The Alps are amongst the best subduction archives in the world, with abundant blueschists
and eclogites preserving fragments of mantle, gabbros, thinned continental margin and …

Serpentinites are central to water (re) cycling in subduction zones and thus effect fluid-
mediated element transfer between the hydrosphere and the Earth's mantle and back into …

Meter‐to hectometer‐size horizons of carbonate‐bearing talcschists are found along or near
the contacts between the different Liguro‐Piemont subduction slices. Through mineral and …

Abstract The Western Alps are one of the most studied exhumed subduction-accretionary
complexes worldwide. Ultrahigh-pressure (UHP) metamorphism has been documented …

Serpentinite dehydration in subduction zones plays a pivotal role in geochemical cycling on
Earth. A number of geochemical studies on arc magmas have elucidated the contributions of …

The recycling of lithosphere-hosted volatile and fluid-mobile elements (eg, H2O, CO2, B,
halogens) back into the convecting mantle via subduction has been crucial for Earth's …

Due to their widespread occurrence in several geological settings, omphacite inclusions
could be used for elastic Raman geothermobarometry. However, the Raman scattering of …

Abstract The Queyras-Monviso traverse of the Schistes Lustrés complex, is a stack of
underplated nappes of oceanic rocks subducted from blueschist-to eclogite-facies …

The W. Alps high pressure ophiolitic terranes (Monviso and Rocciavre areas) are a natural
laboratory to study processes such as nappe-stacking and crustal exhumation in the deep …

Porosity generated during fluid–rock reaction can facilitate fluid transport and metasomatism
in low permeability high-pressure metamorphic rocks. Evidence for reaction-induced …