东非铬钒钙铝榴石(察沃石)宝石的矿物学和地球化学研究现状

吕林素, 毛冰, 何雪梅

吕林素, 毛冰, 何雪梅. 东非铬钒钙铝榴石(察沃石)宝石的矿物学和地球化学研究现状[J]. 宝石和宝石学杂志, 2014, 16(4): 1-13.
引用本文: 吕林素, 毛冰, 何雪梅. 东非铬钒钙铝榴石(察沃石)宝石的矿物学和地球化学研究现状[J]. 宝石和宝石学杂志, 2014, 16(4): 1-13.
LYU Linsu, MAO Bing, HE Xuemei. Mineralogy and Geochemistry of Gem Vanadian-chromian Grossulars(Tsavorites)from East Africa[J]. Journal of Gems & Gemmology, 2014, 16(4): 1-13.
Citation: LYU Linsu, MAO Bing, HE Xuemei. Mineralogy and Geochemistry of Gem Vanadian-chromian Grossulars(Tsavorites)from East Africa[J]. Journal of Gems & Gemmology, 2014, 16(4): 1-13.

东非铬钒钙铝榴石(察沃石)宝石的矿物学和地球化学研究现状

基金项目: 

地质遗迹标本采集与购置项目(1211311381001)和地质矿产调查评价项目(1212011220038)成果

详细信息
    作者简介:

    吕林素(1965-),女,博士,研究员,主要从事矿物(含宝石)、岩石和矿床研究工作

  • 中图分类号: TS93

Mineralogy and Geochemistry of Gem Vanadian-chromian Grossulars(Tsavorites)from East Africa

  • 摘要: 东非(包括肯尼亚、坦桑尼亚和马达加斯加)铬钒钙铝榴石(察沃石)均赋存于新元古代莫桑比克变质带的钙质硅酸盐石墨片麻岩中。矿物学研究表明,东非察沃石为宝石级钒(±铬)钙铝榴石,以w(V2O3)≈0.20%或w(Cr2O3)≈0.30%为分界线可划分为钒钙铝榴石、铬钙铝榴石和铬钒钙铝榴石3类,其中以钒钙铝榴石为主。东非察沃石的晶体化学式为(Ca2.792~3.005Fe0~0.013Mn0.008~0.080Mg0.022~0.0782.948~3.110(Al1.787~1.968 Ti0.005~0.028 Cr0.001~0.072 Fe0~0.080V0.005~0.163)1.890~2.052 [Al0~0.288 Si2.712~3.017] O12,可简写成Ca3(Al,Cr,Fe,V)2[Si04]3;其端员组分为Grs87.61~96.79 Gld0.16~5.66Uvr0.02~2.46 Pyr0.73~2.68 Sps0.28~2.75Adr0.00~2.71Alm0.00~0.43,表明它由钙铝榴石(87.61%~96.79%)、钙钒榴石(0.16%~5.66%)和钙铬榴石(0.02%~2.46%)组成。以往研究表明,东非不同国家所产的察沃石之间 V/Cr 质量分数比值存在明显差异,它们的化学成分是可变的,但同一矿床的 V/Cr 质量分数比值通常是不变的;并且它们还具有3 组一致的δ18O值,依次为9.5‰~11.0‰、11.6‰~14.8‰和15.5‰~21.1‰,利用O同位素与 V-Cr-Mn微量元素量相结合的方法,可鉴别其地质和地理来源。
    Abstract: The gem vanadian(chromian)grossulars from East Africa(e.g.Kenya,Tanzania and Madagascar),also known as Tsavorites,are usually hosted in calc-silicate graphitic gneiss of the Neoproterozoic Mozambique Metamorphic Belt.According to the divisions at w(V2O3)≈0.20%or w(Cr2O3)≈0.30%,the tsavorites from East African can be classified into three types,which are vanadian grossulars,chromium grossulars and vanadian-chromium grossulars.Mineralogical analysis shows that the tsavorite from East Africa is mainly aluminum calc-silicate in composition,with crystallochemical formula of(Ca2.792~3.005Fe0~0.013 Mn0.008~0.080Mg0.022~0.078)2.948~3.110 (Al1.787~1.968Ti0.005~0.028Cr0.001~0.072Fe0~0.080V0.005~0.163)1.890~2.052[Al0~0.288Si2.712~3.017O12],abbreviated as Ca3(Al,Cr,Fe,V)2[SiO4]3.The end-member components of the tsavorite from East Africa are Grs87.61~96.79Gld0.16~5.66Uvr0.02~2.46Pyr0.73~2.68 Sps0.28~2.75Adr0.00~2.71Alm0.00~0.43,suggesting a composition of grossular(87.61%to 96.79%)with a small amount of goldmanite(0.16%to 5.66%),and uvarovite(0.02%to 2.46%).Previous research suggested that there was an obvious difference in V/Cr ratio among the tsavorites from different countries in East Africa.Although the chemical composition of tsavorites is variable,V/Cr ratios remain constant for a given deposit.In addition,three consistent sets ofδ18 O values,from 9.5‰to 11.0‰,from 11.6‰to 14.5‰,and from 15.5‰to 21.1‰,have been recognized for the tsavorites from Tanzania,Kenya,and Madagascar,respectively.The geological and geographical sources of tsavorites can be identified by the combined research on oxygen isotope compositions and V-Cr-Mn quantification.
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  • 收稿日期:  2014-03-10

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