张玲, 朱建亚, 许萍, 何钧, 刘元生. 青岛及邻近地区地震活动特征分析[J]. 华北地震科学, 2007, 25(2): 33-35.
引用本文: 张玲, 朱建亚, 许萍, 何钧, 刘元生. 青岛及邻近地区地震活动特征分析[J]. 华北地震科学, 2007, 25(2): 33-35.
ZHANG Ling, ZHU Jian-ya, XU Ping, HE Jun, LIU Yuan-sheng. CHARACTERISTICS OF EARTHQUAKE ACTIVITY IN QINGDAO AND ITS ADJACENT REGION[J]. North China Earthquake Sciences, 2007, 25(2): 33-35.
Citation: ZHANG Ling, ZHU Jian-ya, XU Ping, HE Jun, LIU Yuan-sheng. CHARACTERISTICS OF EARTHQUAKE ACTIVITY IN QINGDAO AND ITS ADJACENT REGION[J]. North China Earthquake Sciences, 2007, 25(2): 33-35.

青岛及邻近地区地震活动特征分析

CHARACTERISTICS OF EARTHQUAKE ACTIVITY IN QINGDAO AND ITS ADJACENT REGION

  • 摘要: 对青岛及邻近地区的地震地质背景和地震活动情况进行了分析, 并结合本区的小震综合机制解的特点, 分析了P、T轴时序变化与邻区地震活动之间关系, 发现中强地震的发生可导致研究区域内P、T轴方位的变化。P、T轴方位变化的时间较为同步, 而P轴方位变化幅度更为明显。

     

    Abstract: The seismogeological background and seismic activity in Qingdao and its adjacent area are analyzed.Combined the focal mechanism of small earthquakes in the region, the relation between time sequence variation of P and T axes and earthquake activities in adjacent area is studied.The results show that the occurrence of strong earthquakes can cause the variation of P and T axis direction.The variation of P and T axes is synchronous, but the magnitude of P axis change is more obvious.

     

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