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Real-time inversions for finite fault slip models and rupture geometry based on high-rate GPS data

机译:基于高速GPS数据的有限断层滑动模型和破裂几何形状的实时反演

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摘要

We present an inversion strategy capable of using real-time high-rate GPS data to simultaneously solve for a distributed slip model and fault geometry in real time as a rupture unfolds. We employ Bayesian inference to find the optimal fault geometry and the distribution of possible slip models for that geometry using a simple analytical solution. By adopting an analytical Bayesian approach, we can solve this complex inversion problem (including calculating the uncertainties on our results) in real time. Furthermore, since the joint inversion for distributed slip and fault geometry can be computed in real time, the time required to obtain a source model of the earthquake does not depend on the computational cost. Instead, the time required is controlled by the duration of the rupture and the time required for information to propagate from the source to the receivers. We apply our modeling approach, called Bayesian Evidence-based Fault Orientation and Real-time Earthquake Slip, to the 2011 Tohoku-oki earthquake, 2003 Tokachi-oki earthquake, and a simulated Hayward fault earthquake. In all three cases, the inversion recovers the magnitude, spatial distribution of slip, and fault geometry in real time. Since our inversion relies on static offsets estimated from real-time high-rate GPS data, we also present performance tests of various approaches to estimating quasi-static offsets in real time. We find that the raw high-rate time series are the best data to use for determining the moment magnitude of the event, but slightly smoothing the raw time series helps stabilize the inversion for fault geometry.
机译:我们提出了一种反演策略,它能够使用实时高速率GPS数据同时随着破裂的发生而实时求解分布式滑模和断层几何形状。我们使用贝叶斯推断,使用简单的解析解决方案找到最佳的断层几何形状以及该几何形状可能的滑动模型的分布。通过采用贝叶斯分析方法,我们可以实时解决这一复杂的反演问题(包括计算结果的不确定性)。此外,由于可以实时计算分布滑动和断层几何的联合反演,因此获得地震震源模型所需的时间不取决于计算成本。取而代之的是,所需的时间由破裂的持续时间和信息从信号源传播到接收器所需的时间控制。我们将我们的建模方法(称为贝叶斯循证断层定向和实时地震滑动)应用于2011年东北冲木地震,2003年十胜冲木地震和模拟的海沃德断层地震。在这三种情况下,反演都能实时恢复滑动的幅度,空间分布和断层几何形状。由于我们的反演依赖于从实时高速率GPS数据估计的静态偏移,因此,我们还提出了各种方法的性能测试,以实时估计准静态偏移。我们发现原始高速率时间序列是用于确定事件的矩量级的最佳数据,但是稍微平滑原始时间序列有助于稳定断层几何形状的反演。

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