Quantifying and Analyzing the Uncertainty in Fault Interpretation Using Entropy

IF 2.8 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Zhicheng Lei
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Abstract

Fault interpretation in geology inherently involves uncertainty, which has driven the need to develop methods to quantify and analyze this uncertainty. This paper introduces a novel framework for this task by integrating graph theory, entropy, and random walk. The proposed approach employs graph theory to mathematically represent a fault network in both map-view and profile sections. By integrating the theory of two-dimensional random walk, the stochastic nature of the fault growth process can be effectively characterized, enabling the development of tailored probability formulations for the fault network through weighted graph theory. In addition, entropy models tailored to the fault network are formulated, providing a solid foundation for uncertainty quantification and analysis. Furthermore, the proposed method employs the principle of increase of entropy to quantitatively assess the uncertainty involved in comparing different fault networks. A case study is presented to demonstrate the practical application in addressing the challenges associated with quantifying, communicating, and analyzing the uncertainty in fault interpretation. The findings obtained in this study suggest that (1) entropy serves as a reliable metric for measuring and communicating the uncertainty in fault interpretation; (2) entropy can be used to estimate the potential numbers of evolutionary paths available for a fault network; and (3) the growth process of a fault network adheres to the principle of increase of entropy, enabling us to utilize entropy to measure the complexity of the fault network and subsequently compare the differences between various fault networks. The results obtained highlight the potential of this approach not only for understanding the geological meaning of uncertainty in fault interpretation but also for enhancing decision-making in related fields.

Abstract Image

利用熵对断层解释中的不确定性进行量化和分析
地质学中的断层解释本质上涉及不确定性,因此需要开发量化和分析这种不确定性的方法。本文通过整合图论、熵和随机漫步,为这项任务引入了一个新颖的框架。所提出的方法采用图论,在地图视图和剖面图中以数学方式表示断层网络。通过整合二维随机游走理论,可以有效地描述故障增长过程的随机性质,从而通过加权图论为故障网络制定量身定制的概率公式。此外,还制定了针对故障网络的熵模型,为不确定性量化和分析提供了坚实的基础。此外,所提出的方法还采用了熵增加原理,对比较不同故障网络所涉及的不确定性进行定量评估。本研究还通过一个案例,展示了该方法在应对与故障解释中不确定性的量化、交流和分析相关的挑战方面的实际应用。研究结果表明:(1) 熵是衡量和交流故障解释不确定性的可靠指标;(2) 熵可用于估算故障网络的潜在演化路径数量;(3) 故障网络的增长过程遵循熵增加的原则,使我们能够利用熵来衡量故障网络的复杂性,进而比较不同故障网络之间的差异。所获得的结果凸显了这一方法的潜力,它不仅有助于理解断层解释中不确定性的地质含义,还有助于加强相关领域的决策。
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来源期刊
Mathematical Geosciences
Mathematical Geosciences 地学-地球科学综合
CiteScore
5.30
自引率
15.40%
发文量
50
审稿时长
>12 weeks
期刊介绍: Mathematical Geosciences (formerly Mathematical Geology) publishes original, high-quality, interdisciplinary papers in geomathematics focusing on quantitative methods and studies of the Earth, its natural resources and the environment. This international publication is the official journal of the IAMG. Mathematical Geosciences is an essential reference for researchers and practitioners of geomathematics who develop and apply quantitative models to earth science and geo-engineering problems.
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