Márcio Vinicius Santana Dantas , Kaio Henrique Masse Vieira , Thomás Jung Spier , José Arthur Oliveira Santos , Alan Cabral Trindade Prado , Danilo Vomlel , Mariana Leite , Felipe Alves Farias , Daniel Galvão Carnier Fragoso , Humberto Reis , Gabriel Coutinho , Douglas G. Macharet
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引用次数: 0
Abstract
Performing the high-resolution stratigraphic analysis may be challenging and time-consuming if one has to work with large datasets. Moreover, sedimentary records have signals of different frequencies and intrinsic noise, resulting in a complex signature that is difficult to identify only through eyes-based analysis. This work proposes identifying transgressive-regressive (T-R) sequences from carbonate facies successions of three South American basins: (i) São Francisco Basin - Brazil, (ii) Santos Basin - Brazil, and (iii) Salta Basin - Argentina. We applied a hidden Markov model in an unsupervised approach followed by a Score-Based Recommender System that automatically finds medium or low-frequency sedimentary cycles from high-frequency ones. Our method is applied to facies identified using Fullbore Formation Microimager (FMI) logs, outcrop description, and composite logs from carbonate intervals. The automatic recommendation results showed better long-distance correlations between medium- to low-frequency sedimentary cycles, whereas the hidden Markov model method successfully identified high-resolution (high-frequency) transgressive and regressive systems tracts from the given facies successions. Our workflow offers advances in the automated analyses and construction of lower- to higher-rank stratigraphic framework and short to long-distance stratigraphic correlation, allowing for large-scale automated processing of the basin dataset. Our approach in this work fits the unsupervised learning framework, as we require no previous input of stratigraphical analysis in the basin. The results provide solutions for prospecting any sediment-hosted mineral resource, especially for the oil and gas industry, offering support for subsurface geological characterization, whether at the exploration scale or for reservoir zoning during production development.
如果必须处理大型数据集,那么进行高分辨率地层分析可能是具有挑战性和耗时的。此外,沉积记录具有不同频率的信号和固有噪声,这导致了复杂的特征,仅通过肉眼分析很难识别。本文提出了从三个南美盆地(1)巴西s o Francisco盆地、(2)巴西Santos盆地和(3)阿根廷Salta盆地的碳酸盐岩相序列中识别海侵-退(T-R)层序的方法。我们在无监督的方法中应用了隐马尔可夫模型,然后是基于分数的推荐系统,该系统自动从高频沉积旋回中发现中低频沉积旋回。我们的方法应用于通过全孔地层微成像仪(FMI)测井、露头描述和碳酸盐岩层段的复合测井来识别相。自动推荐结果显示中低频沉积旋回之间具有较好的长距离相关性,而隐马尔可夫模型方法则成功地从给定的相序列中识别出高分辨率(高频)海侵和海退体系域。我们的工作流程在低阶到高阶地层格架的自动化分析和构建以及短距离到长距离地层对比方面取得了进展,从而允许对盆地数据集进行大规模的自动化处理。我们在这项工作中的方法适合无监督学习框架,因为我们不需要事先输入盆地的地层分析。研究结果为任何含沉积物矿产资源的勘探提供了解决方案,特别是对油气行业来说,无论是在勘探规模上还是在生产开发过程中进行储层划分,都为地下地质特征提供了支持。