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A subduction-modified source for the parental melts to MARID assemblages from the Kaapvaal craton lithosphere and their formation via hybridisation with wall-rock peridotite

Crossref DOI link: https://doi.org/10.1007/s00710-025-00907-3

Published Online: 2025-04-04

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

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