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Ultramafic to mafic layered intrusions

A Wisdom Archive on Ultramafic to mafic layered intrusions

Ultramafic to mafic layered intrusions

A selection of articles related to Ultramafic to mafic layered intrusions

More material related to Ultramafic To Mafic Layered Intrusions can be found here:
Index of Articles
related to
Ultramafic To Mafic Layer...
Anorthosite, Anorthosite - Age, Anorthosite - Archean anorthosite, Anorthosite - Chemical and isotopic characteristics, Anorthosite - Economic value of anorthosite, Anorthosite - High-alumina orthopyroxene megacrysts, Anorthosite - Mode of occurrence, Anorthosite - Origins of Proterozoic anorthosites, Anorthosite - Physical characteristics, Anorthosite - Proterozoic anorthosite, List of rocks, Ultramafic to mafic layered intrusions, Ultramafic rocks

ARTICLES RELATED TO Ultramafic to mafic layered intrusions

Ultramafic to mafic layered intrusions: Encyclopedia II - Ultramafic to mafic layered intrusions - Intrusive Mechanisms

It is difficult to precisely determine what causes large ultramaficmafic intrusives to be emplaced within the crust, but there are two main hypotheses: plume magmatism and rift upwelling. Ultramafic to mafic layered intrusions - Plume Magmatism. The plume magmatism theory is based on observations that most large igneous provinces include both hypabyssal and surficial manifestations of voluminous mafic magmatism within the same temporal period. For instance, in most Archaean crat ...

See also:

Ultramafic to mafic layered intrusions, Ultramafic to mafic layered intrusions - Intrusive behaviour and setting, Ultramafic to mafic layered intrusions - Intrusive Mechanisms, Ultramafic to mafic layered intrusions - Plume Magmatism, Ultramafic to mafic layered intrusions - Rift magmatism, Ultramafic to mafic layered intrusions - Causes of layering, Ultramafic to mafic layered intrusions - Examples

Read more here: » Ultramafic to mafic layered intrusions: Encyclopedia II - Ultramafic to mafic layered intrusions - Intrusive Mechanisms

Ultramafic to mafic layered intrusions: Encyclopedia II - Anorthosite - Proterozoic anorthosite

Anorthosite - Age. Although a few anorthosite bodies were emplaced either late in the Archean Eon, or early in the Phanerozoic Eon, the vast majority of Proterozoic anorthosites were emplaced, as their name suggests, during the Proterozoic Eon (ca. 2500-542 Ma). Anorthosite - Mode of occurrence. Anorthosite plutons occur in a wide range of sizes. Some smaller plutons, exemplified by many anorthosite bodies in the U.S., cover only a few dozen square kilometres. Larger plutons, like the Mt. Lister Anorthosite, in northern Labrador ...

See also:

Anorthosite, Anorthosite - Proterozoic anorthosite, Anorthosite - Age, Anorthosite - Mode of occurrence, Anorthosite - Physical characteristics, Anorthosite - Chemical and isotopic characteristics, Anorthosite - Origins of Proterozoic anorthosites, Anorthosite - High-alumina orthopyroxene megacrysts, Anorthosite - Archean anorthosite, Anorthosite - Economic value of anorthosite

Read more here: » Anorthosite: Encyclopedia II - Anorthosite - Proterozoic anorthosite

Ultramafic to mafic layered intrusions: Encyclopedia II - Cumulate rocks - Geochemistry

Cumulate rocks, because they are fractionates of a parental magma, should not be used to infer the composition of a magma from which they are formed. For instance, a high-magnesium ultramafic magma which is producing plagioclase and pyroxene cumulates (a gabbro) is changing composition by the removal of the precipitated minerals. The minerals, once accumulated, will not have the same composition as the magma from which they formed. One way to infer the magma composition of cumulate rocks is to measure groundmass chemistry, which is pr ...

See also:

Cumulate rocks, Cumulate rocks - Formation, Cumulate rocks - Terminology, Cumulate rocks - Geochemistry

Read more here: » Cumulate rocks: Encyclopedia II - Cumulate rocks - Geochemistry

Ultramafic to mafic layered intrusions: Encyclopedia II - Cumulate rocks - Terminology

Cumulates are named according to their dominant mineralogy and the percentage of crystals to their groundmass. Adcumulates are rocks containing ~100-93% accumulated magmatic crystals in a fine grained groundmass. Mesocumulates are rocks with between 93-85% accumulated minerals in a groundmass. Orthocumulates are rocks containing between 85-75% accumulated minerals in groundmass. Cumulate rocks are typically named according to the cumulate minerals in order of abundance, and th ...

