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Stress transfer in earthquakes, hazard estimation and ensemble forecasting: Inferences from numerical simulations

机译:地震中的应力传递,危害评估和整体预报:数值模拟的推论

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Observations indicate that earthquake faults occur in topologically complex, multi-scale networks driven by plate tectonic forces. We present realistic numerical simulations, involving data-mining, pattern recognition, theoretical analyses and ensemble forecasting techniques, to understand how the observable space-time earthquake patterns are related to the fundamentally inaccessible and unobservable dynamics. Numerical simulations can also help us to understand how the different scales involved in earthquake physics interact and influence the resulting dynamics. Our simulations indicate that elastic interactions (stress transfer) combined with the nonlinearity in the frictional failure threshold law lead to the self-organization of the statistical dynamics, producing 1) statistical distributions for magnitudes and frequencies of earthquakes that have characteristics similar to those possessed by the Gutenberg-Richter magnitude-frequency distributions observed in nature; and 2) clear examples of stress transfer among fault activity described by stress shadows, in which an earthquake oil one group of faults reduces the Coulomb failure stress oil other faults, thereby delaying activity oil those faults. In this paper, we describe the Current state of modeling and simulation efforts for Virtual California, a model (or all the major active strike slip faults in California. Noting that the Working Group oil California Earthquake Probabilities (WGCEP) uses statistical distributions to produce earthquake forecast probabilities, we demonstrate that Virtual California provides a powerful tool for testing the applicability and reliability of the WGCEP statistical methods. Furthermore, we show how the simulations call be used to develop statistical earthquake forecasting techniques that are complementary to the methods used by the WGCEP, but improve upon those methods in a number of important ways. In doing so, we distinguish between the "official", forecasts of the WGCEP, and the "research-quality" forecasts that we discuss here. Finally, we provide a brief discussion of future problems and issues related to the development of ensemble earthquake hazard estimation and forecasting techniques. (c) 2005 Elsevier B.V. All rights reserved.
机译:观测表明,地震断层发生在由板块构造力驱动的拓扑复杂的多尺度网络中。我们提出了现实的数值模拟,包括数据挖掘,模式识别,理论分析和整体预测技术,以了解可观察到的时空地震模式与根本上无法接近且无法观察到的动力学之间的关系。数值模拟还可以帮助我们理解地震物理中涉及的不同尺度如何相互作用并影响所产生的动力学。我们的模拟表明,弹性相互作用(应力传递)与摩擦破坏阈值定律中的非线性相结合会导致统计动力学的自组织,从而产生1)地震震级和频率的统计分布,其特征与地震所具有的相似。自然界中观察到的古腾堡-里希特幅频分布; 2)用应力阴影描述的断层活动之间的应力转移的清晰例子,其中一组地震油降低了库仑破裂应力,而其他断层又降低了库仑破裂应力,从而延缓了这些断层的活动。在本文中,我们描述了虚拟加利福尼亚州(一种模型(或加利福尼亚州所有主要的活动走滑断层))的建模和仿真工作的当前状态。注意到工作组石油加州地震概率(WGCEP)使用统计分布来产生地震预报概率,我们证明了虚拟加利福尼亚州为测试WGCEP统计方法的适用性和可靠性提供了一个强大的工具,此外,我们还展示了如何使用模拟方法来开发统计地震预报技术,这些技术是对WGCEP统计方法的补充,但是在许多重要方面改进了这些方法,在此过程中,我们区分了WGCEP的“官方”预测,本文所讨论的“研究质量”预测。与整体地震灾害估计和预报技术发展有关的未来问题。 (c)2005 Elsevier B.V.保留所有权利。

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