Calculating amphibole formula from electron microprobe analysis data using a machine learning method based on principal components regression

被引:47
作者
Li, Xiaoyan [1 ,2 ]
Zhang, Chao [1 ,2 ]
Behrens, Harald [2 ]
Holtz, Francois [2 ]
机构
[1] Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China
[2] Leibniz Univ Hannover, Inst Mineral, D-30167 Hannover, Germany
基金
中国国家自然科学基金;
关键词
Amphibole formula; Amphibole nomenclature; Machine learning; Principal components regression; Electron microprobe analysis; HIGH-TEMPERATURE BEHAVIOR; FERRIC IRON; CRYSTAL-CHEMISTRY; CALCIC AMPHIBOLES; SODIC AMPHIBOLES; FE OXIDATION; MODEL; BIOTITE; TI; DEPROTONATION;
D O I
10.1016/j.lithos.2020.105469
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Wepresent a new method for calculating amphibole formula from routine electron microprobe analysis (EMPA) data by applying a principal components regression (PCR)-based machine learning algorithm on reference amphibole data. The reference amphibole data collected from literature are grouped in two datasets, for Li-free and Li-bearing amphiboles respectively, which include Fe2+, Fe3+, OH contents and the ion site assignments determined by single crystal structure refinement. We established two PCR models, for Li-free and Li-bearing amphiboles respectively, by the 10-fold cross validation of training datasets and evaluated by independent test datasets. The results show that our models can successfully reproduce the reference data for most ions with an error less than +/- 0.01 atom per formula unit (apfu), for Fe3+ within an error less than +/- 0.2 apfu and for (OH)-O-W and O-W(2-) with errors less than +/- 0.3 apfu. The error in estimated Fe3+/Sigma Fe ratio shows a rough negative dependence on FeOT content (total iron expressed as FeO), ranging within +/- 0.3 for amphiboles with FeOT >= 5 wt% and within +/- 0.2 for amphiboles with FeOT >= 10 wt%. Our models are applicable to both (W)(OH, F, Cl)-dominant and O-W-dominant amphiboles. It is notable that this method is not suitable for calculating mineral formula of amphiboles that have been affected by deprotonation as a result of secondary oxidation, but it could offer an estimation of initial (OH)-O-W prior to the post-formation oxidation. A user-friendly Excel worksheet is provided with two independent PCR models for calculating the formula of Li-free amphibole and Li-bearing amphibole, respectively. An automatic nomenclature function is also provided according to the nomenclature criteria of the 2012 International Mineralogical Association (IMA) report. (C) 2020 Elsevier B.V. All rights reserved.
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页数:13
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