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The local magnitude scale and seismicity of the central United States.

机译:美国中部地区的局部震级和地震活动度。

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摘要

A local magnitude scale is developed for the central U.S. The distance correction function can be expressed as - log Ao = 0.939*log(r/100)--0.000276*(r--100) + 3.0, with amplitude Ao in mm and hypocentral distance r in km, showing a weak attenuation with distance. Estimations for b values and magnitudes of earthquakes with a return period of 500 years in the central U.S. are performed, based on the original New Madrid catalog (MD or m bLg) and the newly created ML catalog. Results show that the b value is smaller for the ML catalog (0.790), yielding one M 7.5 event every 500 years, a result that converges with the paleoearthquake estimate for the region. On average, the relation between ML and MD or mbLg (for 1.5 ≤ MD ≤ 5.0) can be expressed as ML=1.008*MD +0.0714.; We develop local magnitude scales for the Mississippi embayment of the central U.S. and the Kachchh basin of western India to understand the distance attenuation in these two regions. Results show that Kachchh basin distance attenuation is closer to southern California than to the central U.S., suggesting fundamental differences in local wave propagation between these two intraplate regions.; The spatial distribution of earthquake energy release for the New Madrid seismic zone (NMSZ) is mapped using the standard empirical magnitude-energy relation. The depth distribution of earthquake energy release may be a better proxy for modeling crustal strength than seismicity histograms in the NMSZ. We also map global earthquake energy release based on parameters of 445,373 events of the NEIC earthquake catalog with magnitudes equal to or greater than 1.0 over the time period from 1973 to 2006. The pattern of earthquake energy release in North America shows evidence of a seismic belt that encircles the cratonic interior. The global average relationship between earthquake energy release and strain rate is estimated to be log10 E = 1og10 3&d2; + 25 (with energy release in ergs and time in years). Using this relationship, the strain rate for the central U.S. is estimated to be between 7.9x10 -19 s-1 and 5.5x10-15 s-1.
机译:为美国中部地区开发了一个局部震级标尺。距离校正函数可以表示为-log Ao = 0.939 * log(r / 100)-0.000276 *(r--100)+ 3.0,振幅Ao以毫米为单位,并且位于中心距离r(以km为单位),显示随距离的衰减很小。根据原始的新马德里目录(MD或m bLg)和新创建的ML目录,对美国中部具有500年返回期的地震的b值和震级进行估算。结果表明,ML目录的b值较小(0.790),每500年发生一次M 7.5事件,其结果与该地区的古地震估计相吻合。平均而言,ML与MD或mbLg(对于1.5≤MD≤5.0)之间的关系可以表示为ML = 1.008 * MD +0.0714。我们为美国中部密西西比河沿岸和印度西部的Kachchh盆地开发了局部震级量表,以了解这两个地区的距离衰减。结果表明,Kachchh盆地距离衰减比美国中部距离加利福尼亚南部更近,这表明这两个板内区域之间的局部波传播存在根本差异。使用标准的经验量能关系图绘制了新马德里地震带(NMSZ)的地震能量释放的空间分布。与NMSZ中的地震直方图相比,地震能量释放的深度分布可能是模拟地壳强度的更好替代。我们还根据1973年至2006年期间NEIC地震目录中445,373个事件的大小等于或大于1.0的参数,绘制了全球地震能量释放的图表。北美地震能量释放的模式显示出一条地震带的证据。环绕克拉通内部。地震能量释放和应变率之间的全球平均关系估计为log10 E = 1og10 3&d2; + 25(能量释放以ergs为单位,时间以年为单位)。利用这种关系,美国中部的应变率估计在7.9x10 -19 s-1和5.5x10-15 s-1之间。

著录项

  • 作者

    Miao, Qingwen.;

  • 作者单位

    The University of Memphis.;

  • 授予单位 The University of Memphis.;
  • 学科 Geophysics.
  • 学位 Ph.D.
  • 年度 2007
  • 页码 110 p.
  • 总页数 110
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

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