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地震 ›› 2015, Vol. 35 ›› Issue (2): 111-120.

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唐山古冶、 滦县地区中小地震活动与构造关系研究

刘亢1,2, 曲国胜2, 房立华3, 李红光2   

  1. 1.中国地质科学院地质研究所, 北京 100037;
    2.中国地震应急搜救中心, 北京 100049;
    3.中国地震局地球物理研究所, 北京 100081
  • 收稿日期:2014-07-21 出版日期:2015-04-30 发布日期:2020-06-24
  • 作者简介:刘亢(1980-), 男, 陕西商洛人, 副研究员, 主要从事构造地质学研究。
  • 基金资助:
    地震行业科研专项(201208018)、 “十二五”国家科技支撑计划项目(2012BAK19B01-03)、中国地震应急搜救中心青年科技基金(YJ12021077)资助

Relationship between Tectonics and Small to Moderate Earthquakes in Guye and Luanxian area, Hebei Province

LIU Kang1, QU Guo-sheng1, FANG Li-hua2, LI Hong-guang1   

  1. 1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
    2. National Earthquake Response Support Service, Beijing, 100049, China;
    3. Institute of Geoghysics, CEA, Beijing 100081, China
  • Received:2014-07-21 Online:2015-04-30 Published:2020-06-24

摘要: 小震活动与断层运动紧密相关, 小震定位技术已逐渐成为地震断层破裂、 发震构造研究中不可或缺的手段。 本文采用双差定位法对唐山地区1978—2011年内发生地震进行重新定位, 以地震学与构造地质学为理论基础, 着眼于唐山地震构造系统与滦县地震构造系统的交汇区, 对连续、 丰富的地震数据进行时间、 空间综合分析, 发现古冶东侧出现一条新生地震带。 开滦煤矿地质资料证实了该新生地震带展布与徐家楼—王喜庄基岩断层完全重合, 推测2010年MS4.2地震与2012年MS4.8地震均由徐家楼—王喜庄断层活动引起, 应加强该区地震监测工作。

关键词: 发震构造, 双差定位, 时空分析, 中小震活动

Abstract: Small earthquake activity is closely associated with fault movement, and small earthquake location method is commonly used for earthquake fault rupture and seismogenic structure research. Using double difference algorithm, earthquakes occurred from 1978 to 2011 are relocated. On the basis of seismology and active tectonics, focusing on Tangshan earthquake tectonic system and Luanxian earthquake tectonic system, we discover a new earthquake belt in the east of Guye area through the spatial-temporal analysis of the plenty of consecutive small earthquakes, and we speculate there exists a deep fault of NNE-striking, which is coordinated with the linear feature and coal seams distribution features. The speculated fault coincides with the Xujialou fault from the coal field geological exploration data, which is considered to trigger the MS4.2 and MS4.8 earthquakes in the past 3 years. We suggest the earthquake monitoring on this region should be strengthened and active tectonic research about the speculated fault should be carried out.

Key words: Small earthquake activity, Double-difference location, Spatial-temporal analysis, Seismogenic structure

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