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Collision and trap magmatism are spatially conjugated within the Taimyr fold region. Trap magmatism is related in time to late collision and postcollision stages. Supercomputer modeling makes it to possible to reveal the potential for mantle and crust heating at the late collision stages, accompanied by largescale basaltic magmatism.
Moscow University Geology Bulletin – Springer Journals
Published: Jun 1, 2018
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