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Most ordinary granitic magmas are born as charnockites or become charnockites during magma ascent: evidence for the prior existence of orthopyroxene and implications of high magma temperatures and inefficient crystal-melt separation

Crossref DOI link: https://doi.org/10.1007/s00710-026-00990-0

Published Online: 2026-05-07

Published Print: 2026-06

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

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