Geochemistry of volatiles in PGE ore of the Western Pana layered pluton in the Kola Peninsula

被引：1
|
作者：
Nivin, V. A. [1 ]
Kul'chitskaya, A. A. [2 ]
Rundqvist, T. V. [1 ]
机构：
[1] Russian Acad Sci, Inst Geol, Kola Sci Ctr, Apatity 184200, Murmansk Oblast, Russia
[2] Natl Acad Sci Ukraine, Inst Geochem Mineral & Ore Format, UA-03142 Kiev, Ukraine
来源：
GEOLOGY OF ORE DEPOSITS | 2009年 / 51卷 / 04期
基金：
俄罗斯基础研究基金会;
关键词：
HORIZON; MASSIF;
D O I：
10.1134/S1075701509040060
中图分类号：
P5 [地质学];
学科分类号：
0709 ; 081803 ;
摘要：
The distribution of volatiles in ore units of the Western Pana layered mafic pluton in the Kola province was studied with pyrolytic gas chromatography. In comparison with barren rocks, the rocks containing Pt-Pd mineralization are characterized by a much higher concentration of volatiles, especially H(2)S, SO(3), and CH(4). With a drop in temperature, the redox potential of the fluid phase in the ore-magmatic system increased. PGE mineralization was largely formed at the postcumulus stage with participation of volatiles under variable redox conditions.
引用
收藏
页码：330 / 337
页数：8
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