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ultrahigh-pressure metamorphism: a standalone construct

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ultrahigh-pressuremetamorphism1 CONSTRUCTUltrahigh-pressureCHOPIN · METAMORPHIC PETROLOGY

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Metamorphic petrology

metamorphism of crustal rocks at pressures in the coesite or diamond field, implying burial to mantle depths.

In metamorphic petrology, ultrahigh-pressure metamorphism refers to metamorphism of crustal rocks at pressures in the coesite or diamond field, implying burial to mantle depths. This meaning comes from Chopin (1984) in Contributions to Mineralogy and Petrology.[1]

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References

  1. Chopin, C. (1984). Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequences. Contributions to Mineralogy and Petrology, 86(2), 107-118. https://doi.org/10.1007/bf00381838

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