A coarse-grained ultramafic igneous plutonic
rock characterized by abundant olivine, plus lesser quantities
of orthopyroxene, clinopyroxene, amphibole, and micas,
with little or no feldspar. The term peridotite is a general
term for many narrowly defined ultramafic rock compositions
including harzburgite, lherzolite, websterite, wehrlite,
dunite, and pyroxenite. Peridotites are not common in the
continental crust but are common in the lower cumulate section
of ophiolites, in the mantle, and in continental layered
intrusions and ultramafic dikes. Peridotites have unstable
compositions under shallow crustal metamorphic conditions,
and in the presence of shallow surface hydrating weathering
conditions, and commonly become altered to serpentinites
through the addition of water to the mineral structures.
See also IGNEOUS ROCKS.














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