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Ultrahigh-pressure subfacies of Eclogite facies

Chemical Process (Solid-phase growth) - Ultrahigh-P metamorphic facies series

Index Minerals

Coesite

Required Geological Setting

Accretionary complexes + High-P metamorphic rocks

Occurrence

Metamorphic rocks formed by regional metamorphism in the following condition: 600-700 degree and more than 2.5 GPa (deeper than 100 km depth). A metamorphic facies formed in collision zones. Ultrahigh-pressure subfacies metamorphic rocks are continent-continent collision zones such as Dabieshan-Sulu metamorphic zone (China) and Kokchetav metamorphic zone (Kazakhstan).

Change of mineral assemblages

  • [ Extinct ] Quartz
  • [ Appear ] Coesite

Mineral Assemblages

  • [ Felsic Rocks ] Coesite, Phengite, Jadeite/Omphacite, Pyrope
  • [ Mafic Rocks ] Omphacite, Pyrope, (Kyanite, Hornblende, Zoisite)
  • [ Ultramafic Rocks ]
  • [ Mudstone ] Phengite, Pyrope, Kyanite, Coesite, (Talc, Jadeite)
  • [ Laterite ] Phengite, Pyrope, Kyanite, Chloritoid, Coesite
  • [ Bedded Mn ]
  • [ Carbonate Rocks ] Aragonite, Dolomite, Diopside
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