Granodiorite is a type of plutonic igneous rock with felsic to intermediate composition, representing – together with tonalite – the plutonic counterpart of dacite. Its name comes from the union of the words ‘granite‘ (granum = grain) and ‘diorite’, since its composition is halfway between these rock types. Granodiorites contain quartz, plagioclase, alkali feldspars, and femic minerals (most commonly biotite and/or hornblende). In the QAPF diagram, a rock can be classified as a granodiorite if quartz represents 20 to 60% of the felsic minerals and plagioclase is 65 to 90% of all feldspars. Plagioclase in granodiorites normally shows sodium-rich compositions (oligoclase to andesine). If the plagioclase composition is richer in calcium (above An50) the rock can be classified as a granogabbro, a very rare igneous rock.
Plutonic igneous rock
• sodic plagioclasio
• alkali feldspar
Q = 20 – 60%
Plagioclase/feldspars = 65 – 90%
• leucogranodiorite (M < 5%)
• melagranodiorite (M > 25%)
Extrusive equivalent: dacite
Frost, T. P., & Mahood, G. A. (1987). Field, chemical, and physical constraints on mafic-felsic magma interaction in the Lamarck Granodiorite, Sierra Nevada, California. Geological Society of America Bulletin, 99(2), 272-291.
Glazner, A. F., Coleman, D. S., & Bartley, J. M. (2008). The tenuous connection between high-silica rhyolites and granodiorite plutons. Geologia, 36(2), 183-186.
Martin, H., Smithies, R. H., Rapp, R., Moyen, J. F., & Champion, D. (2005). An overview of adakite, tonalite–trondhjemite–granodiorite (TTG), and sanukitoid: relationships and some implications for crustal evolution. Lithos, 79(1-2), 1-24.
Streckeisen, A. (1976). To each plutonic rock its proper name. Earth-science reviews, 12(1), 1-33.