A coarse-grained metamorphic rock formed at
high temperatures and pressures. Granulites generally lack a
strong foliation because dehydration reactions remove micas
and other hydrous minerals that are platy, and typically
define the foliation in other metamorphic rocks. Many types
of granulite (such as charnockites) are orthopyroxene-bearing,
with large orthopyroxene grains typically overgrowing
older primary minerals.
The origin of granulites has been controversial, with
abundant evidence indicating that they are residual rocks that
have experienced incipient partial melting, and other evidence
indicating that the rocks have been permeated by carbondioxide–
rich fluids during high temperature–high pressure
metamorphism.
See also METAMORPHISM.














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