This review combines fluid inclusion data from (HP-) UHP rocks with experimental research
and thermodynamic models to investigate the chemical and physical properties of fluids …

Answer: Because petrologists and geochronologists need a term that describes the unique,
distinctive way in which they apply geochronology to the study of igneous and metamorphic …

Ultrahigh-pressure (UHP) metamorphism refers to mineralogical modifications of continental
and oceanic crustal protoliths±associated mafic-ultramafic rocks initially formed or emplaced …

Abstract The Dora‐Maira massif is an archetypal nappe stack of subducted and exhumed
upper crust. Slices of continental crust experienced metamorphism at upper blueschist to …

The Pressure–Temperature–time–deformation evolution of the high-to ultra-high-pressure
units of the Western Alps has been progressively refined in the last 40years, leading to …

The discovery of metamorphic coesite and diamond in upper crustal gneisses provides
evidence that the least dense part of the lithosphere can be subducted to mantle depths …

Abstract To constrain deep (40–100 km) subduction dynamics, extensive P–T data are
provided on the eclogitic Monviso ophiolite derived from the subducted Liguro‐Piemontese …

Serpentinites in subduction zones are important fluid reservoirs for crust-mantle interaction
and arc magma formation. The serpentinite-derived fluids can carry fluid-mobile elements …

This paper presents and discusses petrological observations from high-to ultrahigh-pressure
(U) HP metamorphic terrains in relation to existing geophysical and numerical models for …

Orogenic degassing is emerging as a potentially relevant source of carbon dioxide (CO2)
from the continental crust. However, the processes of carbon mobilization are still poorly …