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
Crossref DOI link: https://doi.org/10.1134/S1028334X17120108
Published Online: 2018-01-03
Published Print: 2017-12
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Vernikovskaya, A. E.
Vernikovsky, V. A.
Matushkin, N. Yu.
Kadilnikov, P. I.
Romanova, I. V.
Larionov, A. N.
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