我国首次发现的砷钙锌石和羟砷锌石的矿物学特征及其意义
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Austinite and Adamite Discovered for the First Time in China and Their Significanc
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    摘要:

    我国首次发现的砷钙锌石和羟砷锌石产于内蒙古自治区额济纳旗老硐沟金矿脉 氧化带矿石的空洞中。砷钙锌石多呈半自形或自形晶体,绿或淡绿色,透明,比重4.32(计算)。 Ng=1.778,Nm=1.760,Np=1.756,二轴晶(+),2V=46°。化学分子式为Ca0.99(Zn0.94 Cu0.07)1.01[(AsO4)0.97(CO3)0.03]1.00(OH),其中(CO3)2-取代部分(AsO4)3-为红外光谱分析所 证实,这不同于国外报道的砷钙锌石。据X射线粉末衍射分析的主要谱线,计算得其晶胞参数: a=0.7473nm,b=0.9017nm,c=0.5916nm。羟砷锌石常呈集合体或单个晶体产出,淡黄绿色 或无色,透明,比重4.44(计算)。Ng=1.761,Nm=1.738,Np=1.719,二轴晶(+),2V=87°。 化学分子式为(Zn1.97Ca0.02)1.99(AsO4)(OH)。据X射线粉末衍射分析的主要谱线,计算得其晶 胞参数:a=0.8304nm,b=0.8516nm,c=0.6054nm。

    Abstract:

    Austinite and adamite are secondary arsenate minerals, which were discovered for the first time in ore caves of the No.98 gold vein oxidized zone within the Laodonggou gold deposit, In ner Mongolia.Austinitemostlyoccursassubhedraloreuhedraltransparentcrystals1 . 0×0 . 8 —4.0×3.0 mm in size, with the color being green or greenish; its calculated specific gravity is 4.32. Adamite occurs commonly as transparent aggregates or crystal 1.8×1.5—3.5×2.5mm in size, with the color being light yellow-green or colculess; its caloulated specific gravity is 4.44. Studies under microscope give the following optidal characteristics:Ng=1.778,Nm=1.760,Np=1.756, positive optical character of biaxial crystal, with optic angle of 46°for austinite, and Ng=1.761,Nm=1.738,Np=1.719, positive optical character of biaxial crystal, with optic angle of 87°for adamite. Chemical analysis (wt %) shows that the composition of austinite is CaO 21.57, ZnO 29.61, CuO 2.29, MnO 0.002, Fe2O30.02, As2O5 43.07, CO20.43 and H2O+3.68, making up a chemical formula of Ca0.99(Zn0.94Cu0.07)1.01 [(AsO4)0.97(CO3)0.03]1.00(OH), and that the composition of adamite is ZnO 56.18, CuO 0.46, PbO 0.13, Fe2O30.004, As2O539.89 and H2O+3.31,making up a chemical formula of (Zn1.97Cu0.02)1.99(AsO4)(OH). As is detected by infrared spectral analysis, austinite contains minor CO2, and this is different from the feature of austimite reported by D. Radciffe et al. (1971). According to X-ray diffraction analysis, the unit cell parameters are a=0.7473nm,b=0.9017nm,c=0.5916nm for austinite and a=8304nm,b=0.8516nm,c=0.6054nm for adamite, respectively. The main ore mineral assemblage of the vein oxidized zone is scorodite+limonite+austinite+adamite+native gold+native silver+quartz+calcite+opal. The result of the study shows that adamite and austinite may be crystallized from acid to neutral solution under oxidation condition; nevertheless, the former is crystallized only when the solution has relatively high zinc ion activity. As these two arsenate minerals are of indication significance, their discovery contributes to the prospecting for secondary leaching type gold deposits.

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黄典豪,王宝林,吴澄宇,等, 1996. 我国首次发现的砷钙锌石和羟砷锌石的矿物学特征及其意义[J]. 岩石矿物学杂志, 15(3):259~268.
, 1996. Austinite and Adamite Discovered for the First Time in China and Their Significanc[J]. Acta Petrologica et Mineralogica, 15(3): 259~268.

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