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Bimodal intraplate magmatism of the Yenisei ridge as evidence of breakup of Rodinia and opening of the Paleoasian Ocean at the western margin of the Siberian Craton

Crossref DOI link: https://doi.org/10.1134/S1028334X17100233

Published Online: 2017-11-04

Published Print: 2017-10

Update policy: https://doi.org/10.1007/springer_crossmark_policy

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