节点文献
青岛胶州湾3.2级地震构造背景与控震断裂
The Background of Seismic Structure and Controlled-Earthquake Faults of 3.2 Grade Earthquake in Jiaozhou Bay of Qingdao
【摘要】 本文应用构造分析的方法 ,对青岛胶州湾 3.2级地震发生的地震地质背景和构造背景进行分析。结果表明 :胶州湾 3.2级地震主要受 NEE向郝官庄断裂和 NNW向大沽河断裂控制 ,并根据现代活动断裂的标志 ,对上述 2组断裂活动性特征作了阐述
【Abstract】 By using the method of geologic structural analysis, the backgroung of seismic structure and the controlled earthquake faults of 3.2 grade earthquake in Jiaozhou Bay are studied. It is assumed that the earthquake was mainly controlled by the Haoguanzhuang fault and Daguhe fault which run in the NEE and NNW direction respectively. Based on the marks of modern movements of fractures, the characteristics of the two faults are expounded.
【关键词】 青岛胶州湾；
地震；
构造地质背景；
控震断裂；
城市环境地质；
【Key words】 Jiaozhou Bay of Qingdao； earthquake； background of structural geology； controlled earthquake faults； city evironment geology；
【Key words】 Jiaozhou Bay of Qingdao； earthquake； background of structural geology； controlled earthquake faults； city evironment geology；
- 【文献出处】 青岛海洋大学学报(自然科学版) ,Journal of Ocean University of Qingdao , 编辑部邮箱 ,2002年05期
- 【分类号】P315.2
- 【被引频次】11
- 【下载频次】98