孙瑞祯, 郑亚龙, 王成博, 彭子诚. 金黄色透辉石的宝石学特征及颜色成因初探[J]. 宝石和宝石学杂志(中英文), 2023, 25(3): 36-42. DOI: 10.15964/j.cnki.027jgg.2023.03.005
引用本文: 孙瑞祯, 郑亚龙, 王成博, 彭子诚. 金黄色透辉石的宝石学特征及颜色成因初探[J]. 宝石和宝石学杂志(中英文), 2023, 25(3): 36-42. DOI: 10.15964/j.cnki.027jgg.2023.03.005
SUN Ruizhen, ZHENG Yalong, WANG Chengbo, PENG Zicheng. Gemmological Characteristic and Colour Genesis of Golden Diopside[J]. Journal of Gems & Gemmology, 2023, 25(3): 36-42. DOI: 10.15964/j.cnki.027jgg.2023.03.005
Citation: SUN Ruizhen, ZHENG Yalong, WANG Chengbo, PENG Zicheng. Gemmological Characteristic and Colour Genesis of Golden Diopside[J]. Journal of Gems & Gemmology, 2023, 25(3): 36-42. DOI: 10.15964/j.cnki.027jgg.2023.03.005

金黄色透辉石的宝石学特征及颜色成因初探

Gemmological Characteristic and Colour Genesis of Golden Diopside

  • 摘要: 采用常规宝石学测试、傅里叶变换红外光谱仪、拉曼光谱仪、能量型色散X射线荧光能谱仪(EDXRF)、激光剥蚀电感耦合等离子体质谱(LA-ICP-MS)和紫外-可见光谱仪等测试分析,对市场上少见的一种金黄色透辉石的宝石学特征和谱学特征进行了深入分析,探讨了其颜色成因。结果表明,该样品的矿物组成为透辉石,其中含有包括Fe在内的多种微量元素;样品中Fe的存在形式主要为Fe3+;Fe3+在450 nm处的T位Fe3+-O电荷转移和M1位Fe3+的d-d跃迁是金黄色透辉石致色的重要原因。

     

    Abstract: In order to analyze the gemmological characteristics, spectroscopic characteristics and the possible colour genesis of the golden diopside, some samples were tested by conventional gemmological tests, Raman spectrometer, Fourier infrared spectrometer(FTIR), UV-Vis spectrometer, energy dispersive X-ray fluorescence spectrometer (EDXRF) and LA-ICP-MS. The results showed that the main mineral of the samples is diopside, and they contain a variety of trace elements including Fe. The Fe element in the sapmples mainly exists in the form of Fe3+. And the Fe3+-O charge transfer at 450 nm, T position and the Fe3+ d-d transition at M1 position are the important cause of the colour of golden diopside.

     

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