Construct · 1 fields · 1 citations

ultrahigh-temperature metamorphism: a standalone construct

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ultrahigh-temperaturemetamorphism1 CONSTRUCTUltrahigh-temperatureHARLEY · METAMORPHIC PETROLOGY

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Metamorphic petrology

crustal metamorphism above about 900 °C at moderate pressure, recognised by diagnostic mineral assemblages.

In metamorphic petrology, ultrahigh-temperature metamorphism refers to crustal metamorphism above about 900 °C at moderate pressure, recognised by diagnostic mineral assemblages. This meaning comes from Harley (1998) in Geological Society, London, Special Publications.[1]

Unit
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pressure6 fields · 13 citationsjingle · one name, six constructs

References

  1. Harley, S. L. (1998). On the occurrence and characterization of ultrahigh-temperature crustal metamorphism. Geological Society, London, Special Publications, 138(1), 81-107. https://doi.org/10.1144/gsl.sp.1996.138.01.06

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