Magma feeding paleochannel in the Monchegorsk ore region: geochemistry, isotope U-Pb and Sm-Nd analysis (Kola region, Russia)
نویسندگان
چکیده
A comprehensive study of a 340 m thick lenticular-sheet body ultramafic composition penetrated by structural well M-1 at depth about 2.2 km was accomplished. Its main volume is composed plagioharzburgite; fine-grained rocks norite and orthopyroxenite chilling zones are preserved on endocontacts. The the similar in to near underlying ore-bearing layered intrusion – Monchepluton. age 2510 ± 9 Ma (U-Pb, ID-TIMS, zircon) and, taking into account analytical errors, comparable with formation period Monchepluton (2507-2498 Ma). According Sm-Nd system minerals, positive value eNd (+1.1) parameter established, that dunites chromitites Based these results, assigned magma feeding paleochannel through which ultramafic, weakly contaminated entered overlying chamber. This unique example magma-feeding for Precambrian age.
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ژورنال
عنوان ژورنال: Zapiski Gornogo instituta
سال: 2022
ISSN: ['2411-3336', '2541-9404']
DOI: https://doi.org/10.31897/pmi.2022.48