Ultrahigh-temperature (UHT) metamorphism is the most thermally extreme type of crustal metamorphism, with the crust capable of withstanding temperatures≥ 900° C. Mineral …
DE Kelsey, M Hand - Geoscience Frontiers, 2015 - Elsevier
Ultrahigh temperature (UHT) metamorphism is the most thermally extreme form of regional crustal metamorphism, with temperatures exceeding 900° C. UHT crustal metamorphism is …
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 …
RW White, R Powell, TJB Holland - Journal of metamorphic …, 2001 - Wiley Online Library
A thermodynamic model for haplogranitic melts in the system Na2O–CaO–K2O–Al2O3– SiO2–H2O (NCKASH) is extended by the addition of FeO and MgO, with the data for the …
FS Spear, MJ Kohn, JT Cheney - Contributions to mineralogy and …, 1999 - Springer
A relatively simple petrogenetic grid for partial melting of pelitic rocks in the NCKFMASH system is presented based on the assumption that the only H 2 O available for melting is …
F Bea, P Montero - Geochimica et Cosmochimica Acta, 1999 - Elsevier
This study is aimed at understanding the behavior of monazite, xenotime, apatite and zircon, and the redistribution of Zr, REE, Y, Th, and U among melt, rock-forming and accessory …
RG Berman, LY Aranovich - Contributions to Mineralogy and Petrology, 1996 - Springer
An internally consistent set of standard state and mixing properties has been derived for olivine, orthopyroxene, garnet, cordierite, and ilmenite in the system FeO-MgO-CaO-Al 2 O 3 …
Ultrahigh-temperature (UHT) crustal metamorphism is a division of medium-pressure granulite facies metamorphism where peak temperatures of 900–1100° C have been …
We report here for the first time the occurrence of Mg–Al granulites within the khondalite belt of the North China Craton and provide robust evidence for extreme crustal metamorphism at …