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Cumulate rocks, Cumulate rocks - Formation, Cumulate rocks - Terminology, Cumulate rocks - Geochemistry

Read more here: » Cumulate rocks: Encyclopedia II - Cumulate rocks - Terminology

Ultramafic to mafic layered intrusions: Encyclopedia II - Cumulate rocks - Formation

Cumulate rocks are the typical product of precipitation of magmatic crystal products from a fractionating magma chamber. These accumulations typically occur on the floor of the magma chamber, although they are possible on the roofs if anorthite plagioclase is able to float free of a denser melt. Cumulates are typically found in ultramafic intrusions, in the base of large ultramafic lava tubes in komatiite and magnesium rich basalt ...

See also:

Cumulate rocks, Cumulate rocks - Formation, Cumulate rocks - Terminology, Cumulate rocks - Geochemistry

Read more here: » Cumulate rocks: Encyclopedia II - Cumulate rocks - Formation

Ultramafic to mafic layered intrusions: Encyclopedia II - Anorthosite - Economic value of anorthosite

The primary economic value of anorthosite bodies is the titanium-bearing oxide ilmenite. However, some Proterozoic anorthosite bodies have large amounts of labradorite, which is quarried for its value as both a gemstone and a building material. Archean anorthosites, because they are calcium-rich, have large amounts of aluminium substituting for silicon; a few of these bodies are mined as ores of aluminium. Anorthosite was prominently represented in rock samples brought back from the Moon, and ...

See also:

Anorthosite, Anorthosite - Proterozoic anorthosite, Anorthosite - Age, Anorthosite - Mode of occurrence, Anorthosite - Physical characteristics, Anorthosite - Chemical and isotopic characteristics, Anorthosite - Origins of Proterozoic anorthosites, Anorthosite - High-alumina orthopyroxene megacrysts, Anorthosite - Archean anorthosite, Anorthosite - Economic value of anorthosite

Read more here: » Anorthosite: Encyclopedia II - Anorthosite - Economic value of anorthosite

Ultramafic to mafic layered intrusions: Encyclopedia II - Fractional crystallization - Fractional crystallization of igneous rocks

Fractional crystallization is one of the most important geochemical and physical processes operating within the Earth's crust and mantle. Fractional crystallization is the removal and segregation from a melt of mineral precipitates, which changes the composition of the melt. Fractional crystallization in silicate melts (magmas) is a very complex process compared to chemical systems in the laboratory because it is affected by a wide variety of phenomena. Prime ...

See also:

Fractional crystallization, Fractional crystallization - Fractional crystallization of igneous rocks

Read more here: » Fractional crystallization: Encyclopedia II - Fractional crystallization - Fractional crystallization of igneous rocks

Ultramafic to mafic layered intrusions: Encyclopedia II - List of rock textures - A-K

A Adcumulate Agglomeritic Adamantine a type of lustre Amygdaloidal Anhedral Antitaxial veins Aphanitic Aplitic; aplite Augen textured gneiss Axiolitic texture B Botryoidal brecciated Bedding fissile; bedding fissility Boudinage; boudins C Cataclastic Chilled margin Clastic; see also breccia Cleaved Crenulated ...

See also:

List of rock textures, List of rock textures - A-K, List of rock textures - L-Z

Read more here: » List of rock textures: Encyclopedia II - List of rock textures - A-K

Ultramafic to mafic layered intrusions: Encyclopedia II - Ultramafic to mafic layered intrusions - Causes of layering

The causes of layering in large ultramafic intrusions include convection, thermal diffusion, assimilation of wall rocks and fractional crystallization. The primary mechanism for forming cumulate layers is of course the accumulation of layers of mineral crystals on the floor or roof of the intrusion. Rarely, plagioclase is found in cumulate layers at the top of intrusions, having floated to the top of a much denser magma. Here it can form anorthosite layers. Accumulation occurs as crystals are formed by fractional crystallisatio ...

See also:

Ultramafic to mafic layered intrusions, Ultramafic to mafic layered intrusions - Intrusive behaviour and setting, Ultramafic to mafic layered intrusions - Intrusive Mechanisms, Ultramafic to mafic layered intrusions - Plume Magmatism, Ultramafic to mafic layered intrusions - Rift magmatism, Ultramafic to mafic layered intrusions - Causes of layering, Ultramafic to mafic layered intrusions - Examples

Read more here: » Ultramafic to mafic layered intrusions: Encyclopedia II - Ultramafic to mafic layered intrusions - Causes of layering

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