Calibration, Validation and Evaluation of Machine Learning Thermobarometers in Metamorphic Petrology: An Application to Biotite and Outlook for Future Strategy

IF 3.4 2区 地球科学 Q1 GEOLOGY
Philip Hartmeier, Jacob B. Forshaw, Pierre Lanari
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Abstract

Geothermobarometry provides crucial constraints on the physical conditions of metamorphism, offering insights into petrogenetic processes and providing key information on thermal regimes and metamorphic depths to other geological disciplines. However, calibrating a thermobarometer from the natural record is challenging because independent pressure (P) and temperature (T) estimates are required, and the compositional variation of minerals—governed by multiple metamorphic reactions—must be captured in a complex function. This work calibrates a machine learning thermobarometer for biotite using relative PT estimates based on mineral assemblage sequences. A neural network is used as a flexible model to fit a high-dimensional thermobarometric regression curve. To address the challenge of sparse training data, a transfer learning strategy is employed, where the model is primarily trained on a large dataset generated with phase equilibrium modelling before refinement with natural data. A general framework for calibrating machine learning thermobarometers is outlined using a neural network thermobarometer for biotite as an example. Selection of the best-performing model is guided by k-fold cross-validation alongside complementary accuracy checks using metamorphic sequences and precision assessments via Monte Carlo error propagation. Evaluation on an independent test dataset, compiled from the literature, indicates that the model is a potential biotite single-crystal thermometer with a root mean square error of ± 45°C, consistent with the estimated uncertainty of Ti-in-Bt thermometry applied to the same data. A potential barometer is affected by systematic underestimation of pressures above 0.6 GPa due to regression to the mean of the natural database, which is biased towards low-pressure metamorphism. This limits its applicability in higher-pressure regimes. This study highlights the potential of using neural networks with transfer learning in petrological applications since they are often constrained by limited natural data.

Abstract Image

变质岩石学中机器学习温度计的校准、验证和评估:在黑云母上的应用及未来策略展望
地温测压法对变质作用的物理条件提供了关键的约束,为岩石形成过程提供了见解,并为其他地质学科提供了热状态和变质深度的关键信息。然而,从自然记录中校准温度计是具有挑战性的,因为需要独立的压力(P)和温度(T)估计,并且矿物的成分变化(由多重变质反应控制)必须在一个复杂的函数中捕获。这项工作使用基于矿物组合序列的相对P-T估计校准黑云母的机器学习温度计。采用神经网络作为柔性模型拟合高维热气压回归曲线。为了解决稀疏训练数据的挑战,采用了一种迁移学习策略,在使用自然数据进行细化之前,模型首先在由相平衡建模生成的大型数据集上进行训练。以黑云母神经网络温度计为例,概述了校准机器学习温度计的一般框架。最佳表现模型的选择由k-fold交叉验证指导,同时使用变质序列进行互补精度检查,并通过蒙特卡罗误差传播进行精度评估。根据文献编制的独立测试数据集进行的评估表明,该模型是一个潜在的黑云母单晶温度计,其均方根误差为±45°C,与应用于相同数据的Ti-in-Bt测温法的估计不确定度一致。由于回归到自然数据库的平均值,系统地低估了0.6 GPa以上的压力,这对潜在的气压表有影响,这偏向于低压变质作用。这限制了它在高压环境中的适用性。这项研究强调了在岩石学应用中使用神经网络和迁移学习的潜力,因为它们通常受到有限的自然数据的限制。
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来源期刊
CiteScore
6.60
自引率
11.80%
发文量
57
审稿时长
6-12 weeks
期刊介绍: The journal, which is published nine times a year, encompasses the entire range of metamorphic studies, from the scale of the individual crystal to that of lithospheric plates, including regional studies of metamorphic terranes, modelling of metamorphic processes, microstructural and deformation studies in relation to metamorphism, geochronology and geochemistry in metamorphic systems, the experimental study of metamorphic reactions, properties of metamorphic minerals and rocks and the economic aspects of metamorphic terranes.
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