Abstract: In this paper,the shear wave splitting features in Longtan reservoir area are studied by adopting the traditional cross-correlation coefficient method and polarization analysis,using the data recorded by the seismic network founded by a project under the National Science and Technology Pillar Program from April 2009 to April 2010.We found that most of polarization directions at seismic stations are consistent with the direction of the overall regional stress field,but local structures and faults may control or influence the fast shear-wave polarization direction.The time-delay normalized to source-station path is between 10 to 25ms/km,and among them,the time-delay is about 10ms/km at the stations LIL and XIL,which are farther away from the dam.The water depth is relatively shallow and seismic activity relatively weak after water storage,indicating the effect of reservoir water penetration or loading on the state of cracks in the reservoir area.We also found that the delay time changes consistently with the water level at stations DPD and GAL.It may be related to crack expansion and water penetration caused by the reservoir impoundment.

Key words: Longtan Reservoir, shear-wave splitting, fast shear-wave polarization direction, delay time

摘要： 利用在龙滩地震观测台网2009年4月至2010年4月记录到的16,452条地震波形数据,采用传统的相关系数法和偏振分析方法,对龙滩库区剪切波分裂特征进行了系统的研究,并讨论了库区范围介质的各向异性特征。研究发现,库区较大区域内地震台站附近的偏振方向主要反映了区域整体应力场的作用方向,但局部构造和断层会控制或影响台站的快剪切波偏振优势方向。归一化1km单位距离上的延迟时间为10～25ms/km,其中距离库坝区较远、水深较浅、蓄水后响应地震活动相对较弱的LIL和XIL台单位距离上的延迟时间在10ms/km左右,而其他台站尤其库坝区附近蓄水后水深较深的则在20ms/km左右,这表明了库水渗透或载荷对库区裂隙状态的影响。研究还发现DPD和GAL台的快慢波延迟时间随水位变化而出现变化,其变化趋势呈现出与水位变化形态基本一致的现象,初步认为是与库区蓄水加载引起的裂隙进水扩张有关。

关键词: 龙滩水库, 剪切波分裂分析, 快波偏振方向, 快慢波时间延迟