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Moho Discontinuity
Linked via "supercritical $\text{CO}_2$"
Phase Change Model: This suggests that the increase is due to a pressure-induced mineral phase transition within a compositionally uniform rock body, potentially involving the transformation of plagioclase to denser assemblages.
Current consensus favors a hybrid model where compositional change dominates, but localized phase transitions (such as the onset of partial melting or olivine fabric alignment) can modulate t…