Earth Science Frontiers ›› 2022, Vol. 29 ›› Issue (5): 464-475.DOI: 10.13745/j.esf.sf.2022.2.75
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ZHU Ziyi1(), ZHOU Fei1, WANG Yu1, ZHOU Tong1, HOU Zhaoliang2, QIU Kunfeng1,3,*()
Received:
2021-12-16
Revised:
2022-03-18
Online:
2022-09-25
Published:
2022-08-24
Contact:
QIU Kunfeng
CLC Number:
ZHU Ziyi, ZHOU Fei, WANG Yu, ZHOU Tong, HOU Zhaoliang, QIU Kunfeng. Machine learning-based approach for zircon classification and genesis determination[J]. Earth Science Frontiers, 2022, 29(5): 464-475.
判别图解 | 准确率/% | |||
---|---|---|---|---|
岩浆锆石 | 热液锆石 | 变质锆石 | 平均 | |
Th/U | 81.65 | - | 23.5 | 73.1 |
LaN-(Sm/La)N | 42.4 | 20.9 | - | 38.5 |
Table 1 The accuracy of the published diagram to classify different zircon provenance
判别图解 | 准确率/% | |||
---|---|---|---|---|
岩浆锆石 | 热液锆石 | 变质锆石 | 平均 | |
Th/U | 81.65 | - | 23.5 | 73.1 |
LaN-(Sm/La)N | 42.4 | 20.9 | - | 38.5 |
序号 | 母岩类型 | 数据量 | 参考文献 |
---|---|---|---|
1 | 岩浆锆石 | 2466 | [ |
2 | 热液锆石 | 508 | [ |
3 | 变质锆石 | 524 | [ |
Table 2 Published data of zircon trace elements from different provenance
序号 | 母岩类型 | 数据量 | 参考文献 |
---|---|---|---|
1 | 岩浆锆石 | 2466 | [ |
2 | 热液锆石 | 508 | [ |
3 | 变质锆石 | 524 | [ |
元素 | 元素数据缺失率 | 元素 | 元素数据缺失率 | ||||
---|---|---|---|---|---|---|---|
热液 锆石 | 岩浆 锆石 | 变质 锆石 | 热液 锆石 | 岩浆 锆石 | 变质 锆石 | ||
La | 0% | 7% | 23% | Tm | 4% | 1% | 17% |
Ce | 0% | 0% | 0% | Yb | 0% | 0% | 0% |
Pr | 0% | 1% | 4% | Lu | 0% | 0% | 12% |
Nd | 0% | 0% | 2% | Y | 20% | 7% | 38% |
Sm | 0% | 0% | 1% | Hf | 27% | 8% | 41% |
Eu | 1% | 0% | 1% | Nb | 38% | 23% | 58% |
Gd | 0% | 0% | 0% | Ta | 36% | 67% | 65% |
Tb | 5% | 1% | 20% | Ti | 40% | 23% | 47% |
Dy | 0% | 0% | 0% | Pb | 42% | 79% | 78% |
Ho | 5% | 0% | 14% | Th | 13% | 2% | 15% |
Er | 0% | 0% | 2% | U | 13% | 2% | 15% |
Table 3 Missing data of zircon trace elements from different provenance
元素 | 元素数据缺失率 | 元素 | 元素数据缺失率 | ||||
---|---|---|---|---|---|---|---|
热液 锆石 | 岩浆 锆石 | 变质 锆石 | 热液 锆石 | 岩浆 锆石 | 变质 锆石 | ||
La | 0% | 7% | 23% | Tm | 4% | 1% | 17% |
Ce | 0% | 0% | 0% | Yb | 0% | 0% | 0% |
Pr | 0% | 1% | 4% | Lu | 0% | 0% | 12% |
Nd | 0% | 0% | 2% | Y | 20% | 7% | 38% |
Sm | 0% | 0% | 1% | Hf | 27% | 8% | 41% |
Eu | 1% | 0% | 1% | Nb | 38% | 23% | 58% |
Gd | 0% | 0% | 0% | Ta | 36% | 67% | 65% |
Tb | 5% | 1% | 20% | Ti | 40% | 23% | 47% |
Dy | 0% | 0% | 0% | Pb | 42% | 79% | 78% |
Ho | 5% | 0% | 14% | Th | 13% | 2% | 15% |
Er | 0% | 0% | 2% | U | 13% | 2% | 15% |
模型 | 准确率 | 最优超参数 |
---|---|---|
SVM(linear) | 0.868 | C = 16 |
SVM(RBF) | 0.802 | C=16,gamma = 0.5 |
KNN | 0.860 | weights = distance, n neighbors = 1 |
ANN | 0.899 | alpha = 0.001, activation = tanh, hidden layer sizes = (20,1) |
Random Forest | 0.878 | n estimators = 100, max depth = 30, max features = 16 |
Table 4 Hyper-parameters of the 4 models and the accuracy on the test set
模型 | 准确率 | 最优超参数 |
---|---|---|
SVM(linear) | 0.868 | C = 16 |
SVM(RBF) | 0.802 | C=16,gamma = 0.5 |
KNN | 0.860 | weights = distance, n neighbors = 1 |
ANN | 0.899 | alpha = 0.001, activation = tanh, hidden layer sizes = (20,1) |
Random Forest | 0.878 | n estimators = 100, max depth = 30, max features = 16 |
锆石类型 | 精确率 | 召回率 | F1分数 | 数量 |
---|---|---|---|---|
热液锆石 | 0.855 | 0.855 | 0.855 | 76 |
岩浆锆石 | 0.857 | 0.868 | 0.863 | 76 |
变质锆石 | 0.893 | 0.882 | 0.887 | 76 |
宏平均(macro) | 0.868 | 228 |
Table 5 Accuracy, recall, and F1 score of the test set in the SVM
锆石类型 | 精确率 | 召回率 | F1分数 | 数量 |
---|---|---|---|---|
热液锆石 | 0.855 | 0.855 | 0.855 | 76 |
岩浆锆石 | 0.857 | 0.868 | 0.863 | 76 |
变质锆石 | 0.893 | 0.882 | 0.887 | 76 |
宏平均(macro) | 0.868 | 228 |
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