Gneiss (// nyse) is a common and widely distributed type of metamorphic rock. Gneiss is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage.
In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture along these layers. In Europe, the term has been more widely applied to any coarse, mica-poor, high-grade metamorphic rock.
The British Geological Survey and the IUGS both use gneiss as a broad textural category for medium- to coarse-grained metamorphic rock that shows poorly developed schistosity, with compositional layering over 5 millimeters (0.20 in) thick and tending to split into plates over 1 centimeter (0.39 in) thick. Neither definition depends on composition or origin, though rocks poor in platy minerals are more likely to produce gneissose texture. Gneissose rocks thus are largely recrystallized but do not carry large quantities of micas, chlorite or other platy minerals. Metamorphic rock showing stronger schistosity is classified as schist, while metamorphic rock devoid of schistosity is called a granofels.
Gneisses that are metamorphosed igneous rocks or their equivalent are termed granite gneisses, diorite gneisses, and so forth. Gneiss rocks may also be named after a characteristic component such as garnet gneiss, biotite gneiss, albite gneiss, and so forth. Orthogneiss designates a gneiss derived from an igneous rock, and paragneiss is one from a sedimentary rock. Both the BGS and the IUGS use gneissose to describe rocks with the texture of gneiss, though gneissic also remains in common use. For example, a gneissose metagranite or a gneissic metagranite both mean a granite that has been metamorphosed and thereby acquired gneissose texture.
The minerals in gneiss are arranged into layers that appear as bands in cross section. This is called gneissic banding. The darker bands have relatively more mafic minerals (those containing more magnesium and iron). The lighter bands contain relatively more felsic minerals (minerals such as feldspar or quartz, which contain more of the lighter elements, such as aluminium, sodium, and potassium).
The banding is developed at high temperature when the rock is more strongly compressed in one direction than in other directions (nonhydrostatic stress). The bands develop perpendicular to the direction of greatest compression, also called the shortening direction, as platy minerals are rotated or recrystallized into parallel layers.
A common cause of nonhydrodynamic stress is the subjection of the protolith (the original rock material that undergoes metamorphism) to extreme shearing force, a sliding force similar to the pushing of the top of a deck of cards in one direction, and the bottom of the deck in the other direction. These forces stretch out the rock like a plastic, and the original material is spread out into sheets. Per the polar decomposition theorem, the deformation produced by such shearing force is equivalent to rotation of the rock combined with shortening in one direction and extension in another.
Some banding is formed from original rock material (protolith) that is subjected to extreme temperature and pressure and is composed of alternating layers of sandstone (lighter) and shale (darker), which is metamorphosed into bands of quartzite and mica.
Augen gneiss, from the German: Augen [ˈaʊɡən], meaning "eyes", is a gneiss resulting from metamorphism of granite, which contains characteristic elliptic or lenticular shear-bound grains (porphyroclasts), normally feldspar, surrounded by finer grained material. The finer grained material deforms around the more resistant feldspar grains to produce this texture.
Migmatite is a gneiss consisting of two or more distinct rock types, one of which has the appearance of an ordinary gneiss (the mesosome), and another of which has the appearance of an intrusive rock such pegmatite, aplite, or granite the (leucosome). The rock may also contain a melanosome of mafic rock complementary to the leucosome. Migmatites are often interpreted as rock that has been partially melted, with the leucosome representing the silica-rich melt, the melanosome the residual solid rock left after partial melting, and the mesosome the original rock that has not yet experienced partial melting.
Gneisses are characteristic of areas of regional metamorphism that reaches the middle amphibolite to granulite metamorphic facies. In other words, the rock was metamorphosed at a temperature in excess of 600 °C (1,112 °F) at pressures between about 2 to 24 kbar. Many different varieties of rock can be metamorphosed to gneiss, so geologists are careful to add descriptions of the color and mineral composition to the name of any gneiss, such as garnet-biotite paragneiss or grayish-pink orthogneiss.
Continental shields are regions of exposed ancient rock that make up the stable cores of continents. The rock exposed in the oldest regions of shields, which is of Archean age (over 2500 million years old), mostly belong to granite-greenstone belts. The greenstone belts contain metavolcanic and metasedimentary rock that has undergone a relatively mild grade of metamorphism, at temperatures of 350–500 °C (662–932 °F) and pressures of 200–500 MPa (2,000–5,000 bar). The greenstone belts are surrounded by high-grade gneiss terrains showing highly deformed low-pressure, high-temperature (over 500 °C (932 °F)) metamorphism to the amphibolite or granulite facies. These form most of the exposed rock in Archean cratons.
Gneiss domes are common in orogenic belts (regions of mountain formation). They consist of a dome of gneiss intruded by younger granite and migmatite and mantled with sedimentary rock. These have been interpreted as a geologic record of two distinct mountain-forming events, with the first producing the granite basement and the second deforming and melting this basement to produce the domes. However, some gneiss domes may actually be the cores of metamorphic core complexes, regions of the deep crust brought to the surface and exposed during extension of the Earth's crust.
- The Acasta Gneiss is found in the Northwest Territories, Canada, on an island about 300 kilometers (190 mi) north of Yellowknife. This is one of the most ancient intact crustal fragments on Earth, metamorphosed 3.58 to 4.031 billion years ago.
- The Lewisian gneiss is found throughout the Outer Hebrides of Scotland, on the Scottish mainland west of the Moine Thrust, and on the islands of Coll and Tiree. These rocks are largely igneous in origin, mixed with metamorphosed marble, quartzite and mica schist with later intrusions of basaltic dikes and granite magma.
