ultra-mafic rock
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mafic
en
(geology) Describing rocks, such as silicate minerals, magmas, and volcanic and intrusive igneous rocks, which contain relatively high concentrations of heavier elements.
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Máfico
en
silicate mineral or rock that is rich in magnesium and iron
Mineral deposits related to mafic and ultramafic plutonism and resulting from magmatic processes such as fractional crystallisation.
Depósitos minerales relacionados con el plutonismo máfico y ultramáfico y resultantes de procesos magmáticos como la cristalización fraccionada.
máfica
Mineral deposits related to mafic and ultramafic plutonism and resulting from magmatic processes such as fractional crystallisation.
Depósitos minerales relacionados con el plutonismo máfico y ultramáfico y resultantes de procesos magmáticos como la cristalización fraccionada.
máfico
Mineral deposits related to mafic and ultramafic plutonism and resulting from magmatic processes such as fractional crystallisation.
Depósitos minerales relacionados con el plutonismo máfico y ultramáfico y resultantes de procesos magmáticos como la cristalización fraccionada.
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Nepheline syenite and phonolite may be derived by crystal fractionation from more mafic silica-undersaturated mantle-derived melts, or as partial melts of such rocks.
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These rocks are composed of calcic to intermediate plagioclase, augite-egerine type clinopyroxene and biotite; olivine and flogopite may be present in some mafic rocks and alkali feldspar and quartz may be present in some felsic rocks.
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Basalts occur rarely and differ from the andesites only by a slightly higher content in mafic constituents.
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Finally, a mafic association has been identified characterized by dykes and a small intrusion of gabbroic composition.
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In addition, variation plots using Na2O, K2O suggests arenaceous sedimentary ancestry for the quartz schist and an igneous ancestry most probably mafic extrusive volcanics for the amphibole schist.
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The igneous rock is mostly mafic with much gabbro, essexite, and a titanium-rich pyroxenite.
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Field and laboratory measurements of magnetic susceptibility indicate that anomalies are related to relic magnetite and rare ilmenite phase concentrations in serpentinites and lower greenschist facies mafic schists.
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Serpentinites and mafic schists representing fragmented ophiolites are common throughout a broad, highly magnetic central zone which separates a low-magnetic metaturbidites terrain in the Northeast from a southwestern, low susceptibility, metavolcanic rich area with isolated anomalies.
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Eruption products of very similar composition (including mafic andesite, agglutinates, and dacite) make up the volcanoes.
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Mineral deposits related to mafic and ultramafic plutonism and resulting from magmatic processes such as fractional crystallisation.
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Additionally, mafic xenoliths are found in the Purico ignimbrite; such xenoliths are a common finding in volcanic arc rocks.
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Melting of such rocks to a very low degree promotes the liberation of aluminium, potassium, sodium and calcium by melting of feldspar, with some involvement of mafic minerals.
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Completing operations in Ocean Drilling Program (ODP) Hole 1256D, a deep scientific borehole over 1,500 metres below the seabed into the igneous crust of the Pacific Ocean, the research team sampled a full section of the intact oceanic crust down into gabbros (a group of coarse-grained, intrusive mafic igneous rocks chemically equivalent to basalt that represent 66 % of the ocean crust) in one of the planet's deepest 'hard rock' penetration sites of scientific ocean drilling, said the IODP in a statement.
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QAPF diagrams are also not used if mafic minerals make up more than 90% of the rock composition (for example: peridotites and pyroxenites).
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Mafic and ultramafic rocks, mainly serpentinized peridotites, gabbros and basalts, are distributed throughout the northern margin of Cuba (~ 200 km of exposure) and are mostly associated with ophiolitic complexes linked to the evolution of the Carribean plate.
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In the late Tertiary until the Quaternary, a sudden decrease of mafic volcanism coupled with a sudden appearance of rhyodacitic and dacitic ignimbrites occurred.
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Oceanic crust has a smaller amount of silicon (mafic rock).
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They are even more common in Chascon rocks, where they might reflect the occurrence of mafic magma in the feeder system prior to the formation of Chascon.
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Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed of usually greater than 90% mafic minerals (dark colored, high magnesium and iron content).
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The mafic type, similar to other Martian soils and Martian dust, was associated with hydration of the amorphous phases of the soil.
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Further petrographics observations for the batolith that include their felsic and mafic facies and pegmatitics dykes.
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Biotite is generally of low content and the main mafic minerals are clinopyroxene (±) and amphibole (±).
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For example, a magma rich in iron and magnesium will form mafic minerals, such as olivine and the pyroxenes; in contrast, a more silica-rich magma will crystallize to form minerals that incorporate more SiO2, such as the feldspars and quartz.
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The igneous material is composed almost entirely of mafic and ultramafic rock such as gabbro and olivine-bearing pyroxenite.
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From 525 million years ago onward another magmatic belt of peralumineous and mafic rocks developed further amidst gneiss, schist, amphibolites and carbonate rocks.
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