later Quaternary.
Keywords:Pishikou fault  space distribution  modern activity  environmental geology  
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