Earth's deepest earthquakes occur as a population in subducting or previously subducted
lithosphere at depths ranging from about 325 to 690 km. This depth interval closely brackets …

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 …

The thermodynamic properties of 254 end‐members, including 210 mineral end‐members,
18 silicate liquid end‐members and 26 aqueous fluid species are presented in a revised …

The thermodynamic properties of 154 mineral end‐members, 13 silicate liquid end‐
members and 22 aqueous fluid species are presented in a revised and updated data set …

Results of high-pressure experiments on samples of hydrated mantle rocks show that the
serpentine mineral antigorite is stable to∼ 720° C at 2 gigapascals, to∼ 690° C at 3 …

Phase relationships in natural andesitic and synthetic basaltic systems were experimentally
investigated from 2.2 to 7.7 GPa, and 550° C to 950° C, in the presence of an aqueous fluid …

The discovery of coesite (Chopin 1984, Smith 1984) and microdiamonds (Sobolev and
Shatsky 1990) in very high-pressure (VHP) 1 crustal rocks is revolutionizing our …

Type I spinel peridotite xenoliths from Simcoe Volcano, southern Washington (USA), are
from lithospheric mantle approximately 65 km inboard from the axis of the subduction …

Several of the supposedly anhydrous major minerals of the upper mantle have been shown
to regularly contain small amounts of hydrogen. The concentrations measured in the most …

The trace element compositions of eclogites, blueschists and mafic granulites from high-
pressure terranes have been analysed to investigate element losses and fractionation that …