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Directional Statistics, Bayesian Methods of Earthquake Focal Mechanism Estimation, and Their Application to New Zealand Seismicity Data

机译:方向统计,地震震源机制估计的贝叶斯方法及其在新西兰地震数据中的应用

摘要

A focal mechanism is a geometrical representation of fault slip during an earthquake. Reliable earthquake focal mechanism solutions are used to assess the tectonic characteristicsof a region, and are required as inputs to the problem of estimating tectonic stress. We develop a new probabilistic (Bayesian) method for estimating the distribution of focal mechanismparameters based on seismic wave polarity data. Our approach has the advantage of enabling us to incorporate observational errors, particularly those arising from imperfectly known earthquake locations, allowing exploration of the entire parameter space, and leads to natural point estimates of focal mechanism parameters. We investigate the use of generalised Matrix Fisher distributions for parameterising focal mechanism uncertainties by minimising the Kullback-Leibler divergence. We present here the results of our method in two situations. We first consider the case in which the seismic velocity of the region of interest (described by a velocity model) is presumed to be precisely known, with application to seismic data from the Raukumara Peninsula,New Zealand. We then consider the case in which the velocity model is imperfectly known, with application to data from the Kawerau region, New Zealand. We find that our estimated focal mechanism solutions for the most part are consistent with all available polarity data, and correspond closely to solutions obtained using established methods. Further, the generalised Matrix Fisher distributions we examine provide a good fit to our Bayesian posterior PDF of the focal mechanism parameters, enabling the posterior PDF to be succinctly summarised by reporting the estimated parameters of the fitted distribution.
机译:震源机制是地震过程中断层滑动的几何表示。可靠的地震震源机制解决方案用于评估区域的构造特征,并且是估计构造应力问题的输入。我们开发了一种新的概率(贝叶斯)方法,用于基于地震波极性数据估计震源机制参数的分布。我们的方法的优势在于使我们能够合并观测误差,尤其是由于不完全已知的地震位置而产生的观测误差,从而可以探索整个参数空间,并导致对震源机制参数进行自然点估计。我们通过最小化Kullback-Leibler散度来研究使用广义矩阵Fisher分布来参数化焦点机制不确定性。我们在这里介绍两种情况下方法的结果。我们首先考虑将感兴趣的区域(由速度模型描述)的地震速度准确地已知的情况,并将其应用于来自新西兰劳库马拉半岛的地震数据。然后,我们考虑将速度模型不完全已知的情况,并将其应用于来自新西兰Kawerau地区的数据。我们发现,我们估计的震源机制解大部分与所有可用的极性数据一致,并且与使用已建立方法获得的解紧密对应。此外,我们检查的广义矩阵Fisher分布提供了与焦点机制参数的贝叶斯后验PDF的良好契合度,通过报告拟合分布的估计参数,可以简洁地总结后验PDF。

著录项

  • 作者

    Walsh David;

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  • 年度 2008
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  • 正文语种 en_NZ
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