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Spatial Variations of b-Values in the Coastal Area of Guangdong

机译:广东沿海地区b值的空间变化

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摘要

We used earthquake catalogs recorded by Guangdong Seismological Network from 2008 to 2014 to resolve the spatial variations of b-values in the coastal area of Guangdong,particularly in three key research areas (Yangjiang,Heyuan,and offshore Nanao Island) with strong seismicity.Our results revealed that b-values exhibited significant spatial variations,and zones with low b-values could indicate the most likely seismogenic area of large earthquakes.We observed three clear low b-value patches in the offshore Nanao Island.We found a distinct high b-value peak at the depth of 11 km and two minimum peaks at about 14 and 7-8 km in the Yangjiang area.The overall b-values generally decrease with depth in the Heyuan area.The spatial variations of b-values reflect tectonic anomalies;that is,the ‘low-high-low’ distribution of b-values in the offshore Nanao Island and the Yangjiang area may indicate the anomaly of the crustal structure with a weak layer.The b-values of reservoir-induced seismicity are obviously lower than that induced by tectonism.This finding indicates that the reservoir area is generally at high stress state under the condition of high pore pressure.We inferred that large earthquakes might be prone to occur at 10-12 km depth in the offshore Nanao Island,at 12-15 km depth in the Yangjiang area,and at the lower part of the seismic activity zone in the Heyuan area.Moreover,the upstream area of the Xinfengjiang reservoir is the most likely area of future large earthquakes in the Heyuan area.
机译:我们从2008年到2014年使用广东地震网络记录的地震目录,解决了广东沿海地区B价值的空间变化,特别是在三个关键研究领域(阳江,河源和近海纳娜岛),具有强大的地震。结果表明,B值表现出显着的空间变化,低B值的区域可以表明大地震的最有可能的地震区域。我们观察到南纳诺岛的三个清晰的低B值贴片。我们发现了一个明显的高B. - 在阳江地区约14至7-8公里的深度为11公里的峰值高达峰值,在大约14至7-8公里处。总体B值通常随着河源地区的深度而减少。B值的空间变化反映了构造异常即,南纳岛岛和阳江地区的B值的“低低低”分布可能表示具有薄弱层的地壳结构的异常。储层诱导的地震性的B值明显低于由构造症引起的。该发现表明,储层区域通常在高孔隙压力条件下处于高应力状态。我们推断出大地震可能在离岸南纳的10-12公里深度发生岛屿,在阳江地区12-15公里深度,河源地区地震活动区的下半部分。新丰江水库上游地区是河源地区未来大地震的最具可能的地区。

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  • 来源
    《中国海洋大学学报(英文版)》 |2018年第1期|177-185|共9页
  • 作者单位

    CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology,Chinese Academy of Sciences, Guangzhou 510301, China;

    College of Earth Sciences, University of Chinese Academy of Sciences, Beijing 100049, China;

    CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology,Chinese Academy of Sciences, Guangzhou 510301, China;

    CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology,Chinese Academy of Sciences, Guangzhou 510301, China;

    CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology,Chinese Academy of Sciences, Guangzhou 510301, China;

    CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology,Chinese Academy of Sciences, Guangzhou 510301, China;

    CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology,Chinese Academy of Sciences, Guangzhou 510301, China;

    Institute of Deep-Sea Science and Engineering, Chinese Academy of Sciences, Sanya 572000, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-19 03:49:05
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