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Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part I

机译:地震过程:物理建模,数值模拟和数据分析第一部分

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摘要

In the last decade of the 20th century there has been great progress in the physics of earthquake generation; that is, the introduction of laboratory-based fault constitutive laws as a basic equation governing earthquake rupture, quantitative description of tectonic loading driven by plate motion, and a microscopic approach to study fault zone processes. The fault constitutive laws plays the role of an interface between microscopic processes in fault zones with macroscopic processes of a fault system, and the plate motion connects diverse crustal activities and mantle dynamics. The APEC Cooperation for Earthquake Simulation (ACES) aims to develop realistic computer simulation models for the complete earthquake generation process on the basis of microscopic physics in fault zones and macroscopic dynamics in the crust-mantle system, and to assimilate seismological and geodetical observations into such models. Simulation of the complete earthquake generation process is an ambitious challenge. Recent advances in high performance computer technology and numerical simulation methodology are bringing this vision within reach.
机译:在20世纪的最后十年,地震发生物理学取得了长足的进步。就是说,引入了基于实验室的断层本构定律作为控制地震破裂的基本方程式,定量描述了板块运动驱动的构造载荷,以及研究断层带过程的微观方法。断层本构定律在断层带的微观过程与断层系统的宏观过程之间起着界面作用,板块运动将各种地壳活动和地幔动力学联系起来。 APEC地震模拟合作组织(ACES)旨在在断层带的微观物理学和地幔幔系统的宏观动力学的基础上,为整个地震发生过程开发现实的计算机模拟模型,并将地震和大地观测资料纳入其中楷模。模拟完整的地震发生过程是一个艰巨的挑战。高性能计算机技术和数值模拟方法的最新进展使这一愿景遥不可及。

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