Machine learning assisted geophysical characterization of deep-seated upper jurassic carbonate deposits in Penobscot Field, Nova Scotia

IF 4.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Physics and Chemistry of the Earth Pub Date : 2025-06-01 Epub Date: 2025-01-27 DOI:10.1016/j.pce.2025.103876
Vijay Kumar , Satya Narayan , S.D. Sahoo , Brijesh Kumar , S.K. Pal
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Abstract

Carbonate rocks hold significant potential for economic activities, including mineral and hydrocarbon exploration, highlighting the importance of detailed characterization. This study focuses on delineating and characterizing deep-seated Upper Jurassic carbonate deposits (Abenaki Formation) in the Penobscot Field using model-based inversion (MBI) and machine learning (ML) algorithms. The MBI model achieved 94.3% correlation with a relatively lower error of 605.8 m/s∗g/cm3 in impedance estimation. The ML models were evaluated using metrics such as precision, recall, F1 score, accuracy, and misclassification rates. The XGB model consistently outperformed the RF, ANN, and SVM models, achieving the highest precision, recall, F1 score, and accuracy across shale, sand, and carbonate facies classifications. It recorded an overall accuracy of 0.927 and a misclass rate of 0.073, surpassing SVM (accuracy: 0.901, misclass: 0.099), RF (accuracy: 0.866 & misclass: 0.134), and ANN (accuracy: 0.838 & misclass: 0.162). Furthermore, the effective porosity volume was predicted with a correlation of 85.75% and a mean absolute error of 0.02. It was found that the Artimon Member (∼85 m) includes an upper porous carbonate reservoir unit (∼35 m) with impedance 11,500–15,000 m/s∗g/cm3, carbonate probability 70–80% and porosity 12–15%, and a deeper siliciclastic unit (∼45 m) with impedance 9500–13,000 m/s∗g/cm3, carbonate probability 20–30% and porosity nearly 3–4% possibly during a significant transgressive phase of sea-level rise. The underlying Baccaro Member (∼260 m) predominantly comprises thick carbonate facies with impedance 12,500–16,000 m/s∗g/cm3, carbonate probability 80–90% and porosity nearly 6–9%. This quantitative study examines how depositional environments, mineralization, and diagenesis shape the distribution of carbonate facies in the Penobscot Field. By integrating advanced seismic inversion with machine learning, it refines the characterization of deep-seated carbonate facies, offering insights for identifying potential carbonate hydrocarbon bearing zones worldwide.
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机器学习辅助新斯科舍Penobscot油田深部上侏罗统碳酸盐岩矿床的地球物理表征
碳酸盐岩具有巨大的经济活动潜力,包括矿物和碳氢化合物勘探,突出了详细表征的重要性。本研究的重点是利用基于模型的反演(MBI)和机器学习(ML)算法,对Penobscot油田深部上侏罗统碳酸盐沉积(Abenaki组)进行圈定和表征。MBI模型的阻抗估计误差为605.8 m/s∗g/cm3,相关系数为94.3%。使用精度、召回率、F1分数、准确性和错误分类率等指标对ML模型进行评估。XGB模型始终优于RF、ANN和SVM模型,在页岩、砂岩和碳酸盐相分类中实现了最高的精度、召回率、F1分数和准确性。总体准确率为0.927,错类率为0.073,超过了支持向量机(准确率0.901,错类0.099)和射频(准确率0.866 &;误分类:0.134)和人工神经网络(准确率:0.838 &;misclass: 0.162)。预测有效孔隙度体积的相关系数为85.75%,平均绝对误差为0.02。发现Artimon段(~ 85 m)包括一个阻抗为11,500 ~ 15,000 m/s∗g/cm3,碳酸盐概率为70 ~ 80%,孔隙度为12 ~ 15%的上部多孔碳酸盐储层单元(~ 35 m)和一个阻抗为9500 ~ 13,000 m/s∗g/cm3,碳酸盐概率为20 ~ 30%,孔隙度接近3 ~ 4%的深部硅屑层单元(~ 45 m),可能在海平面上升的显著海侵阶段。下伏Baccaro段(~ 260 m)主要为厚碳酸盐相,阻抗为12500 ~ 16000 m/s∗g/cm3,碳酸盐概率为80 ~ 90%,孔隙度接近6 ~ 9%。这项定量研究考察了沉积环境、矿化和成岩作用如何塑造了Penobscot油田碳酸盐岩相的分布。通过将先进的地震反演技术与机器学习技术相结合,该技术可以改善深层碳酸盐岩相的特征,为识别全球潜在的碳酸盐岩含油气带提供见解。
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来源期刊
Physics and Chemistry of the Earth
Physics and Chemistry of the Earth 地学-地球科学综合
CiteScore
5.40
自引率
2.70%
发文量
176
审稿时长
31.6 weeks
期刊介绍: Physics and Chemistry of the Earth is an international interdisciplinary journal for the rapid publication of collections of refereed communications in separate thematic issues, either stemming from scientific meetings, or, especially compiled for the occasion. There is no restriction on the length of articles published in the journal. Physics and Chemistry of the Earth incorporates the separate Parts A, B and C which existed until the end of 2001. Please note: the Editors are unable to consider submissions that are not invited or linked to a thematic issue. Please do not submit unsolicited papers. The journal covers the following subject areas: -Solid Earth and Geodesy: (geology, geochemistry, tectonophysics, seismology, volcanology, palaeomagnetism and rock magnetism, electromagnetism and potential fields, marine and environmental geosciences as well as geodesy). -Hydrology, Oceans and Atmosphere: (hydrology and water resources research, engineering and management, oceanography and oceanic chemistry, shelf, sea, lake and river sciences, meteorology and atmospheric sciences incl. chemistry as well as climatology and glaciology). -Solar-Terrestrial and Planetary Science: (solar, heliospheric and solar-planetary sciences, geology, geophysics and atmospheric sciences of planets, satellites and small bodies as well as cosmochemistry and exobiology).
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