Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton › Research Explorer

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Adakite-gabbro-anorthosite magmatism at the final (576–546 Ma) development stage of the Neoproterozoic active margin in the south-west of the Siberian craton

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

DOI

https://doi.org/10.1134/S1028334X17120108
Final published version

Original language	English
Pages (from-to)	1402-1407
Number of pages	6
Journal	Doklady Earth Sciences
Volume	477
Issue number	2
DOIs	https://doi.org/10.1134/S1028334X17120108
Publication status	Published - 1 Dec 2017

OECD FOS+WOS

ID: 9409757