宝石和宝石学杂志(中英文)2024,Vol.26Issue(6) :15-24.DOI:10.15964/j.cnki.027jgg.2024.06.002

马达加斯加硅硼镁铝石的宝石学及谱学特征

Gemmological and Spectroscopic Characteristics of Grandidierite from Madagascar

柏玉林 刘衔宇 涂彩 龚雪 陈全莉
宝石和宝石学杂志(中英文)2024,Vol.26Issue(6) :15-24.DOI:10.15964/j.cnki.027jgg.2024.06.002

马达加斯加硅硼镁铝石的宝石学及谱学特征

Gemmological and Spectroscopic Characteristics of Grandidierite from Madagascar

柏玉林 1刘衔宇 2涂彩 3龚雪 1陈全莉4
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作者信息

  • 1. 桂林理工大学地球科学学院,广西桂林 541006
  • 2. 桂林理工大学地球科学学院,广西桂林 541006;上海建桥学院珠宝学院,上海 201306
  • 3. 上海建桥学院珠宝学院,上海 201306
  • 4. 中国地质大学(武汉)珠宝学院,湖北武汉 430074
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摘要

硅硼镁铝石是一种极其罕见的铝硼硅酸盐,产地和产量的有限性使其谱学表征及颜色形成机理研究较少.本文采用常规宝石学测试方法以及电子探针、紫外-可见光光谱、傅里叶变换红外光谱、激光拉曼光谱等测试技术,对马达加斯加宝石级硅硼镁铝石样品的宝石学特征、化学成分及谱学特征进行了系统研究.化学成分分析表明,马达加斯加硅硼镁铝石样品中除主量元素Al、Si、Mg、Fe外,还含有Ca、Mn、Cr、Ti和Zn等微量元素,浅色与深色样品FeOT平均含量分别为0.63%、1.29%,X(X=wFe/w(Fe+Mg))分别为0.024、0.049,X值越大,颜色饱和度越高,多色性色调逐渐加深,多色性强度增大,折射率值与X呈正相关关系.硅硼镁铝石样品的紫外-可光光谱在387、443 nm处特征吸收峰分别为八面体晶体场中Fe3+离子的d-d跃迁6A1→T2(4D)和自旋禁阻跃迁6A1→(4A1g,4Eg)引起,ⅤFe2+离子在三角双锥结构中的晶体场类似于畸变的八面体配位场,因此458 nm处吸收峰与ⅤFe2+"五态"(6 D)和"三态"(3 H)分裂项的自旋禁阻跃迁5T2g→3T2g有关,477 nm处吸收峰与ⅤFe2+离子d-d跃迁有关,515 nm处吸收峰为八面体晶体场Ⅵ Fe2+的自旋禁阻跃迁引起,746、771、797 nm和823 nm处吸收峰可能与Fe3+和ⅤFe2+离子之间的Fe2+/Fe3+IVCT有关.红外光谱测试结果显示,400~500 cm-1和630~800 cm-1红外吸收峰分别为[AlO5]+[AlO6]的v4和v3振动;530~630 cm-1范围内的吸收为[SiO4]的v4振动;800~1 100 cm-1范围内为硅氧骨干Si-O-Si不对称伸缩振动和硼氧吸收引起;1 300~1 500 cm-1范围内的吸收带属于[BO3]的 振动;3 400~4 200 cm-1范围内的吸收率与OH的伸缩振动有关.拉曼光谱中1 300~1 500 cm-1拉曼位移为[BO3]的 v3反对称伸缩振动.

Abstract

Grandidierite is an extremely rare aluminum borosilicate.Due to the limitation of produ-cing area and yield,there are few studies on its spectral characterization and colour formation mech-anism.In this paper,the gemmological characteristics,chemical compositions and spectral charac-teristics of gem-quality grandidierites from Madagascar have been studied in detail using convention-al gemmological testing methods,electron microprobe,UV-Vis spectrometer,Fourier transform in-frared spectrometer and laser Raman spectrometer.Chemical composition analysis showed that the samples contains trace elements such as Ca,Mn,Cr,Ti and Zn in addition to the main elements Al,Si,Mg and Fe,and the average content of FeOT of light and dark samples is 0.63%and 1.29%,respectively,X(X=wFe/w(Fe+Mg))is 0.024 and 0.049,respectively.With the higher value of the X-ratio,the higher the saturation of the colour,and the intensity of the polychromatici-ty and the polychromatic hue gradually deepened,the refractive index value is positively correlated with X.The characteristic absorption peaks in the UV-Vis spectra of grandidierite at 387 nm and 443 nm are due to the d-d leap 6A1→T2(4D)and the spin-barrier leap 6A1→(4A1g,4Eg)of the Fe3+ion in the octahedral crystal field,respectively,ⅤFe2+in the triangular bipyramidal structure resembles the distorted octahedral coordination field,so 458 nm is associated with the spin-barrier leap 5 T2g→3 T2g for the ⅤFe2+"five-state"(6D)and"three-state"(3H)splitting terms,and 477 nm is associated with the d—d leap of ⅤFe2+ions,515 nm is caused by the spin-barrier leap of ⅥFe2+in the octahedral crystal field,746,771,797 nm and 823 nm absorption peaks may be associated with the Fe2+/Fe3+IVCT between Fe3+and ⅤFe2+ions.The infrared spectra test results show that the infrared absorption peaks at 400-500 cm-1and 630-800 cm-1 are the v4 and v3 vibrations of[AlO5]+[AlO6],respectively;the absorption at 530-630 cm-1 belongs to the v4 vibration of[SiO4];the absorption at 800-1 100 cm-1 is due to the asymmetric stretching vibration of the silica-oxygen backbone Si-O-Si and the absorption of boron oxygen;the absorption bands of 1 300-1 500 cm-1belong to the v3 vibration of[BO3];3 400-4 200 cm-1is related to lat-tice vibration of OH.Raman spectra 1 300-1 500 cm-1 Raman shift is the v3 antisymmetric stretching vibration of[BO3].

关键词

硅硼镁铝石/颜色成因/紫外-可见光光谱/红外光谱/拉曼光谱

Key words

grandidierite/colour origin/UV-Vis spectrum/infrared spectrum/Raman spectrum

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出版年

2024
宝石和宝石学杂志(中英文)
中国地质大学(武汉)

宝石和宝石学杂志(中英文)

影响因子:0.4
ISSN:2096-9120
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