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首页> 外文期刊>Earth, planets and space: EPS >An imaging technique for subsurface faults using Teleseismic-Wave Records II -Improvement in the detectability of subsurface faults-
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An imaging technique for subsurface faults using Teleseismic-Wave Records II -Improvement in the detectability of subsurface faults-

机译:使用远震波记录II的地下断层成像技术-改善地下断层的可探测性-

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摘要

We have developed an imaging algorithm for subsurface faults on the basis of the steepest descent method in our previous paper. In this paper we introduce two new techniques, the multi-event stacking and multi-master stacking, to improve detectability for subsurface faults. The multi-event stacking is a technique using data from plural earthquakes with different incident angles. The multi-master stacking is a technique using data of a single earthquake, in which the images obtained by employing different master receiver are stacked. We examined the feasibility of our approach using several trial models and synthetic data with different signal to noise ratios, different pulse durations and different incident angles in the two dimensional SH cases. In the numerical experiments, we could recover the image of the subsurface fault for all the trial models used, which indicates our method has a potential for sensing real subsurface faults.
机译:在之前的论文中,我们已经基于最速下降法开发了一种针对地下断层的成像算法。在本文中,我们介绍了两种新技术,即多事件堆栈和多主堆栈,以提高地下故障的可检测性。多事件叠加是一种使用来自具有不同入射角的多次地震的数据的技术。多主堆叠是使用单次地震数据的技术,其中堆叠通过采用不同的主接收器获得的图像。我们在二维SH案例中使用了几种试验模型和具有不同信噪比,不同脉冲持续时间和不同入射角的综合数据,检验了我们方法的可行性。在数值实验中,我们可以为所有使用的试验模型恢复地下断层的图像,这表明我们的方法具有检测实际地下断层的潜力。

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