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Geochemical discrimination and characteristics of magmatic tectonic settings; a machine learning-based approach

机译:岩浆构造的地球化学识别与特征   设置;基于机器学习的方法

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摘要

Geochemically discriminating between magmatism in different tectonic settingsremains a fundamental part of understanding the processes of magma generationwithin the Earth's mantle. Here, we present an approach where machine-learning(ML) methods are used for quantitative tectonic discrimination and featureselection using global geochemical datasets containing data for volcanic rocksgenerated in eight different tectonic settings. This study uses support vectormachine, random forest, and sparse multinomial regression (SMR) approaches. Allthese ML methods with data for 20 elements and 5 isotopic ratios allowed thesuccessful geochemical discrimination between igneous rocks formed in eightdifferent tectonic settings with a discriminant ratio better than 83% for allsettings barring oceanic plateaus and back-arc basins. SMR is a particularlypowerful and interpretable ML method because it quantitatively identifiesgeochemical signatures that characterize the tectonic settings of interest andthe characteristics of each sample as a probability of the membership of thesample for each setting. We also present the most representative basaltcomposition for each tectonic setting. The new data provide reference pointsfor future geochemical discussions. Our results indicate that at least 17elements and isotopic ratios are required to characterize each tectonicsetting, suggesting that geochemical tectonic discrimination cannot be achievedusing only a small number of elemental compositions and/or isotopic ratios. Theresults show that volcanic rocks formed in different tectonic settings haveunique geochemical signatures, indicating that both volcanic rock geochemistryand magma generation processes are closely connected to the tectonic setting.
机译:从地球化学上区分不同构造环境中的岩浆仍是了解地幔内部岩浆生成过程的基本部分。在这里,我们提出一种方法,其中使用机器学习(ML)方法进行定量构造判别和特征选择,方法是使用全球地球化学数据集,其中包含在八个不同构造环境中生成的火山岩的数据。本研究使用支持向量机,随机森林和稀疏多项式回归(SMR)方法。所有这些具有20个元素和5个同位素比率的数据的ML方法都可以成功地区分在八种不同构造环境中形成的火成岩,对于除海洋高原和后弧盆地以外的所有环境,判别比率均优于83%。 SMR是一种特别强大且可解释的ML方法,因为它定量地标识了地球化学特征,这些特征表征了感兴趣的构造环境和每个样本的特征,作为每个环境下样本成员资格的概率。我们还为每种构造背景提供了最具代表性的玄武岩成分。新数据为将来的地球化学讨论提供参考。我们的结果表明,至少需要17个元素和同位素比来表征每个构造背景,这表明仅使用少量的元素组成和/或同位素比就无法实现地球化学构造的区分。结果表明,不同构造背景下形成的火山岩具有独特的地球化学特征,表明火山岩的地球化学和岩浆生成过程均与构造背景密切相关。

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