Earth Science Frontiers ›› 2024, Vol. 31 ›› Issue (4): 417-428.DOI: 10.13745/j.esf.sf.2023.9.2
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ZHANG Huanbao1(), HE Haiyang1,*(
), YANG Shijiao1, LI Yalin2, BI Wenjun3, HAN Shili1, GUO Qinpeng1, DU Qing1
Received:
2023-05-26
Revised:
2023-07-27
Online:
2024-07-25
Published:
2024-07-10
CLC Number:
ZHANG Huanbao, HE Haiyang, YANG Shijiao, LI Yalin, BI Wenjun, HAN Shili, GUO Qinpeng, DU Qing. Machine learning-based approach for adakitic rocks tectonic setting determination[J]. Earth Science Frontiers, 2024, 31(4): 417-428.
序号 | 构造背景类型 | 数据量/条 |
---|---|---|
1 | 汇聚板块边缘 | 583 |
2 | 板内火山活动 | 315 |
3 | 太古宙克拉通(包括绿岩带) | 177 |
Table 1 Quantity of major and trace element data of adakitic rocks from different sources
序号 | 构造背景类型 | 数据量/条 |
---|---|---|
1 | 汇聚板块边缘 | 583 |
2 | 板内火山活动 | 315 |
3 | 太古宙克拉通(包括绿岩带) | 177 |
Fig.4 (a) Confusion matrix based on validation results of Gaussian SVM classifier; (b) Learning curve of Gaussian SVM classifier in classifying different tectonic setting types of adakitic rock
Fig.5 Comparison of four machine learning classification algorithms on the decision problem of distinguishing different tectonic setting types of adakitic rocks
主成分 | 特征元素组合的权重 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Sr/Nd | Ba | Ce | SiO2/La | Al2O3/Ba | Sr/Hf | Rb/Ni | Sr/Pr | Sr/Zr | Sr/La | TiO2/CaO | Pr | |
PC1 (46.0%) | 0.398 07 | 0.025 32 | -0.293 69 | 0.277 49 | 0.001 62 | 0.310 43 | -0.205 32 | 0.408 68 | 0.291 53 | 0.398 02 | -0.219 01 | -0.283 56 |
PC2 (31.2%) | 0.132 42 | 0.460 18 | 0.343 38 | -0.352 9 | -0.451 24 | 0.234 32 | -0.118 09 | 0.114 08 | 0.279 38 | 0.116 22 | 0.167 87 | 0.350 74 |
Table 3 The PCA component matrix of important characteristic elements
主成分 | 特征元素组合的权重 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Sr/Nd | Ba | Ce | SiO2/La | Al2O3/Ba | Sr/Hf | Rb/Ni | Sr/Pr | Sr/Zr | Sr/La | TiO2/CaO | Pr | |
PC1 (46.0%) | 0.398 07 | 0.025 32 | -0.293 69 | 0.277 49 | 0.001 62 | 0.310 43 | -0.205 32 | 0.408 68 | 0.291 53 | 0.398 02 | -0.219 01 | -0.283 56 |
PC2 (31.2%) | 0.132 42 | 0.460 18 | 0.343 38 | -0.352 9 | -0.451 24 | 0.234 32 | -0.118 09 | 0.114 08 | 0.279 38 | 0.116 22 | 0.167 87 | 0.350 74 |
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