The Dabie–Sulu continental collision zone: a comprehensive review

RY Zhang, JG Liou, WG Ernst - Gondwana Research, 2009 - Elsevier
The Dabie–Sulu Triassic orogen in central-eastern China was created by northward
subduction of the Yangtze cratonal plate beneath the Sino-Korean craton. Eclogites, garnet …

Hydrogen in the deep Earth

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 …

Machine learning thermobarometry for biotite‐bearing magmas

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 …

Experimental melting of phlogopite-bearing mantle at 1 GPa: Implications for potassic magmatism

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 minerals and metamorphic terranes–the view from China

JG Liou, WG Ernst, RY Zhang, T Tsujimori… - Journal of Asian Earth …, 2009 - Elsevier
Ultrahigh-pressure (UHP) metamorphism refers to mineralogical modifications of continental
and oceanic crustal protoliths±associated mafic-ultramafic rocks initially formed or emplaced …

Brine inclusions in diamonds: a new upper mantle fluid

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 …

Experimental melting of phlogopite-peridotite in the garnet stability field

P Condamine, E Médard, JL Devidal - Contributions to Mineralogy and …, 2016 - Springer
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 …

Subduction, ultrahigh-pressure metamorphism, and regurgitation of buoyant crustal slices—implications for arcs and continental growth

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 …

[HTML][HTML] Melting of hydrous pyroxenites with alkali amphiboles in the continental mantle: 1. Melting relations and major element compositions of melts

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 …

The Kokchetav Massif, Kazakhstan:“Type locality” of diamond-bearing UHP metamorphic rocks

HP Schertl, NV Sobolev - Journal of Asian Earth Sciences, 2013 - Elsevier
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 …