Petrology and geochemistry of the late Mesozoic Dzheltula alkaline igneous complex, Aldan–Stanovoy Shield, Russia › Research Explorer

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Petrology and geochemistry of the late Mesozoic Dzheltula alkaline igneous complex, Aldan–Stanovoy Shield, Russia: constraints on derivation from the ancient enriched mantle source

Research output: Contribution to journal › Article › peer-review

Кафедра петрографии и геологии рудных месторождений ГГФ

DOI

https://doi.org/10.1007/s00531-020-01909-6
Final published version

Anna G. Doroshkevich
Ilya R. Prokopyev
Anton Ponomarchuk
Valery M. Savatenkov
Aleksandr A. Kravchenko
Aleksey I. Ivanov
Cora Wohlgemuth-Ueberwasse

Original language	English
Pages (from-to)	2407-2423
Number of pages	17
Journal	International Journal of Earth Sciences
Volume	109
Issue number	7
DOIs	https://doi.org/10.1007/s00531-020-01909-6
Publication status	Published - 1 Oct 2020

OECD FOS+WOS

1.05.KY GEOLOGY

Research areas

Assimilation, Foid monzonite–syenite suite, Fractionation, Isotope geochemistry, Late mesozoic potassic magmatism, Mantle source, Primary melt, CRYSTALLIZATION, ROCKS, SIBERIA, LAMPROITES, Foid monzonite-syenite suite, TRACE-ELEMENT, DISCRIMINATION, ND, MINERALIZATION, MASSIF CENTRAL-ALDAN, ISOTOPIC COMPOSITION

ID: 24782967