Deep Learning Method for Latent Space Analysis

B. Wallet, T. Ha
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Abstract

Seismic attributes are a well-established method for highlighting subtle features buried in seismic data in order to improve interpretability and suitability for quantitative analysis. Seismic attributes are a critical enabling technology in such areas thin bed analysis, 3D geobody extraction, and seismic geomorphology. When it comes to seismic attributes, we often suffer from an "abundance of riches" as the high dimensionality of seismic attributes may cause great difficulty in accomplishing even simple tasks. Spectral decomposition, for instance, typically produces 10's and sometimes 100's of attributes. However, when it comes to visualization, for instance, we are limited to visualizing three or at most four attributes simultaneously. My co-authors and I first proposed the use of latent space analysis to reduce the dimensionality of seismic attributes in 2009. At the time, we focused upon the use of non-linear methods such as self-organizing maps (SOM) and generative topological maps (GTM). Since then, many other researchers have significantly expanded the list of unsupervised methods as well as supervised learning. Additionally, latent space methods have been adopted in a number of commercial interpretation and visualization software packages. In this paper, we introduce a novel deep learning-based approach to latent space analysis. This method is superior in that it is able to remove redundant information and focus upon capturing essential information rather than just focusing upon probability density functions or clusters in a high dimensional space. Furthermore, our method provides a quantitative way to assess the fit of the latent space to the original data. We apply our method to a seismic data set from the Canterbury Basin, New Zealand. We examine the goodness of fit of our model by comparing the input data to what can be reproduced from the reduced dimensional data. We provide an interpretation based upon our method.
潜在空间分析的深度学习方法
地震属性是一种行之有效的方法,用于突出地震数据中隐藏的细微特征,以提高定量分析的可解释性和适用性。地震属性是薄层分析、三维地质体提取和地震地貌学等领域的关键技术。当涉及到地震属性时,我们经常会遇到“富余”的问题,因为地震属性的高维可能会给完成简单的任务带来很大的困难。例如,光谱分解通常会产生10个甚至100个属性。然而,当涉及到可视化时,例如,我们被限制为同时可视化三个或最多四个属性。我和我的合著者在2009年首次提出使用潜在空间分析来降低地震属性的维数。当时,我们专注于使用非线性方法,如自组织映射(SOM)和生成拓扑映射(GTM)。从那时起,许多其他研究人员大大扩展了无监督方法和监督学习的列表。此外,许多商业解释和可视化软件包都采用了潜在空间方法。在本文中,我们介绍了一种新的基于深度学习的潜在空间分析方法。该方法的优点在于能够去除冗余信息,专注于捕获基本信息,而不是仅仅关注高维空间中的概率密度函数或聚类。此外,我们的方法提供了一种定量的方法来评估潜在空间与原始数据的拟合程度。我们将该方法应用于新西兰坎特伯雷盆地的地震数据集。我们通过将输入数据与降维数据进行比较来检验模型的拟合优度。我们根据我们的方法提供一种解释。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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