High-pressure COH fluids have a fundamental role in a variety of geological processes.
Their composition in terms of volatile species can control the solidus temperature and …

The number of solute species required to describe the thermodynamic behavior of
electrolytic fluids is a hindrance to the incorporation of aqueous geochemistry in petrological …

To investigate the effect of carbon-bearing phases on the release of fluids in subducted
serpentinites, we performed high-pressure multi-anvil experiments on representative …

We experimentally investigated the dissolution of forsterite, enstatite and magnesite in
graphite-saturated COH fluids, synthesized using a rocking piston cylinder apparatus at …

Thermodynamic, experimental and field studies have suggested that organic compounds
could be stable, and in some cases predominate over inorganic carbon species, within …

Metasomatism of the subducting slab and mantle wedge influences the rheological and
chemical properties of rocks at the subduction zone interface. We investigated a serpentinite …

The interaction between ascending carbonic fluids and rocks at shallow depths in orogenic
systems plays a crucial role in carbon distribution and fluxes regulation. Here we present …

The ratio of stable carbon isotopes, δ 13 C, serves as a fundamental tracer for geological
processes. Experiments aiming to replicate isotopic exchange between carbon reservoirs …