中条山北麓断裂形变异常的研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
叙述了山西地震带南端运城盆地及其周边100km范围近20a的地震活动特征,运用形变异常参数、差分、统计等方法对运城盆地内跨中条山北麓断裂的水准观测资料进行了研究。结果表明,断层大幅度形变速率异常变化较好地对应了研究区内1979年至2002年7次ML≥4.2的地震活动,且山西永济风柏峪测线自2001年8月至2002年4月仍存在一定的形变异常信息,表明,中条山北麓断裂目前正处于增强活动之中。
Seismicity characteristics in Yuncheng basin of the southern part of Shanxi seismic belt as well as its peripheral area, ranging 100 km, during last 20 years are described. A study is made for leveling data observed across the fault at north Zhongtiao Mountain in Yuncheng basin, by using ground deformation anomaly parameter calculation, difference and statistic processing. The result shows that large ground deformation rate anomalies at the fault well correspond to 7 earthquakes of M_L≥4.2 ,from 1979 to 2002, in the studied area. There were some ground deformation anomalies at observation line located at Fengbai Mountain of Yongji,Shanxi, which indicate that the activity of the fault at North Zhongtiao Mountain is going up.
引文
[1] 中国地震局监测预报司.地震前兆异常落实工作指南[M].北京:地震出版社,2000.19.
    [2] 王向阳,杨海祥,刘国俊.山西永济风柏峪流动水准观测的监测能力判定[J].山西地震,2002(1):7-10.
    [3] 郭良迁,谢觉民.张北6.2级地震的断层形变速率异常[J].地壳形变与地震,2001,21(1):79-84.
    [4] 谭金意,杨林章.地壳形变观测与分析[M].北京:地震出版社,1998.196-218.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心