4.6 Article

Estimating the thermal conductivity of plutonic rocks from major oxide composition using machine learning

Journal

GEOPHYSICAL JOURNAL INTERNATIONAL
Volume 234, Issue 3, Pages 2143-2159

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/gji/ggad193

Keywords

Composition and structure of the continental crust; Heat flow; Heat generation and transport; Thermal conductivity; Plutonic rocks

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This study compiles a comprehensive dataset of 530 representative plutonic rock samples, including thermal conductivity, major oxide composition, and modal mineralogy. Three machine learning algorithms are employed to estimate the thermal conductivity of plutonic rocks using the major oxide composition feature. Results show that the machine learning models outperform non-ML models and achieve high prediction accuracy.
The accurate estimation of temperature distribution in the earth's crust and modelling of heat-related processes in geodynamics requires knowledge of the thermal conductivity of plutonic rocks. This study compiled an extensive data set of 530 representative plutonic rock samples, including thermal conductivity, major oxide composition and (for two subsets of data) modal mineralogy. For the first time, three machine learning algorithms (ML; i.e. support vector regression, random forest and extreme gradient boosting) were employed to estimate the thermal conductivity of plutonic rocks using the major oxide composition feature as input variables. The performance of these ML-based models was evaluated against a geochemically compositional model and eight mineral-driven physically based empirical mixing models. Results show that the means of predicted thermal conductivity by the ML-based models and the geochemically compositional model are not significantly different from the measured thermal conductivity at a significance level of 5 per cent. However, the ML-based models outperformed the best-performing non-ML model, the geochemically compositional model. The highest prediction accuracy was achieved by extreme gradient boosting, which reduced the mean absolute percentage error and root mean square error by more than 50 per cent. Furthermore, SiO2 is confirmed as the most important independent variable, followed by Al2O3, TiO2, CaO and K2O. The turning point observed in the thermal conductivity trend with SiO2 wt per cent may be primarily attributed to variations in mineral composition within the subgroup of igneous rock types classified based on SiO2 wt per cent. This study explores, for the first time, the use of ML algorithms to estimate the thermal conductivity of plutonic rocks from their major oxide composition.

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