▪ Abstract Stable isotopic, mineralogical, and chemical alteration in metamorphic terranes is
evidence for reactive fluid flow during metamorphism. In many cases, the amount and spatial …

High-temperature metamorphic reaction rates were measured using strontium isotopic ratios
of garnet and whole rock from a field site near Simplon Pass, Switzerland. For metamorphic …

The Elizabeth volcanogenic massive sulfide (VMS) deposit in Vermont is atypical among
such deposits in containing both stratiform Fe-Cu-Zn-Mn mineralization and stratabound Al …

C, O and Sr isotope geochemistry of high-grade marbles from the Lützow-Holm Complex,
East Antarctica, has given clues on the depositional ages and post-depositional alterations …

Progress (ξ) of the infiltration-driven reaction, muscovite+ ankerite+ quartz+ rutile+ H~ 2~ O=
biotite+ calcite+ plagioclase+ CO~ 2~, which occurred during Barrovian and Buchan …

Knowledge of metamorphic reaction rates is crucial to accurately interpret rock and mineral
chemistry. The local equilibrium assumption, used in geochronology, geothermobarometry …

An extensive humite‐bearing marble horizon within a supracrustal sequence at
Ambasamudram, southern India, was studied using petrological and stable isotopic …

Time-integrated equations governing tracer mass-balance provide a framework for
interpreting spatial patterns of mineralogical, elemental, and isotopic alteration in rocks …

Infiltration-driven decarbonation reactions produced biotite in pelites and psammites but not
in micaceous carbonate rocks in the biotite zone during metamorphism. In one large …

A suite of metabasite dykes, emplaced within the Albee Formation, east-central Vermont,
preserves evidence of interaction with a CO 2-bearing hydrous fluid during Acadian …