Petrology of Gabbroides and Isotope Signature of Sulfide Mineralization from Fedorov-Pansky Layered Mafic Intrusion, Kola Peninsula, Russia-Reference-Cited by-同舟云学术

Petrology of Gabbroides and Isotope Signature of Sulfide Mineralization from Fedorov-Pansky Layered Mafic Intrusion, Kola Peninsula, Russia

Published:2009-01-01 Issue:-1 Volume:33 Page:19-22
ISSN:1897-1695
Container-title:GEOCHR
language:en
Short-container-title:Geochronometria

Author:

Huber Milosz¹,Halas Stanislaw²,Piestrzyński Adam³

Affiliation:

1. Department of Geology and Lithosphere Conservation, Institute of Earth Sciences, Maria Curie-Skłodowska University, Al. Kraśnicka 2CD, 20-718 Lublin, Poland

2. Mass Spectrometry Laboratory, Institute of Physics, Maria Curie-Skłodowska University, Plac Marii Curie-Skłodowskiej 1, 20-031 Lublin, Poland

3. Zakład Geologii Złożowej i Górniczej, Wydział Geologii, Geofizyki i Ochrony środowiska AGH, Al. Mickiewicza 30, 30-059 Kraków, Poland

Abstract

Petrology of Gabbroides and Isotope Signature of Sulfide Mineralization from Fedorov-Pansky Layered Mafic Intrusion, Kola Peninsula, Russia Samples from Fiodoro-Pansky massif were investigated by polarized light microscopy, EDS electron microscopy and isotope ratio mass spectrometry. We have observed four-stage ore mineralization: (1) magmatic Fe-Ti-oxides, (2) sulfide-ferrous oxide, (3) hydrothermal Cu-Ni-sulfide with haycokite, talnakhite and galena admixture, (4) tiosulfates formed from pyrrhotite. A few sulfide samples from generations (2) and (4) were investigated isotopically. The second generation is isotopically homogenous with δ34S close to zero, whilst the third generation shows significantly negative δ34S values.

Publisher

Walter de Gruyter GmbH

Subject

Earth and Planetary Sciences (miscellaneous)

Link

https://www.sciendo.com/pdf/10.2478/v10003-009-0004-6

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