俄罗斯科拉半岛中部Fedorova-Pana层状侵入体Federova冻土带铂族元素矿床主要硫化物矿物中的痕量贵金属

L. Cabri, V. Subbotin
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摘要

在加拿大和俄罗斯的两个独立项目中,对俄罗斯科拉半岛中部Fedorova- pana层状侵入体早元古代Fedorova冻土带侵入体基底cu - ni -铂族元素矿化的岩心样品进行了研究。在加拿大,用激光烧蚀电感耦合质谱法对323个贱金属硫化物颗粒[镍黄铁矿(101)、磁黄铁矿(98)、黄铜矿(25)和黄铁矿(99)]进行了痕量贵金属分析,结果表明,钯在镍黄铁矿中含量很高。大多数分析(71%)分别使用了代表西坑和东坑矿化的两个主复合样品,即FWMC和FEMC。较少的分析来自西坑的其他三种粉碎的岩心样品被称为“岩性”样品:OLFW(含橄榄石岩石),ANFW(白岩质岩石)和GNFW(辉长花岗岩)。在俄罗斯,从西坑和东坑以及其他四个Fedorova Tundra侵入矿床(Kievey, Northern Kamennik, Eastern Chuarvy和Southern Kievey)的钻芯中切割出120个抛光切片进行了矿物学研究。铂族矿物表征和痕量钯电子探针微分析是利用所有六个地点(n = 95)的抛光切片进行的。西坑样品(n = 35)和东坑样品(n = 19)中钯的痕量电子探针微分析数据,虽然检测水平更高,但被认为与激光烧蚀电感耦合质谱数据相当。东丘瓦利样品显示出特别高的Pd浓度,平均为0.49 wt.% Pd (n = 11),最高可达1.64 wt.% Pd。这些研究的综合数据指导了我们的估计,即镍黄铁矿占这些矿石中Pd的30 - 50%,而硫化物中的Rh固溶体可能占总Rh的50 - 98%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Trace precious metals in major sulfide minerals from the Federova Tundra platinum group element deposit in the Fedorova-Pana layered intrusion, central Kola Peninsula, Russia
Drill-core samples from the basal Cu-Ni-platinum-group element mineralization of the Early Proterozoic Fedorova Tundra intrusion in the Fedorova-Pana layered intrusion, central Kola Peninsula, Russia, were studied in two separate projects in Canada and Russia. In Canada, trace precious metal analyses by laser ablation inductively coupled mass spectrometry of 323 base metal sulfide particles [pentlandite (101), pyrrhotite (98), chalcopyrite (25), and pyrite (99)] show that Pd is highly concentrated in pentlandite. Most of the analyses (71%) were done using two master composite samples of comminuted drill core representative of the West Pit and East Pit mineralization, FWMC and FEMC, respectively. Fewer analyses were made of three other comminuted drill core samples from the West Pit referred to as “lithology” samples: OLFW (olivine-bearing rocks), ANFW (leucocratic rocks), and GNFW (gabbronorite). In Russia, 120 polished sections sliced from drill core from the West and East Pits and from four other Fedorova Tundra intrusion deposits (Kievey, Northern Kamennik, Eastern Chuarvy, and Southern Kievey) were studied mineralogically. Platinum group mineral characterization and trace Pd electron probe microanalyses of pentlandite were done using polished sections from all six locations (n = 95). The trace electron probe microanalysis data for Pd in pentlandite from the West (n = 35) and East (n = 19) Pit samples, though at much higher detection levels, are considered to be comparable to the laser ablation inductively coupled mass spectrometry data. The Eastern Chuarvy samples show particularly high Pd concentrations averaging 0.49 wt.% Pd (n = 11) and as high as 1.64 wt.% Pd. The combined data from these studies guides our estimate that pentlandite accounts for 30 to 50% of the Pd in these ores and that Rh solid solution in sulfides may account for >98% of the total Rh.
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