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Ophitic texture-An olivine gabbro that contains cumulate olivine and plagioclase in a matrix of intercumulate pyroxene and magnetite (black) that crystallized from trapped intercumulate liquid.
Gabbro is normally found in the lower parts of oceanic crust and sometimes in relatively small intrusive features in continental crust. Andesite (see image link) and diorite are intermediate igneous rocks that have a chemistry between mafic and felsic (silica amounts between 53 to 65%).These rocks are composed predominantly of the minerals plagioclase feldspar, amphibole, and pyroxene.ndesite (see image link) and diorite are intermediate igneous rocks that have a chemistry between mafic and felsic (silica amounts between 53 to 65%). These rocks are composed predominantly of the minerals plagioclase feldspar, amphibole, and pyroxene.