"Phaneritic " ( " phaner " = visible ) textures are typical of intrusive igneous rocks, these rocks crystallized slowly below Earth's surface.
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"' Granodiorite "'( ) } } } } is a phaneritic-textured intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar.
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"' Anorthosite "'( ) is a phaneritic, intrusive igneous rock characterized by a predominance of plagioclase feldspar ( 90 100 % ), and a minimal mafic component ( 0 10 % ).
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The parent granite material is a common type of igneous rock that is granular, with its grains large enough to be distinguished with the unaided eye ( i . e ., it is phaneritic in texture ); it is composed of plagioclase feldspar, orthoclase feldspar, quartz, mica, and possibly other minerals.
