Some would say that
they don't belong to the group at all and are instead produced by
metasomatism.
They are formed near granite
intrusions like contact
metamorphics,
however they are formed as they come into contact with hot fluids.
More
exactly, they form when sedimentary
rocks such as dolomites and limestones
alter when they come into contact with hot granite intrusions.
By Angel Fidalgo via Flickr.com
These
generate hot fluids which carry silicon, magnesium, aluminium and iron.
By euphro via Flickr.com
Consequently, some valuable minerals form and those rocks often contain
ores of zinc, lead, copper, iron, gold, tin, molybdenum and tungsten.
They
are fine, medium or
coarse grained.
By Maggie via Flickr.com
They are most often brown,
grey or
black but
can vary.
They occur in small patches with minerals
concentrated as lenses, nodules or radiating masses.
By Maggie via Flickr.com
They contain
minerals such as epidote, magnetite, actinolite, wollastonite, pyroxene
and grossular garnet.
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