钙钒榴石的新变种—铬钙钒榴石的研究
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Chroiman Goldmanite— A Newly Discovered Variety of Garnet Group
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    摘要:

    铬钙钒榴石发现于江苏省句容县铜山铜钼矿外接触带的大理岩中。该矿物属等轴晶系,空间群为Oh(10)-Ia3d。晶胞参数a0=11.9470A,Z=8;化学成分siO2=34.99%,Al2O3=7.61%,CaO=32.95%,V2O5=13.41%,Cr2O3=10.13%,其化学式为:(Ca(2.938)Na(0.003)(2.941)(V(0.737)Cr(0.666)Fe(0.006)Al(0.531)(2.00)(Si(2.938)Al(0.156)(3.094)O(12)。折光率n=1.799(±0.0015)。计算比重为3.72。VHN(100)=1168.7kg/mm2,摩氏硬度7.1。它是一种既有钒,又有铬的同生沉积和岩浆侵入接触交代变质矿物。它的发现为石榴石族增添了新成员,并为铬钙钒榴石成因提供了新的产状资料,同时对铬钒元素的地球化学研究也具有重要意义。

    Abstract:

    Chromian goldmarite is discovered in marble along exocontact zone of the Tongshan copper-molybdenum deposit, Jurorg county, Jiangsu province, It is of isometric system, with space group Oh(10)-Ia3d, unit cell parameters ao=11.9470A Z=8; is chemical composition is Si02=34.99%,A1203=7.61%,Ca0=32.95%, V205=13.41%,Cr2Og=10.13%,giving a chemical composition of(Ca2.938Na0.003)2.941 (Cr0.666V0.737Fe0.006Al0.591)2.00(Si2.938A10.156)3.094O12 Refractive index n=1.799 (士0.0015).Calculated specific gravity3.75, VHN100=1168.7kg/mm2, Moss hard- ness 7.1.It is a mineral formed as a result of syngenetic deposition and intrusive contact metamorphism and contining vanadium, chromium and aluminium. The discovery of this mineral has added a new member to the garnet group and also provided new data of occurrence for chromian-varadic minerals In addition, it is of great sigrificance to the study of chromium-vanadium geochemistry.

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张慧敏,吴乾荣,卜永红, 1989. 钙钒榴石的新变种—铬钙钒榴石的研究[J]. 岩石矿物学杂志, 8(3):260~265.
Zhang Huimin, Wu Qianrong, 1989. Chroiman Goldmanite— A Newly Discovered Variety of Garnet Group[J]. Acta Petrologica et Mineralogica, 8(3): 260~265.

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