首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Automatic imaging of earthquake rupture processes by iterative deconvolution and stacking of high-rate GPS and strong motion seismograms
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Automatic imaging of earthquake rupture processes by iterative deconvolution and stacking of high-rate GPS and strong motion seismograms

机译:通过迭代反卷积和高速GPS和强震地震图的叠加,自动对地震破裂过程进行成像

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摘要

By combining the complementary advantages of conventional network inversion and backprojection methods, we have developed an iterative deconvolution and stacking (IDS) approach for imaging earthquake rupture processes with near-field complete waveform data. This new approach does not need any manual adjustment of the physical (empirical) constraints, such as restricting the rupture time and duration, and smoothing the spatiotemporal slip distribution. Therefore, it has the ability to image complex multiple ruptures automatically. The advantages of the IDS method over traditional linear or nonlinear optimization algorithms are demonstrated by the case studies of the 2008 Wenchuan and 2011 Tohoku earthquakes. For such large earthquakes, the IDS method is considerably more stable and efficient than previous inversion methods. Additionally, the robustness of this method is demonstrated by comprehensive synthetic tests, indicating its potential contribution to tsunami and earthquake early warning and rapid response systems. It is also shown that the IDSmethod can be used for teleseismic waveforminversions. For the twomajor earthquakes discussed here, the IDS method can provide, without tuning any physical or empirical constraints, teleseismic rupture models consistent with those derived from the near-field GPS and strong motion data.
机译:通过结合常规网络反演和反投影方法的互补优势,我们开发了一种迭代反卷积和叠加(IDS)方法,用于利用近场完整波形数据对地震破裂过程进行成像。这种新方法不需要对物理(经验)约束进行任何手动调整,例如,限制破裂时间和持续时间,以及平滑时空滑移分布。因此,它具有自动对复杂的多个破裂进行成像的能力。通过2008年汶川和2011年东北地震的案例研究,证明了IDS方法相对于传统线性或非线性优化算法的优势。对于如此大的地震,IDS方法比以前的反演方法更加稳定和有效。此外,该方法的鲁棒性通过全面的综合测试得到证明,表明其对海啸和地震预警和快速响应系统的潜在贡献。还显示了IDS方法可用于远震波形反演。对于此处讨论的两次大地震,IDS方法可以在不调整任何物理或经验约束的情况下提供与从近场GPS和强运动数据推导出的地震破裂模型一致的地震破裂模型。

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