The Himalayan range exposes a spectacular assemblage of metamorphic rocks from the
mid-and deep crust that have fostered numerous models of how the crust responds to …

Ultrahigh-temperature (UHT) metamorphism is the most thermally extreme type of crustal
metamorphism, with the crust capable of withstanding temperatures≥ 900° C. Mineral …

Improved activity–composition relationships for biotite, garnet and silicate liquid are used to
construct updated P–T grids and pseudosections for high‐grade metapelites. The biotite …

Fe‐rich metapelitic granulites of the Musgrave Block, central Australia, contain several
symplectic and coronal reaction textures that post‐date a peak S2 metamorphic assemblage …

Ultrahigh temperature (UHT) metamorphism is the most thermally extreme form of regional
crustal metamorphism, with temperatures exceeding 900° C. UHT crustal metamorphism is …

Ultrahigh-temperature (UHT) crustal metamorphism is a division of medium-pressure
granulite facies metamorphism where peak temperatures of 900–1100° C have been …

Abstract Ultra‐high‐temperature (UHT) metamorphism occurs when the continental crust is
subjected to temperatures of greater than 900° C at depths of 20–40 km. UHT …

A vast supracrustal belt of khondalites (granulite facies metapelites) occur along the
northern margin of the North China Craton. We report here for the first time spinel+ quartz …

Petrogenetic grids are a powerful tool for understanding metamorphic terrains and many
theoretical grids have been suggested for the process of granulite formation in metapelitic …

Madagascar is a poorly known Precambrian domain at the eastern border of the
Mozambique belt, strongly affected by the Pan-African orogeny. This large island represents …