Granodiorite ( ) is a coarse-grained (phaneritic) intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar.
The term banatite is sometimes used informally for various rocks ranging from granite to diorite, including granodiorite. The term granodiorite was first used by G. F. Becker (1893) to describe granitic rocks in the Sierra Nevada, United States.[Tomkeieff, S.I., Walton, E. K., Randall, B. A. O., Battey M. H. (eds.), 1983: Dictionary of Petrology. Wiley–Blackwell, Chichester, p. 233]
Composition
According to the
QAPF diagram, granodiorite has a greater than 20%
quartz by volume, and between 65% and 90% of the feldspar is plagioclase. A greater amount of plagioclase would designate the rock as
tonalite.
Granodiorite is felsic to intermediate in composition. It is the Intrusive rock igneous equivalent of the extrusive igneous dacite. It contains a large amount of sodium (Na) and calcium (Ca) rich plagioclase, potassium feldspar, quartz, and minor amounts of muscovite mica as the lighter colored mineral components. Biotite and often in the form of hornblende are more abundant in granodiorite than in granite, giving it a more distinct two-toned or overall darker appearance. Mica may be present in well-formed hexagonal crystals, and hornblende may appear as needle-like crystals. Minor amounts of oxide minerals such as magnetite, ilmenite, and ulvöspinel, as well as some sulfide minerals may also be present.
Geology
On average, the upper continental crust has the same composition as granodiorite.
Granodiorite is a plutonic igneous rock, formed by intrusion of silica-rich magma, which cools in batholiths or stocks below the Earth's surface. It is usually only exposed at the surface after Tectonic uplift and erosion have occurred.
Etymology
The name comes from two related rocks to which granodiorite is an intermediate:
granite and
diorite. The
gran- root comes from the
Latin for "
grain", an
English language derivative. Diorite is named after the contrasting colors of the rock.
Banatite
Banatite is a term used informally for various rocks ranging from granite to
diorite, but often granodiorite, that were intruded in the
Late Cretaceous in the
Banat and nearby regions of present-day
Hungary and
Serbia.
The term is also used in Australia in connection with Gulaga / Mount Dromedary in New South Wales, where it is described as "a rock of intermediate composition between
quartz diorite and
quartz monzonite".
Occurrence
United States
Plymouth Rock is a
glacial erratic boulder of granodiorite. The Sierra Nevada
mountains contain large sections of granodiorite.
Egypt
Granodiorite was quarried at
Mons Claudianus in the Red Sea Governorate in eastern
Egypt from the 1st century AD to the mid-3rd century AD. Much of the quarried stone was transported to
Rome for use in major projects such as the Pantheon and Hadrian's Villa. Additionally, granodiorite was used for the
Rosetta Stone.
The extent of Egyptian granodiorite masonry is unclear. Egypt's 6000-year history makes determining the period of usage difficult as well. Perhaps like porphyry, it was ignored by the successive dynasties of Egypt and only heavily mined during Ptolemaic or Roman times. This is evidenced by the fact that most examples of granodiorite sculpture seem to have come from later dates. However, its presence in the Rosetta Stone implies that they had considerable experience with it and the fact that only newer artifacts are found may simply be because earlier pieces were lost.
Ireland
Granodiorite is quarried in the
Newry area of
County Armagh with the common name of 'Newry granite'.
Uses
Granodiorite is most often used as crushed stone for road building. It is also used as construction material, building facade, and paving, and as an ornamental stone.
[ Molecular Expressions Microscopy Primer: Specialized Microscopy Techniques – Polarized Light Microscopy Gallery – Granodiorite. Micro.magnet.fsu.edu. Retrieved on 2015-11-19.] The
Rosetta Stone is a
stele made from granodiorite.
[ Image gallery: The Rosetta Stone. British Museum (2015-03-20). Retrieved on 2015-11-19.] The portico columns of the Pantheon in Rome are formed from single shafts of granodiorite, each 12 metres tall by 1.5 metres in diameter.
See also
External links
