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地震 ›› 2022, Vol. 42 ›› Issue (4): 70-88.doi: 10.12196/j.issn.1000-3274.2022.04.006

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基于沙城地震台的河北怀来地区剪切波分裂特征

孙海霞, 林向东, 司政亚, 钟世军, 赵桂儒, 侯丽娟   

  1. 北京市地震局, 北京 100080
  • 收稿日期:2022-05-30 修回日期:2022-08-30 发布日期:2023-03-31
  • 作者简介:孙海霞(1982-), 女, 山东菏泽人, 工程师, 主要从事地震编目及地震结构学研究。
  • 基金资助:
    北京市地震局面上项目(BJMS-2022001); 中国地震局科技星火计划攻关项目(XH200103); 北京市地震局重点项目(BJZD-2021001)

Characteristics of Shear Wave Splitting in Huailai Area, Hebei Province Based on Shacheng Seismic Station

SUN Hai-xia, LIN Xiang-dong, SI Zheng-ya, ZHONG Shi-jun, ZHAO Gui-ru, HOU Li-juan   

  1. Beijing Earthquake Agency, Beijing 100080, China
  • Received:2022-05-30 Revised:2022-08-30 Published:2023-03-31

摘要: 河北怀来盆地构造断裂发育, 历史上强震频发, 现今中小地震活动频繁。 基于沙城地震台2008年10月—2018年4月记录到的丰富高信噪比小震事件, 对怀来地区进行了剪切波分裂特征研究。 结果显示, 怀来地区快波平均偏振方向为87.3°±33.3°, 水平主压应力方向为NEE或近EW向; 这与前人得到的首都圈地区及华北地区区域构造应力场的主压应力方向一致, 反映了区域构造的局部信息。 沙城台快波偏振优势方向与台站附近NW向黄土窑—土木断裂走向不一致。 较长地震孕育期或小震群活动期, 怀来地区快波偏振方向较凌乱, 无明显优势方向。 在怀来地区小震群活动之前有慢剪切波时间延迟明显减小的趋势, 这将对该地区短临地震预报工作提供一定的支持。 2017年1月—2018年4月怀来地区慢波时间延迟平均值为1.24 ms·km-1, 数值较低, 可能与该时期无较大地震发生有关。

关键词: 剪切波分裂, 快波偏振方向, 慢波时间延迟, 水平主压应力, 震群

Abstract: Huailai Basin in Hebei Province, has developed faults, with frequent strong earthquakes in history and frequent medium-small earthquakes today. According to the high signal-to-noise small earthquake event waveforms recorded by Shacheng Seismic Station from October 2008 to April 2018, the shear-waves splitting characteristics of Huailai area are studied. The results show that the average polarization direction of fast shear-waves in Huailai area is 87.3°±33.3°, which suggests the direction of maximum horizontal principal compressive stress is NEE or nearly EW. This is consistent with the principal compressive stress direction of the regional tectonic stress field in the Capital zone and North China obtained by other predecessors, which reflects local information of regional tectonics. The dominant direction of fast shear-waves of Shacheng station is inconsistent with the strike (NW) of Huangtuyao-Tumu fault near the station. During the periods of seismogenesis or small earthquake swarm, the polarization direction of fast shear-waves in Huailai area is relatively disordered, with no obvious dominant direction. Before the small earthquake swarm activity in Huailai area, there was a significant decrease in the time delay of slow shear-waves, which can provide some supports for the short-impending earthquake prediction in this area. During the period of January 2017 to April 2018, the time delay of slow shear-waves is only 1.24 ms·km-1, which is lower than other periods, probably due to the absence of major earthquakes.

Key words: Shear wave splitting, Fast wave polarization direction, Slow wave delay time, Horizontal principal compressive stress, Earthquake swarm

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