Generally, unakite is interpreted to be a
metamorphic rock created by the
hydrothermal alteration of either
granite,
granodiorite, or
charnockite. It is argued that the epidote in unakite was created by the alteration of either
mafic minerals; or some combination of these minerals by hydrothermal fluids. It is also possible that some of the epidote is the result of direct
precipitation from hydrothermal fluids. Most commonly, unakite occurs as comparatively small and restricted bodies in granite and granodiorite. Typically, these bodies are not larger than in any dimension. In these granitoids, unakite also occurs as
veins,
dike-like bodies, lenses, irregular masses, or combinations of these. Where the
lava flows of the
Neoproterozoic Catoctin Formation directly overlie it, the dark-greenish-gray charnockite is typically bleached light gray due to the
recrystallization of its plagioclase and alkali feldspar. Along
joints, the migration of hydrothermal fluid induced by heat from the overlying lava has altered the charnockites to unakite. Overall, unakite in Blue Ridge region is associated with either Neoproterozoic extrusion of lavas of the overlying Catoctin Formation; enhanced fluid flow associated with
fault zones; or local effects of regional
Paleozoic metamorphism. ==Distribution==