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Abstract

Aspects in Mining & Mineral Science

Role of Fluids in Origin PGE Mineralization’s in the Pansky Tundra Layered Intrusion, Kola Peninsula, NW Russia

  • Open or CloseTurchenko SI*

    Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, Russia

    *Corresponding author: Turchenko SI, Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, Russian Federation, Russia

Submission: August 22, 2019; Published: October 15, 2019

DOI: 10.31031/AMMS.2019.03.000574

ISSN : 2578-0255
Volume3 Issue5

Abstract

The Pansky Tundra layered intrusion belongs to a group of the Paleo Proterozoic layered intrusions (2.45-2.50Ga) located in the north-eastern Fennoscandian Shield, Kola Peninsula (Russia). The intrusions were emplaced during just that epoch of intracontinental rifting. This intrusion consists of norite-gabbronorite-gabbroic megacycles and contain rhythmically layered horizon (up to 200-300m thick).

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