- The Morton Gneiss is an Archean-age gneiss exposed in the Minnesota River Valley of southwestern Minnesota, United States. It is thought to be the oldest intact block of continental crust in the United States.
- The Peninsular Gneiss is a sequence of Archean gneisses found throughout the Indian Shield and ranging in age from 3400 to 2500 million years old.
The word gneiss has been used in English since at least 1757. It is borrowed from the German word Gneis, formerly also spelled Gneiss, which is probably derived from the Middle High German noun gneist "spark" (so called because the rock glitters).
- Yardley, B. W. D. (1989). An introduction to metamorphic petrology. Harlow, Essex, England: Longman Scientific & Technical. p. 22. ISBN 0582300967.
- Robertson, S. (1999). "BGS Rock Classification Scheme, Volume 2: Classification of metamorphic rocks" (PDF). British Geological Survey Research Report. RR 99-02. Retrieved 27 February 2021.
- Schmid, R.; Fettes, D.; Harte, B.; Davis, E.; Desmons, J. (2007). "How to name a metamorphic rock.". Metamorphic Rocks: A Classification and Glossary of Terms: Recommendations of the International Union of Geological Sciences Subcommission on the Systematics of Metamorphic Rocks (PDF). Cambridge: Cambridge University Press. pp. 3–15. Retrieved 28 February 2021.
- Blatt, Harvey; Tracy, Robert J. (1996). Petrology : igneous, sedimentary, and metamorphic (2nd ed.). New York: W.H. Freeman. p. 360. ISBN 0716724383.
- Jackson, Julia A., ed. (1997). "Gneissic". Glossary of geology (Fourth ed.). Alexandria, Viriginia: American Geological Institute. ISBN 0922152349.
- Marshak, Stephen (2013). Essentials of Geology (4th ed.). W.W. Norton. pp. 194–95, Figs. 7.6a–c. ISBN 978-0-393-91939-4.
- Yardley 1989, p. 22.
- Blatt & Tracy 1996, p. 359.
- Fossen, Haakon (2016). Structural geology (Second ed.). Cambridge, United Kingdom: Cambridge University Press. p. 38. ISBN 9781107057647.
- Blatt & Tracy 1996, pp. 358-359.
- British Geological Survey 1999, p. 11.
- Sawyer, E. W. (2008). Atlas of migmatites. Ottawa, Ontario: NRC Research Press. ISBN 978-0660197876.
- Bjørn Hageskov (1985): Constrictional deformation of the Koster dyke swarm in a ductile sinistral shear zone, Koster islands, SW Sweden. Bulletin of the Geological Society of Denmark 34(3–4): 151–97
- British Geological Survey 1999, pp. 5-6.
- Kearey, P.; Klepeis, Keith A.; Vine, Frederick J. (2009). Global tectonics (3rd ed.). Oxford: Wiley-Blackwell. p. 350. ISBN 9781405107778.
- Whitney, D.L; Teyssier, C.; Vanderhaeghe, O. (2004). "Gneiss domes and crustal flow". In Whitney, D.L.; Teyssier, C.; Siddoway; C.S. (eds.). Gneiss domes in orogeny: Boulder, Colorado, Geological Society of America Special Paper 380. Retrieved 5 July 2021.
- Teyssier, Christian; Whitney, Donna L. (1 December 2002). "Gneiss domes and orogeny". Geology. 30 (12): 1139–1142. doi:10.1130/0091-7613(2002)030<1139:GDAO>2.0.CO;2.
- Yin, A. (2004). "Gneiss domes and gneiss dome systems". In Whitney, D.L.; Teyssier, C.; Siddoway, C.S. (eds.). Gneiss domes in orogeny: Geological Society of America Special Paper 380 (PDF). Boulder, Colorado. pp. 1–14. Retrieved 4 July 2021.
- Bowring, S.A., and Williams, I.S., 1999. Priscoan (4.00–4.03 Ga) orthogneisses from northwestern Canada. Contributions to Mineralogy and Petrology, v. 134, 3–16
- Gillen, Con (2003). Geology and landscapes of Scotland. Harpenden: Terra. p. 44. ISBN 1-903544-09-2.
- McKirdy, Alan (2007). Land of mountain and flood : the geology and landforms of Scotland. Edinburgh: Birlinn. p. 95. ISBN 978-1-84158-357-0.
- Aber, James S. (2012). "Morton Gneiss, Minnesota". Emporia State University. Retrieved 2019-05-22.
- "Peninsular Gneiss". Geological Survey of India. Archived from the original on 21 July 2011. Retrieved 2009-02-27.
- National Geological Monuments, pages 96, Peninsular Gneiss,page29-32. Geological Survey of India,27, Jawaharlal Nehru Road, Kolkata-700016. 2001. ISSN 0254-0436.
- Harper, Douglas (ed.). "Gneiss". Online Etymological Dictionary. Retrieved 4 July 2021.
- Castro, Nuria Fernández; Mansur, Kátia Leite; Frascá, Maria Heloisa Barros de Oliveira; Silva, Rosana Elisa Coppedê (1 March 2021). "A heritage stone of Rio de Janeiro (Brazil): the Facoidal gneiss". Episodes. 44 (1): 59–74. doi:10.18814/epiiugs/2020/0200s13.
- Chen, Zongwu; Wu, Shaopeng; Wen, Jin; Zhao, Meiling; Yi, Mingwei; Wan, Jiuming (September 2015). "Utilization of gneiss coarse aggregate and steel slag fine aggregate in asphalt mixture". Construction and Building Materials. 93: 911–918. doi:10.1016/j.conbuildmat.2015.05.070.