LUO Heng, Shen Andy Hsitien, PAN Shaokui, ZHONG Yuan, LI Feng, Pia Tonna. Formation Mechanism of Peridot from Yiqisong, Jilin Province and the Application of Machine Learning to Its Origin Determination[J]. Journal of Gems & Gemmology, 2024, 26(S1): 91-93.
Citation: LUO Heng, Shen Andy Hsitien, PAN Shaokui, ZHONG Yuan, LI Feng, Pia Tonna. Formation Mechanism of Peridot from Yiqisong, Jilin Province and the Application of Machine Learning to Its Origin Determination[J]. Journal of Gems & Gemmology, 2024, 26(S1): 91-93.

Formation Mechanism of Peridot from Yiqisong, Jilin Province and the Application of Machine Learning to Its Origin Determination

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  • Received Date: July 14, 2024
  • To gain further insight into the formation environment and genesis mechanism of the peridot deposit from Yiqisong nanshan, Dunhua city, Jilin Province, China and distinguish the peridot deposit from the other origins, in this paper, a series of petrographic and geochemical analyses of peridot and its basalt were conducted using laser Raman spectroscopy, scanning electron microscopy, and laser ablation inductively coupled plasma mass spectrometer.Additionally, the accuracy of various machine learning models of peridot from differernt origins determination was also evaluated. The results suggest that the basalts in the area are predominantly spinel lherzolite.The formation temperature of the peridot was estimated to be about 903-1 055 ℃ through Ca, Al, and Cr in olivine thermometers.The peridot from this area mainly includes mantle olivine (high Ni group) and porphyritic olivine (low Ni group). The large-grained mantle olivine was captured by basaltic magma, which was fragmented during the ascent of the basaltic magma. In this process, basaltic magma underwent crystal differentiation, diopside, enstatite and porphyritic olivine precipitated. Only the large-grained mantle olivine fragments that survived the magmatic transport have the potential to be the gemstone. Geochemical data imply that the parent magma likely originated from partial melting of the asthenospheric mantle and may be a product of early Archean mantle magmatism.Based on the chemical compositions of peridot, we can use the methods of linear discriminant and machine learning to distinguish the gem-quality peridot from different origins effectively. However, when non-gem-grade olivine is present in the sample, lower quality peridot (where the main influencing factor is the colour) may interfere with the accuracy of the models. Thus, comprehensive peridot samples being various qualities from the same locality are essential to improve the the accuracy of the models.

  • Table  1.  Results of the temperature estimates (temperature is estimated by Al, Cr, Ca in olivine thermometer)
    Thermometer Type Average Temperature /℃
    TAl in ol 926
    TCr in ol 946
    TCa in ol 995
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    Table  2.  Accuracy statistics of identification of olivine origin using linear discrimination and machine learning model based on olive petrochemical compositions
    Model Accuracy/%
    Sample quantity:296 Sample quantity:313
    B-LDA 83.4 84.3
    Extra tree 93.3 93.6
    Random Forest 86.5 88.3
    Xgboost 92.1 88.3
    Logistic Regression 79.8 85.0
    lightgbm 95.5 83.0
    catboost 89.9 92.6
    Naive Bayes 80.9 80.9
    注:产地判别选取Mn,Zn,Na,Al,Sc,V,Cr,P,Ti及REE十种元素,不同模型的准确率基本都高于80%;第一次使用296颗宝石级橄榄石样品进行判别,第二次加入17颗非宝石级橄榄石进行判别,两次判别不同模型的准确率均有所变化,表明样品数量和橄榄石品质对模型准确率有不同程度的影响
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    Figure  1.  Photographs of the olivine basalt samples and test results: (a) peridot crystals and basalt samples; (b) BSE images of olivine basalt showing the presence of olivine, diopside, enstatite, hematite-ilmenite, hornblende, apatite, etc. Olivine and diopside exhibit idiomorphic to hypautomorphic. Hematite-ilmenite typically forms regular hexagons. Hornblende is predominantly observed as short columnar shapes, arranged parallel or nearly perpendicular. Apatite forms near-hexagonal prisms arranged in clusters adjacent to olivine and pyroxene; (c) Raman spectra of the main minerals in the olive basalts; (d) spider diagrams of trace elements (normalized by primitive mantle) in basaltic matrix. The trace elements show a right-dipping distribution, with obvious differences between light and heavy rare earths.Di: Diopside; En: Enstatite; Hem-Ilm: Hematite-Ilmenite; Pl: Plagioclase; Ol: Olivine; Ap: Apatite; Hb: Hornblende
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