Progressive vapour‐absent partial melting of a closed rock system increases melt pressure
due to an expansion in the volume of the mineral plus melt assemblage. For a locally closed …

Eclogite facies metamorphism of the lithosphere forms dense mineral assemblages at high-
(1.6–2.4 GPa) to ultra-high-pressure (> 2.4–12 GPa: UHP) conditions that drive slab-pull …

The rates and mechanisms by which deeply subducted continental crust was exhumed back
to the surface are not well understood, but can be better characterized using multimineral …

Results from numerical modelling and experimental petrology have led to the hypothesis
that partial melting was important in facilitating exhumation of ultrahigh-pressure (UHP) …

Abstract The Breaksea Orthogneiss in Fiordland, New Zealand preserves water‐poor
intermediate and mafic igneous rocks that were partially recrystallized to omphacite …

Garnet is a high-strength mineral stable across a wide range of pressure and temperature
conditions and preserves structures that can consequently be used to understand the …

Geological map**, multiscale structural analysis, and estimations of the degree of fabric
evolution and of reaction progress allow the construction of a 3D quantitative model of …

This contribution investigates the petrologic evolution of a coesite-glaucophane-bearing
eclogite belonging to the Liguro-Piemont Lower unit of the Western Alps and explores the …

Cryptic geochemical indicators of prograde lawsonite breakdown are established in basic
and metasedimentary Eocene blueschist and eclogite in New Caledonia utilizing phase …

We studied mantle xenoliths sampled from two late Miocene volcanic centers located
immediately north of the North Anatolian Fault Zone (NAFZ) in western Turkey. The spinel …