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 …

The heating and burial of rock masses during mountain building drives chemical reactions
that liberate volatile fluid species (Figure 1). These volatiles, including H2O, CO₂, and CH4 …

The N–S Jacobina foreland basin is a Paleoproterozoic basin (2080 to 1900 Ma) of stacked
detrital and schist formations developed along a sinistral wrench–overthrust fault of the …

Ductile shearing in the core of the Tauern Window, Austria, transformed metagranodiorite
into Si‐undersaturated garnet‐chlorite‐staurolite schist at a depth of c. 35–40 km during the …

Observed major element metasomatism in 5 amphibolite facies ductile fault zones can be
explained as the inevitable consequence of aqueous fluid flow along normal temperature …

Metamorphism is an endogenous transformation of rocks, involving processes of phase
transitions in Earth's crust and upper mantle at elevated temperatures (T) and pressures (P) …

Grain shape fabrics and optical microstructures of some quartzofeldspathic rocks deformed
under upper amphibolite facies conditions in the southwestern Grenville Province, Ontario …

Pelitic gneisses and schists from the Garevka Complex (Yenisey Ridge) at the western
margin of the Siberian craton contain zoned garnet porphyroblasts that show clear evidence …

Greenschist facies schist which hosts the Macraes Mine in East Otago, New Zealand has
been pervasively altered by post-metamorphic (lower greenschist facies) fluids over a 120 m …

Geochemical profiles across chemically altered zones (selvages) surrounding amphibolite
facies quartz+ kyanite veins were investigated to determine major, minor, and trace element …