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A bayesian framework to rank and combine candidate recurrence models for specific faults

机译:一个贝叶斯框架,用于对特定故障的候选递归模型进行排序和组合

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摘要

We propose a probabilistic framework in which different types of information pertaining to the recurrence of large earthquakes on a fault can be combined in order to constrain the parameter space of candidate recurrence models and provide the best combination of models knowing the chosen data set and priors. We use Bayesian inference for parameter and error estimation, graphical models (Bayesian networks) for modeling, and stochastic modeling to link cumulative offsets (CO) to coseismic slip. The cumulative offset-based Bayesian approach (COBBRA) method (Fitzenz et al., 2010) was initially developed to use CO data to further constrain and discriminate between recurrence models built from historical and archaeological catalogs of large earthquakes (CLE). We discuss this method and present an extension of it that incorporates trench data (TD). For our case study, the Jordan Valley fault (JVF), the relative evidence of each model slightly favors the Brownian passage time (BPT) and lognormal models. We emphasize that (1) the time variability of fault slip rate is critical to constrain recurrence models; (2) the shape of the probability density functions (PDF) of paleoseismic events is very important, in most cases not Gaussian, and should be reported in its complexity; (3) renewal models are in terms of intervals between consecutive earthquakes, not dates, and the algorithms should account for that fact; and (4) maximum-likelihood methods are inadequate for parameter uncertainty evaluation and model combination or ranking. Finally, more work is needed to define proper priors and to model the relationship between cumulative slip and coseismic slip, in particular, when the fault behavior is more complex.
机译:我们提出了一个概率框架,其中可以组合与断层上大地震的复发有关的不同类型的信息,以约束候选递归模型的参数空间,并提供知道所选数据集和先​​验条件的模型的最佳组合。我们使用贝叶斯推断进行参数和误差估计,使用图形模型(贝叶斯网络)进行建模,并使用随机建模将累积偏移量(CO)链接到同震滑动。基于累积偏移的贝叶斯方法(COBBRA)方法(Fitzenz等人,2010)最初是为了使用CO数据进一步约束和区分从大地震的历史和考古目录(CLE)建立的递归模型而开发的。我们讨论了这种方法,并提出了结合沟槽数据(TD)的扩展。对于我们的案例研究(约旦河谷断层(JVF)),每种模型的相对证据都偏爱布朗通行时间(BPT)和对数正态模型。我们强调(1)断层滑动率的时间变化对于约束递归模型至关重要; (2)古地震事件的概率密度函数(PDF)的形状非常重要,在大多数情况下不是高斯分布,应报告其复杂性; (3)更新模型是根据连续地震之间的间隔而不是日期来确定的,算法应考虑到这一事实; (4)最大似然法不足以进行参数不确定性评估和模型组合或排序。最后,还需要做更多的工作来定义适当的先验并为累积滑动和同震滑动之间的关系建模,尤其是在断层行为更为复杂的情况下。

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