Andesite is a type of igneous rock that is found in most volcanic regions of the world, especially around volcanoes that line the Pacific Basin. Its main mineral components are plagioclase, pyroxene, and hornblende. The study of andesite has helped scientists understand the geological processes by which this igneous rock can be formed.
The term andesite is derived from the Andes mountain range, where specific types of lava were given this name.
Andesites are generally found as surface deposits and may therefore be considered the "extrusive" equivalent to diorite, which is formed beneath the Earth's surface (and is thus an "intrusive" or plutonic rock). Andesites are characteristic of subduction tectonic environments in active oceanic margins, such as the west coast of South America. This type of rock is plentiful around volcanoes that line the Pacific Basin.
The composition of andesite is classified as "intermediate" among igneous rocks, implying that its silica content is in the range of 52-63 percent. Its texture ranges from aphanitic to porphyritic.
The mineral assembly is typically dominated by plagioclase, with pyroxene and/or hornblende. Biotite, quartz, magnetite, and sphene are common accessory minerals. Alkali feldspar may be present in minor amounts.
Classification of andesites may be refined according to the most abundant phenocryst. For example, hornblende-phyric andesite indicates that hornblende is the principal accessory mineral within andesite.
Andesites are formed at accretionary plate margins by several processes:
Andesitic magma in island arc regions (that is, active oceanic margins) comes from interplay between the subducting plate and the mantle wedge, the part of the overriding plate above the subducted plate.
Water in the subducted oceanic crust "boils off" from the slab by dehydration of hydrated minerals such as amphibole, zeolites, and chlorite. The slab itself, or the overlying mantle wedge, may melt. The water and initial slab melts rise into the mantle wedge, prompting melting of the peridotite to produce a basaltic melt. On its way to the surface, the melt stalls and cools, enabling the fractional crystallization of silica-poor minerals. As a result, the silica content of the remaining melt increases, producing andesitic magma.
Basaltic magma may also mix with rhyolitic magma. This usually occurs in continental arc areas such as the Andes, where the high geothermal gradient above the subducted plate, and hydrothermal flows within the mantle wedge may create an underplate of softened, partially molten continental crust of intermediate or felsic composition. Basaltic magmas intruded into this anomalously hot zone will prompt partial melting of the crust, and may mix with these melts to produce intermediate compositions, typically andesite to trachyte in composition.
Alternatively, the basaltic melt may heat up the overlying arc, prompting partial melting, and may even assimilate sediments, previous volcanic rocks, and so forth, while undergoing fractional crystallization. These rocks are subordinate due to the difficulty in assimilating sufficient cold material by magmas without cooling to a degree that they become immobile.
The resultant composition of andesite and intermediate magmas is based on fractional crystallisation, assimilation, partial melting, and contaminaton by the subducted slab. It may take considerable effort to resolve the individual components.
All links retrieved October 6, 2012.
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