岩石矿物学杂志2024,Vol.43Issue(3) :673-684.DOI:10.20086/j.cnki.yskw.2024.0315

福建云霄石榴子石宝石矿物学特征

Gem mineralogy characteristics of Yunxiao garnet,Fujian,China

陈星韵 张良 王豪帅 张瑞锐 孙思辰
岩石矿物学杂志2024,Vol.43Issue(3) :673-684.DOI:10.20086/j.cnki.yskw.2024.0315

福建云霄石榴子石宝石矿物学特征

Gem mineralogy characteristics of Yunxiao garnet,Fujian,China

陈星韵 1张良 2王豪帅 3张瑞锐 3孙思辰4
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作者信息

  • 1. 中国地质大学(北京)珠宝学院,北京 100083
  • 2. 中国地质大学(北京)珠宝学院,北京 100083;中国地质大学(北京)地质过程与矿产资源国家重点实验室,北京 100083
  • 3. 中国地质大学(北京)地球科学与资源学院,北京 100083
  • 4. 福建省地质矿产勘查开发局,福建福州 350003
  • 折叠

摘要

福建云霄是我国重要的宝石级石榴子石产地,然而该区石榴子石的致色机理不清,制约了对其形成机制的理解及后续开发利用.本文选取7件福建云霄橙黄-橙红色石榴子石样品,利用傅立叶红外光谱、紫外-可见光光谱和拉曼光谱分析其谱学特征,使用电子探针及激光剥蚀电感耦合等离子体质谱仪(LA-ICP-MS)分析限定其主量、微量元素组成.结果表明云霄石榴子石主要为锰铝榴石,其颜色主要与二价锰(Mn2+)和铁离子(Fe2+)对可见光的吸收有关,Mn2+导致其主体呈橙色,少量Fe2+控制其橙红色调,微量Ti4+使其呈褐色调.福建云霄石榴子石样品核部锰含量相对较低而铁、镁含量较高,锰元素含量由核部向边部逐渐升高,且具有重稀土元素富集、轻稀土元素亏损的左倾配分模式和Eu负异常,表明其形成于岩浆结晶作用晚期.

Abstract

Yunxiao is a significant producing area of gem-quality garnet in China.However,the color origin of gar-net in this area remains ambiguous,which restricts the understanding of their formation mechanism and subsequent exploitation.In this paper,7 samples of orange-yellow-orange-red garnet from Yunxiao,Fujian were selected,and the spectral characteristics of the samples were analyzed by Fourier infrared spectrum,UV-visible spectrum and Ra-man spectrum,and the characteristics of main and trace elements were defined by electron probe(EPMA)and la-ser ablation inductively coupled plasma mass spectrometry(LA-ICP-MS)analysis.It is concluded that the color of the garnet is predominantly influenced by the absorption of visible light by Mn2+and Fe2+.Mn2+dictates the yellow tone of the garnet,while a minor amount of Fe2+governs the orange-red tone.Additionally,a trace amount of Ti4+imparts a brownish appearance to the garnet.The samples exhibited a relatively low manganese content and high iron and magnesium content in their core,a gradual increase in manganese content from the core to the rim.The samples also displayed a left-leaning partition pattern,with an enrichment of heavy rare earth elements and a deficit of light rare earth elements.Europium(Eu)showed a negative anomaly.These findings suggest that the garnets from Yunxiao,Fujian were formed during magmatic processes and are products of late-stage magmatic crystallization.

关键词

石榴子石/宝石学特征/矿物光谱/致色机理/福建云霄

Key words

garnet/gemological characteristics/mineral spectroscopy/color mechanism/Yunxiao,Fujian Prov-ince

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基金项目

国家重点研发计划(2019YFA0708603)

高等学校学科创新引智计划(111计划)(BP0719021)

出版年

2024
岩石矿物学杂志
中国地质学会岩石学专业委员会 矿物学专业委员会 中国地质科学院地质所

岩石矿物学杂志

CSTPCDCSCD北大核心
影响因子:1.104
ISSN:1000-6524
参考文献量64
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