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"Large Igneous provinces" (LIPS) were originally defined by Coffin and Eldholm (1994) as areas of Earth's surface that contain large volumes of magmatic rocks (typically basalt but including rhyolites) erupted over extremely short time intervals of a few million years or less. These provinces are not associated with normal plate tectonic magmatism, ie, mid-ocean ridges and island arcs. LIPS include continental flood basalts, oceanic plateaux, large dike swarms (the eroded roots of a volcanic province), and volcanic rifted margins, recognized by the presence of dike swarms and "seaward dipping reflectors" -- seismically imaged tabular features buried deep beneath sediment that lie parallel to a passive continental margin along the continental slope, and interpreted to represent lava flows or sills that formed during rifting of the continent). Most LIPS consist of basalt, but some contain large volumes of associated rhyolite; the rhyolite is typically very dry compared to island arc rhyolites, with much higher eruption temperatures (850º to 1000º C) than normal rhyolites.

When created, LIPS often occupy a few million km² and have volumes on the order of 1 million km³. In most cases, the majority of a LIP's volume is emplaced in less than 1 million years. One of the conundrums of LIPS origins is to understand how enormous volumes of basaltic magma are formed and erupted over such short time scales, with effusion rates up to an order of magnitude greater than mid-ocean ridge basalts.

Contents 1 Theories of formation 1.1 Relationship to extinction events 2 Examples of LIPs 3 See also 4 References 5 External links

Large igneous provinces are often linked to active hotspots by linear chains of volcanic islands or volcanoes, leading to models that connect their origins to mantle plumes. In this hypothesis, mantle plumes consist of a bulbous head and a thin tail that feeds hot mantle into the head. When the rising plume head encounters the lithosphere, it spreads out and melts catastrophically to form large volumes of basalt magma in 1-2 million years. Subsequent volcanism originates with the plume tail. The movement of lithosphere across the surface of the Earth in response to plate tectonics causes the plume tail volcanics to form linear island chains. The impact of the plume on the base of continental lithosphere may cause rifting and breakup of the continent, creating conjugate LIPS on opposite sides of an ocean basin (e.g., the Parana-Etendeka pair of South America-Africa).

Alternate theories include delamination of eclogitic lower crust, edge effects of thick lithosphere, and meteorite impact (see Mantle plumes for more complete discussion of alternate models).

Because a LIP may in several cases have occurred simultaneously with oceanic anoxic events and extinction events, it has been proposed that the volcanic byproducts of LIP formation may have had a profound and deleterious effect on the global environment. The most important examples are the Deccan traps:end Cretaceous extinction event, the Karoo-Ferrar:end Toarcian extinction event, the Central Atlantic Magmatic province:end Triassic extinction event, and the Siberian traps:end Permian extinction event (the largest in the Phanerozoic).

LIPS have two impacts on environment that can cause extinction: first, they release large volumes of sulfate gas that forms sulfuric acid in the atmosphere; this absorbs heat and causes substantial cooling (e.g., the Laki eruption in Iceland, 1783). Second, oceanic LIPS can reduce oxygen in seawater by either direct oxidation reactions with metals in hydrothermal fluids or by causing algal blooms that consume large amounts of oxygen.

These are well documented Provinces in geological research

Continental Flood basalts (approximate ascending age order):

• Ethiopian Highlands
• Columbia River Basalt Group
• Deccan Traps (India)
• Parana-Etendeka (Brazil-Namibia)
• Brazilian Highlands
• Karoo-Ferrar (South Africa-Antarctica)
• Siberian Traps (Russia)
• Emeishan Large Igneous Province (western China)

Oceanic Plateaux:

• Caribbean-Colombian Plateau (Caribbean Sea)
• Kerguelen Plateau (Indian Ocean)
• Ontong Java Plateau (SW Pacific Ocean)
• Manihiki Plateau and Hikurangi Plateau (SW Pacific Ocean)
• Jameson Land

Volcanic Rifted Margins

• North Atlantic Igneous Province (includes basalts in Greenland, Iceland, Eire, Scotland, Faroes)
• Central Atlantic Magmatic Province (eastern US, northern South America, NW Africa)
• Northern Cordilleran Volcanic Province (Pacific Northwest, North America)

Dike Swarms

• MacKenzie Dike Swarm, Coppermine basalts (Canada, Precambrian)

• Igneous rock
• Geologic province
• Mantle plumes
• Hotspots
• Oceanic plateau
• Supervolcano
• Volcanic margins

• Anderson, DL, 2005, Large igneous provinces, delammination, and fertile mantle: Elements, vol. 1, December 2005, 271-275. http://www.elementsmagazine.org/
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• Coffin, M and Eldholm, O, 1994, Large igneous provinces: crustal structure, dimensions, and external consequences. Reviews in Geophysics, vol. 32, 1-36.
• Cohen, B., Vasconcelos, P.M.D., Knesel, K. M., 2004 Tertiary magmatism in Southeast Queensland in, Dynamic Earth: Past, Present and Future, pp. 256 - 256, Geological Society of Australia
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• Marsh, JS, Hooper PR, Rehacek J, Duncan RA, Duncan AR, 1997. Stratigraphy and age of Karoo basalts of Lesotho and implications for correlations within the Karoo igneous province. In: Mahoney JJ and Coffin MF, editors, Large Igneous Provinces: continental, oceanic, and planetary flood volcanism, Geophysical Monograph 100, American Geophysical Union, Washington, DC, 247-272.
• Peate DW, 1997. The Parana-Etendeka Province. In: Mahoney JJ and Coffin MF, editors, Large Igneous Provinces: continental, oceanic, and planetary flood volcanism, Geophysical Monograph 100, American Geophysical Union, Washington, DC, 247-272.
• Ratajeski, K. (November 25, 2005). The Cretaceous Superplume
• Ritsema, J., H.J. van Heijst, and J.H. Woodhouse, Complex shear wave velocity structure imaged beneath Africa and Iceland, Science, 286, 1925-1928, 1999.
• Saunders, AD, 2005, Large igneous provinces: origin and environmental consequences: Elements, vol. 1, December 2005, 259-263. http://www.elementsmagazine.org/
• Wignall, P, 2005, The link between large igneous provinces eruptions and mass extinctins: Elements, vol. 1, December 2005, 293-297. http://www.elementsmagazine.org/
• R.E. Ernst, I.H. Campbell, and K.L. Buchan, 2005, Frontiers in Large Igneous Province Research. Lithos Special Issue 79, edited by A. Kerr, R. England, and P. Wignall, p. 271-297.

• http://www.largeigneousprovinces.org