南极洲利文斯顿岛Caleta Argentina石英多金属矿脉的矿石矿物学和矿物化学

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY

Spisanie Na B Lgarskoto Geologichesko Druzhestov-Review of the Bulgarian Geological Society Pub Date : 2022-12-01 DOI:10.52215/rev.bgs.2022.83.3.191

Ralica Sabeva

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引用次数: 0

摘要

南极利文斯顿岛阿根廷卡莱塔石英多金属矿脉由黄铁矿、黄铜矿、方铅矿和闪锌矿组成。黄铜矿是最常见的矿石矿物，银的浓度(平均240.51 ppm)。闪锌矿含有银(平均50.82)和金(平均0.31 ppm)，黄铁矿-金从无法检测到1.03 ppm(平均0.59 ppm)和银从无法检测到54.33 ppm(平均32.52 ppm)。Caleta Argentina作为赫德半岛的一个矿点，必须与其他研究区域如保加利亚南极基地、保加利亚海滩和Sally Rocks进行关联。

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Ore mineralogy and mineral chemistry of quartz-polymetallic veins in Caleta Argentina, Livingston Island, Antarctica

The quartz-polymetallic veins from Caleta Argentina, Livingston Island, Antarctica consist of pyrite, chalcopyrite, galena, and sphalerite. Chalcopyrite is the most common ore mineral and with concentrations of Ag (average 240.51 ppm). Sphalerite contains Ag (average 50.82) and Au (average 0.31 ppm), and pyrite – Au from not detectable to 1.03 ppm (average 0.59 ppm) and Ag from not detectable to 54.33 ppm (average 32.52 ppm). Caleta Argentina, as one of the ore occurrences in Hurd Peninsula, has to be correlated with the other research area such as the Bulgarian Antarctic Base, the Bulgarian Beach, and Sally Rocks.

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Spisanie Na B Lgarskoto Geologichesko Druzhestov-Review of the Bulgarian Geological Society GEOSCIENCES, MULTIDISCIPLINARY-

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