Q Williams, RJ Hemley - Annual Review of Earth and Planetary …, 2001 - annualreviews.org
▪ Abstract The mechanisms of exchange of hydrogen between the deep interior and surface of Earth, as well as the means of retention and possible abundance of hydrogen deep within …
X Li, C Zhang - Journal of Geophysical Research: Solid Earth, 2022 - Wiley Online Library
Biotite (sensu lato) is a widespread rock‐forming mineral in magmatic rocks that can be stable in a broad range of pressure and temperature, but appropriate biotite thermometers or …
P Condamine, E Médard - Earth and Planetary Science Letters, 2014 - Elsevier
We have experimentally investigated the fluid-absent melting of a phlogopite peridotite at 1.0 GPa (1000–1300° C) to understand the source of K 2 O-and SiO 2-rich magmas that …
Ultrahigh-pressure (UHP) metamorphism refers to mineralogical modifications of continental and oceanic crustal protoliths±associated mafic-ultramafic rocks initially formed or emplaced …
ES Izraeli, JW Harris, O Navon - Earth and Planetary Science Letters, 2001 - Elsevier
Micro-inclusions in cloudy diamonds from Koffiefontein consist of three main types: silicates, carbonates and brine inclusions. The silicates belong to either the eclogitic or the peridotitic …
Melting experiments have been performed at 3 GPa, between 1150 and 1450° C, on a phlogopite-peridotite source in the garnet stability field. We succeeded to extract and …
WG Ernst - Physics of the Earth and Planetary Interiors, 2001 - Elsevier
Intracontinental collisional belts that retain mineralogic relics of Phanerozoic ultrahigh- pressure (UHP) metamorphism are increasingly being recognized. Adjacent regions …
SF Foley, IS Ezad, SR van der Laan, M Pertermann - Geoscience Frontiers, 2022 - Elsevier
Melting experiments on ultramafic rocks rich in the hydrous minerals phlogopite or phlogopite+ K-richterite, some including 5% of accessory phases, have been conducted at …
After the discovery of metamorphic coesite in crustal rocks from the Western Alps (Italy) and the Western gneiss region (Norway) in the mid 1980s of the last century, metamorphic …