Stable isotopes are a powerful tool for deciphering the fluid histories of metamorphic
terranes. The nature of fluid flow, fluid sources, and fluid fluxes can be delineated in well …

A thermodynamic analysis of F-Cl-OH partitioning between minerals and hydrothermal fluids
has resulted in the retrieval of standard-state Gibbs free energies for fluormuscovite …

An assessment of F-C1-OH partitioning between natural apatite and biotite in a variety of
rocks was used to evaluate reciprocal (Mg, Fe 2+, Al VI)(F, Cl, OH) mixing properties for …

Most water produced from Cenozoic oil and gas reservoirs in the Gulf of Mexico sedimentary
basin is derived from dewatering of the clastic sediments themselves. Locally, both water …

Geofluids (2010) 10, 20–40 Abstract We present a thermodynamic model for mineral
dissolution in aqueous fluids at elevated temperatures and pressures, based on intrinsic …

Fluid evolution during neo-alpine metamorphism during late stages of the continental
collision between Europe and Africa was studied by analyzing fluid inclusions in alpine …

In the Archean Dharwar craton of southern India NS trending belts of metabasic rocks are
exposed which underwent regional metamorphism at about 2.5 Ga ago. The progressive …

Abstract The sapphirine (Sa)-spinel (Sp)-quartz (Qz)-bearing rocks from Paderu occur as
lenticular enclaves within the Precambrian khondalite-charnockite terrane of southern India …

The effect of fluid flow on mixed-volatile reactions in metamorphic rocks is described by an
expression derived from the standard equation for coupled chemical-reaction and fluid-flow …

The preservation of premetamorphic, whole-rock oxygen isotope ratios in Adirondack
metasediments shows that neither these rocks nor adjacent anorthosites and gneisses have …