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What Can We Learn from a Simple Physics-Based Earthquake Simulator?

机译:我们可以从一个简单的基于物理的地震模拟器学习什么?

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Physics-based earthquake simulators are becoming a popular tool to investigate on the earthquake occurrence process. So far, the development of earthquake simulators is commonly led by the approach "the more physics, the better". However, this approach may hamper the comprehension of the outcomes of the simulator; in fact, within complex models, it may be difficult to understand which physical parameters are the most relevant to the features of the seismic catalog at which we are interested. For this reason, here, we take an opposite approach and analyze the behavior of a purposely simple earthquake simulator applied to a set of California faults. The idea is that a simple simulator may be more informative than a complex one for some specific scientific objectives, because it is more understandable. Our earthquake simulator has three main components: the first one is a realistic tectonic setting, i.e., a fault data set of California; the second is the application of quantitative laws for earthquake generation on each single fault, and the last is the fault interaction modeling through the Coulomb Failure Function. The analysis of this simple simulator shows that: (1) the short-term clustering can be reproduced by a set of faults with an almost periodic behavior, which interact according to a Coulomb failure function model; (2) a long-term behavior showing supercycles of the seismic activity exists only in a markedly deterministic framework, and quickly disappears introducing a small degree of stochasticity on the recurrence of earthquakes on a fau (3) faults that are strongly coupled in terms of Coulomb failure function model are synchronized in time only in a marked deterministic framework, and as before, such a synchronization disappears introducing a small degree of stochasticity on the recurrence of earthquakes on a fault. Overall, the results show that even in a simple and perfectly known earthquake occurrence world, introducing a small degree of stochastici
机译:基于物理的地震模拟器正在成为调查地震发生过程的流行工具。到目前为止,地震模拟器的发展通常是通过“越多的物理学,越好”的方法。然而,这种方法可能会阻碍对模拟器结果的理解;事实上,在复杂的模型中,可能难以理解哪个物理参数与我们感兴趣的地震目录的特征最相关。出于这个原因,我们采取了相反的方法,并分析了应用于一组加利福尼亚缺陷的故意简单的地震模拟器的行为。这个想法是,对于一些特定的科学目标,一个简单的模拟器比复杂的模拟器更丰富,因为它更加理解。我们的地震模拟器有三个主要组成部分:第一个是逼真的构造环境,即加利福尼亚州的故障数据集;第二个是在每个单一故障上应用地震发生的定量法,最后是通过库仑故障功能的故障交互建模。对此简单模拟器的分析表明:(1)短期聚类可以通过一组故障再现,具有几乎定期行为,根据库仑故障功能模型进行交互; (2)仅在明显的确定性框架中显示出地震活动的超级性的长期行为,并且迅速消失在故障上发生较小的地震复发程度的少量随机性; (3)在库仑故障功能模型方面强烈耦合的故障仅在标记的确定性框架中同步,如前所述,这种同步在故障上引入了较小程度的速度。总的来说,结果表明,即使在一个简单而完美的地震发生世界,也引入了小程度的暂缓

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