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首页> 外文期刊>Bulletin of the Seismological Society of America >Lg Attenuation near the North Korean Border with China, Part I: Model Development from Regional Earthquake Sources
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Lg Attenuation near the North Korean Border with China, Part I: Model Development from Regional Earthquake Sources

机译:朝鲜与中国边界附近的Lg衰减,第一部分:区域地震源的模型开发

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摘要

We have collected broadband data from three seismic networks—two portable and one permanent—in a remote part of northeast China bordering North Korea. The combined network coverage allows first-hand investigations of seismic-wave propagation in a region of import for nuclear test ban monitoring research. Application of the reversed two-station method to the newly acquired data has produced stable measurements of the quality factor Q (=Q0f) for Lg waves. The results, a weighted regional average over 23 interstation paths involving 51 events and 21 stations, point to 1 Hz Q (or Q0) of 345 and of 0.38 in a jarring incongruity with what appears to be a popular perception of the region as being of very low attenuation for Lg waves. The results also show that Lg Q varies from one interstation path to another. The highest Lg-wave attenuation (1100<140) is found along interstation paths that crossed two recently active volcanoes (Huangyishan and Changbaishan). The subregion exhibiting the next highest Lg attenuation is Bohai, an extensional basin known to feature above-average heat flow.
机译:我们在与朝鲜接壤的东北 中国的偏远地区,从三个地震网络(两个 便携式和一个永久性)收集了宽带数据。合并的网络覆盖范围允许 对进口区域 的地震波传播进行第一手调查,以进行核禁试监测研究。反向两站法对新获取的数据 的应用 已产生质量因子Q(= Q 0 f 用于Lg波。结果是23个站间路径的加权平均区域平均值,涉及51个事件和21个站,指向 的1 Hz Q(或Q 0 ) 345和0.38之间存在明显的不一致性 ,这似乎是该区域的一种普遍看法,因为 对Lg波的衰减非常低。结果还 显示了Lg Q从一个站间路径到另一站间路径的变化。 Lg波衰减最高(110 0 <140)在沿着两条最近活跃的火山(黄宜山和长白山)的跨站路径中发现了 。表现出 次高的Lg衰减的次区域是渤海,这是一个以 为特征的热流盆地,其热流高于平均水平。

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  • 来源
    《Bulletin of the Seismological Society of America》 |2009年第5期|3021-3029|共9页
  • 作者单位

    School of Ocean and Earth Science, Tongji University, 1239 Siping Road, Shanghai 200092, China kychun@tongji.edu.cn wyllmein2000@tom.com gary@core.yorku.ca;

    School of Ocean and Earth Science, Tongji University, 1239 Siping Road, Shanghai 200092, China kychun@tongji.edu.cn wyllmein2000@tom.com gary@core.yorku.ca;

    School of Ocean and Earth Science, Tongji University, 1239 Siping Road, Shanghai 200092, China kychun@tongji.edu.cn wyllmein2000@tom.com gary@core.yorku.ca;

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