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首页> 外文期刊>Записки Российского минералогического общества >HYDROXYLELLESTADITE FROM THE GARNET-WOLLASTONITE SKARNS OF ARIMAO-NORTE (CUBA)
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HYDROXYLELLESTADITE FROM THE GARNET-WOLLASTONITE SKARNS OF ARIMAO-NORTE (CUBA)

机译:来自北阿里芒(古巴)的石榴石-硅灰石薄膜中的羟基闪石

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Ellestadite- the rare mineral of apatite group- has been found out for the first time at Cuba, in Arimao-Norte skarn deposit. Ellestadite associates there with wollastonite, garnet of grossular-andradite composition, diopside, vesuvian, calcite, xonotlite, pyrite, etc. It forms small segregations and widespread in disseminated grain. Several its large localitites have been revealed by the drill hole PBW-19, where some intervals of the corp, up to several metres in length, were represented by the ellestaditic rock containing 97-99 percent of this mineral, with minor admixtures of garnet, pyrite, magnetite and stilpnomelane. Density 3.020 g/cm~3, microhardness 390 kg/mm~2 (4.5 on Mohs), indices of refraction No=1.651+0.002, Ne=0.647+0.002. The paper displays data on thermographic and IR spectroscopy peculiarities of the mineral, their interpretation is given also. Chemical composition of ellestadite corresponds to the formula: (Ca_(9.99)Na_(0.001))_(10)((SiO_4)_(2.955)(CO_3)_(0.088)(PO_4)_(0.003))_6 X ((OH)_(1.19)O_(0.49)Cl_(0.31)F_(0.03)_(2.02). Obtained data confirm the typical feature of ellestadite-the Si:S ratio in tetrahedral positions is quite close to 1:1. Unit cell parameters: a=9.526, b=9.506, c=6.922 A, #gamma#=119.99 deg, V=542.89 A~3.
机译:埃利斯塔德-磷灰石族的稀有矿物-在Arimao-Norte矽卡岩矿床首次在古巴被发现。那里的硅藻土与硅灰石,组成刚玉的石榴石,透辉石,维苏威,方解石,硬硅钙石,黄铁矿等结合。它形成小的偏析并广泛散布在谷物中。 PBW-19钻孔揭示了它的几个局部位置,其中该公司的某些间隔(长达几米)以含97-99%这种矿物的石榴石岩石和少量石榴石混合而成,黄铁矿,磁铁矿和stilpnomelane。密度3.020 g / cm〜3,显微硬度390 kg / mm〜2(在Mohs上为4.5),折射率No = 1.651 + 0.002,Ne = 0.647 + 0.002。本文显示了矿物的热成像和红外光谱数据,并给出了解释。凹凸棒石的化学成分对应于下式:(Ca_(9.99)Na_(0.001))_(10)((SiO_4)_(2.955)(CO_3)_(0.088)(PO_4)_(0.003))_ 6 X(( OH)_(1.19)O_(0.49)Cl_(0.31)F_(0.03)_(2.02)。所得数据证实了钙钛矿的典型特征-四面体位置的Si:S比非常接近1:1。参数:a = 9.526,b = 9.506,c = 6.922A,#gamma#= 119.99度,V = 542.89A〜3。

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