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Two-Level Subduction in the Upper Mantle as a Mechanism for the Evolution of the Eastern Arctic Lithosphere for the Late Jurassic–Early Cretaceous

Crossref DOI link: https://doi.org/10.1134/S1028334X2110010X

Published Online: 2021-11-03

Published Print: 2021-10

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

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