Markov Chain Monte Carlo Methods for High-dimensional Mixture Distributions

L. D. Figueiredo, D. Grana, M. Roisenberg, B. B. Rodrigues
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Abstract

Summary We present a Markov chain Monte Carlo method for the computation of the posterior distribution of discrete and continuous properties in geophysical inverse problems. Mixture distributions, Gaussian or non-parametric, have been proposed to model the multimodal behaviour or subsurface properties. However, due to the spatial correlation of subsurface properties, the number of modes of the mixture distribution increases exponentially with the number of samples in the data vector. In this work, we propose a new Markov chain Monte Carlo method based on two steps. First, we update the configuration of the discrete property (for example, facies or rock types), then we update the configuration of the continuous properties (for example, elastic or petrophysical properties). The first step can be performed according to a jump move, where a new configuration is proposed, or a local move, where the configuration of the previous iteration is preserved. The second step is performed by sampling the new configuration of continuous properties either from the analytical expression of the Gaussian distribution of the continuous properties conditioned by the facies configuration in the Gaussian-linear case, or by numerically sampling from the non-parametric conditional distribution in the non-Gaussian and non-linear case. The methodology is demonstrated through the application to synthetic and real datasets.
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高维混合分布的马尔可夫链蒙特卡罗方法
提出了一种计算地球物理反演问题中离散和连续性质后验分布的马尔可夫链蒙特卡罗方法。混合分布,高斯或非参数,已经提出了模型的多模态行为或地下性质。然而,由于地下性质的空间相关性,混合分布的模态数量随着数据向量中样本的数量呈指数增长。本文提出了一种新的基于两步的马尔可夫链蒙特卡罗方法。首先,我们更新离散属性的配置(例如,相或岩石类型),然后我们更新连续属性的配置(例如,弹性或岩石物理属性)。第一步可以根据跳跃移动执行,其中提出了新的配置,或者根据本地移动执行,其中保留了前一次迭代的配置。第二步是对连续属性的新配置进行采样,或者在高斯-线性情况下,从由相配置决定的连续属性的高斯分布的解析表达式中,或者在非高斯和非线性情况下,从非参数条件分布中进行数值采样。通过对合成数据集和实际数据集的应用,验证了该方法的有效性。
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