Document généré le 20/05/2026 depuis l'adresse: https://www.documentation.eauetbiodiversite.fr/fr/notice/rock-mineral-volume-inversion-using-statistical-and-machine-learning-algorithms-for-enhanced-geothermal-systems-in-upper-rhine-graben-eastern-france
Rock Mineral Volume Inversion Using Statistical and Machine Learning Algorithms for Enhanced Geothermal Systems in Upper Rhine Graben, Eastern France
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8-4645782
Identifiant OAI
4645782
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https://brgm.hal.science/hal-04630958v2
Auteur(s):
Joshua Pwavodi,Marquis Guy,Maurer Vincent,Glaas Carole,Montagud Anais,Formento Jean‐luc,Genter Albert,Darnet Mathieu
Mots clés
Advancing Interpretable AI
Date de publication
01/06/2024
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Description
Accurately determining the mineralogical composition of rocks is essential for precise assessments of key petrophysical properties like effective porosity, water saturation, clay volume, and permeability. Mineral volume inversion is particularly critical in geological contexts characterized by heterogeneity, such as in the Upper Rhine Graben (URG), where both carbonate and siliciclastic formations are prevalent. The estimation of mineral volumes poses challenges that involve both linear and nonlinear relationships associated with geophysical data. To address this complexity, our methodology strategically integrates the robust insights from standard statistical approaches with three machine learning (ML) algorithms: multi‐layer perceptron, random forest regression, and gradient boosting regression. Furthermore, we propose a new hybrid ensemble model that incorporates a weighted average of multiple ML approaches to predict mineral composition within the Muschelkalk and Buntsandstein formations of the URG. ML techniques for mineral composition prediction in these formations exhibit robust predictive performance. The predicted mineral volumes align closely with quantitative estimates derived from X‐ray diffraction analysis. Additionally, they are in good qualitative agreement with mineral descriptions obtained from cores and cuttings of the Muschelkalk and Buntsandstein formations.
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