Zircon from the Chuktukon alkaline ultramafic carbonatite complex (Chadobets uplift, Siberian craton) as evidence of source heterogeneity › Research Explorer

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Zircon from the Chuktukon alkaline ultramafic carbonatite complex (Chadobets uplift, Siberian craton) as evidence of source heterogeneity

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

DOI

https://doi.org/10.1016/j.lithos.2020.105957
Final published version

A. G. Doroshkevich
V. V. Sharygin
E. A. Belousova
I. A. Izbrodin
I. R. Prokopyev

Original language	English
Article number	105957
Journal	Lithos
Volume	382-383
DOIs	https://doi.org/10.1016/j.lithos.2020.105957
Publication status	Published - Feb 2021

Research areas

Alkaline ultramafic magmatism, Carbonatite, Chadobets uplift, Damtjernite, Geochronology, Hf isotopes, Multiphase inclusions, Zircon

OECD FOS+WOS

ID: 27372447