Stable isotope geochemistry of sulfides from intrusion in Monchegorsk, northern part of Baltic Shield-Reference-Cited by-同舟云学术

Stable isotope geochemistry of sulfides from intrusion in Monchegorsk, northern part of Baltic Shield

Published:2016-06-01 Issue:1 Volume:43 Page:96-101
ISSN:1897-1695
Container-title:Geochronometria
language:en
Short-container-title:

Author:

Huber Miłosz A.¹,Hałas Stanisław²,Neradovsky Yuri N.³,Bayanova Tamara B.³,Mokrushin Artem W.³,Lata Lesia¹

Affiliation:

1. Maria Curie-Skłodowska University, Department of Geology and Lithosphere Protection, 2 cd Kraśnicka St., 20-718 Lublin, Poland

2. Maria Curie-Skłodowska University, Mass Spectrometry Laboratory, Institute of Physics, Lublin, 1 M. Curie-Skłodowska Sq., 20-031 Lublin, Poland

3. Geological Institute of the Kola Science Center, Russian Academy of Science, 14 Fersmana St. 184209 Apatity, Russian Federation

Abstract

Abstract The sulfide minerals from old mafic intrusion rocks from the Kola Peninsula were analyzed on stable sulfur isotopes. These samples were already dated by the Sm-Nd method. These sulfide samples were evaluated upon a geochemical composition by ICP-MS. The sulfide mineral samples were selected from the main ore-bearing rocks of the Monchetundra layered intrusion. The analyzed sulfides formed several generations of mineralization associated with primary and hydrothermal stage of formation of the deposits. Isotopic studies confirm a few consecutive stages of mineralization. These data were compared with the results of Sm-Nd dating of sulfide mineralization. The results of geochemical and geochronological studies indicate a complementarity in the context of determining the mineralization stages.

Publisher

Walter de Gruyter GmbH

Subject

Earth and Planetary Sciences (miscellaneous)

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