Copper-sulphide mineralization in alkaline rocks from the Salmagorskii ring complex, Kola peninsula, Russia

被引：0
|
作者：
Korobeinikov, AN [1 ]
Mitrofanov, FP [1 ]
Gehor, S [1 ]
Laajoki, K [1 ]
Mamontov, VP [1 ]
Pavlov, VP [1 ]
机构：
[1] Kola Sci Ctr, Inst Geol, Apatity, Russia
来源：
MINERAL DEPOSITS: RESEARCH AND EXPLORATION, WHERE DO THEY MEET? | 1997年
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中图分类号：
TD [矿业工程];
学科分类号：
0819 ;
摘要：
New data on the geological structure and mineralizations of the Salmagorskii ring complex have been obtained by the drilling program carried out in recent 5 years. The concentric zoning of the pluton from its periphery towards the centre is: dunite-clinopyroxenite-melilitolite-urtite-ijolite-melteigite. The copper-sulphide mineralization containing chalcopyrite, minor djerfisherite and cubanite is hosted by ijolite and melteigite. The mineralization is a product of processes of the postmagmatic remobilization of copper under the influence of a residual alkaline fluid rich in H2O, CO2, Cl, sulphur, and phosphorus.
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页码：453 / 456
页数：4
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