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Linarite and connellite dataset from Calabria region (Southern Italy): First evidence

机译:来自卡拉布里亚地区(意大利南部)的扁长石和堇青石数据集:初步证据

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摘要

This dataset article contains mineralogical and chemical data of linarite and connellite sulfate minerals. These minerals were found included in the oxidized zones of cupriferous sulfide ores in the Fiumarella Mine, in Calabria region (Southern Italy). Linarite is a basic sulfate of copper and lead with the formula of PbCuSO4(OH)2 while connellite is a hydrated sulfate of copper with an ideal formula of Cu36Cl6(SO4)2(OH)62∙12H2O.Recently, in the mine of Fiumarella, in addition to primary minerals such as barite, galena, cerussite, anglesite, fluorite and chalcopyrite, wulfenite (PbMoO4) was also detected. Linarite consists of a prismatic bright blue crystal with a vitreous luster of micrometric size implanted upon on a matrix made up of barite. Connellite includes micrometric acicular tuft crystals protruding from matrix. Methods for obtaining the datasets include optical microscopy, micro X-ray Fluorescence and micro-Raman spectroscopy.
机译:该数据集文章包含褐铁矿和硫酸钙质石矿物的矿物学和化学数据。这些矿物被发现包括在卡拉布里亚地区(意大利南部)的菲乌梅雷拉矿的硫化铜矿矿石的氧化区中。菱铁矿是铜和铅的碱性硫酸盐,分子式为PbCuSO4(OH)2,而堇青石是铜的水合硫酸盐,理想分子式为Cu36Cl6(SO4)2(OH)62∙12H2O。除重晶石,方铅矿,方铅矿,角铁矿,萤石和黄铜矿等主要矿物外,还检测到了辉石​​(PbMoO4)。莱纳石(Linarite)由明亮的蓝色棱柱晶体组成,其上植入了由重晶石构成的基质,具有微米级的玻璃光泽。 Connellite包括从基质突出的微米级针状簇状晶体。获取数据集的方法包括光学显微镜,显微X射线荧光和显微拉曼光谱。

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