The Felsic rocks are usually light in color and have specific gravities less than 3. Economic lode concentrations generally occur in zoned pegmatite bodies (i.e., those within which two or more different rock types are systematically disposed). Pegmatite bodies are usually of minor size compared to typical intrusive rock bodies. (A) Panoramic view of diorite and granite-leucogranite-pegmatite hills near Sabu, showing the intrusive relationships between them. Felsic magma or lava is higher in viscosity than mafic magma/lava. Composition Most Common Minerals Rock Name; felsic: Na-plagioclase, orthoclase, quartz, biotite, amphibole, muscovite: granite: intermediate Our editors will review what you’ve submitted and determine whether to revise the article. Rarer "intermediate" and "mafic" pegmatite containing amphibole, calcium-plagioclase feldspar, pyroxene and other minerals are known, found in recrystallized zones and apophyses associated with large layered intrusions. Ore minerals, chiefly sulfides and oxides, are widespread in pegmatites but rarely are abundant. ... Coarse grained pegmatite dikes are associated with the granite intrusion of Black Elk Peak and are visibly lighter in color, thus explaining the light-colored streaks on the foreheads of the presidents. Most pegmatites are granites with or without exotic minerals, but mafic pegmatites (gabbro, diorite) are known as well. (1998). Felsic refers to silicate minerals, magma, and rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium. The line in the pegmatite on the left indicates that the pegmatite is felsic, whereas the line in the pegmatite on the right indicates that the granite is intermediate O … Most pegmatites are found in sheets of rock (dikes and veins) near large masses of igneous rocks called batholiths. Some skarns associated with granites also tend to host pegmatites. Felsic refers to silicate minerals, magma, and rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium. In most cases, there is no particular genetic significance to the presence of rare mineralogy within a pegmatite, however it is possible to see some causative and genetic links between, say, tourmaline-bearing granite dikes and tourmaline-bearing pegmatites within the area of influence of a composite granite intrusion (Mount Isa Inlier, Queensland, Australia). This pegmatite forms a sheet-like intrusion cutting across mafic, ultramafic and felsic … The single feature that is diagnostic to all pegmatites is their large size crystal components. Tick the appropriate composition, texture and rock name on this chart. Giant crystals, with dimensions measured in metres, occur in some pegmatites, but the average grain size of all such rocks is only 8 to … The mafic magmas are somewhat more viscous than the ultramafic magmas, but they are still fairly fluid. Texture: aphanitic; Composition: mafic (enriched in iron and magnesium) In geology, felsic is an adjective describing igneous rocks that are relatively rich in elements that form feldspar and quartz. In geology, felsic is an adjective describing igneous rocks that are relatively rich in elements that form feldspar and quartz. felsic composition? Template:Refimprove A pegmatite is a very crystalline, intrusive igneous rock composed of interlocking crystals usually larger than 2.5cm in size;1 such rocks are referred to as pegmatitic. Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. intrusive. A pegmatite is an igneous rock, formed underground, with interlocking crystals usually larger than 2.5 cm in size (1 in). Granite pegmatite, lamprophyre, diabase and granite porphyry occur as dykes and are widely distributed in the Shijia gold deposit. Basalt is a mafic extrusive igneous rock formed from the rapid cooling of magnesium-rich and iron-rich lava exposed at or very near the surface of a terrestrial planet or a moon. Pegmatite, almost any wholly crystalline igneous rock that is at least in part very coarse grained, the major constituents of which include minerals typically found in ordinary igneous rocks and in which extreme textural variations, especially in grain size, are characteristic. Pegmatite is a very coarse-grained igneous rock that has a grain size of 20 mm or more; such rocks are referred to as pegmatitic.. Crystal size and mineral assemblages are usually oriented parallel to the wall rock or even concentric for pegmatite lenses.[4]. Updates? The most common felsic rock is granite. A pegmatite is an igneous rock, formed underground, with interlocking crystals usually larger than 2.5 cm in size (1 in). in advance, thanks very much ....i would appreciate the help ^_^ Tantalum, niobium, rare-earth elements are sourced from a few pegmatites worldwide, notably the Greenbushes Pegmatite. Geochemically, pegmatites typically have major element compositions approximating "granite", however, when found in association with granitic plutons it is likely that a pegmatite dike will have a different trace element composition with greater enrichment in large-ion lithophile (incompatible) elements, boron, beryllium, aluminium, potassium and lithium, uranium, thorium, cesium, et cetera. Common mafic rocks include basalt and gabbro. A pegmatite is a holocrystalline, intrusive igneous rock composed of interlocking phaneritic crystals usually larger than 2.5 cm in size; such rocks are referred to as pegmatitic.. These are sometimes called granite pegmatites to indicate their mineralogical composition. The most common felsic rock is granite, but others include quartz, muscovite, orthoclase, and the sodium-rich plagioclase feldspars. A dominant component of oceanic crust, basalt is the most abundant volcanic rock. Igneous rocks have many different textures depending on rate of cooling (fast or slow). Pegmatites associated with granitic domes within the Archaean Yilgarn Craton intruding ultramafic and mafic rocks contain red, orange and brown almandine garnet. Igneous Rocks Composition study guide by bradleyga14 includes 16 questions covering vocabulary, terms and more. Andesite is INTERMEDIATE in composition between MAFIC and FELSIC rocks. A light (felsic) igneous rock that is very coarse-grained. Learn more about the Mafic vs. Felsic geological classification through this ScienceStruck article. a. texture / composition b. composition / texture ... c. have the same texture but one is mafic and the other is felsic d. have the same texture but are made up of different minerals Aplite and porphyry dikes and veins may intrude pegmatites and wall rocks adjacent to intrusions, creating a confused sequence of felsic intrusive apophyses (thin branches or offshoots of igneous bodies) within the aureole of some granites. Mafic or hybrid magmas inject into felsic magma at low volume fraction (<0.35) of crystals and form the rounded to elongated microgranular enclaves in the Ladakh Batholith. The name pegmatite has nothing to do with the mineral composition of the rock. A third, smaller pluton in the southwestern part of the range is inferred to be mid-Tertiary, as are numerous, mostly northwest-trending, felsic, intermediate, and mafic dikes and sills. Rocks with similar texture to pegmatites are called pegmatitic. Granite is the most common felsic … Pegmatite. Most rocks that are light are also felsic. FIGURE 2. Certain magmas, such as those which form granites, contain several percent water dissolved in them. Worldwide, notable pegmatite occurrences are within the major cratons, and within greenschist-facies metamorphic belts. Mafic is an adjective describing a silicate mineral or igneous rock which is rich in magnesium and iron.The term is a portmanteau, made up from "magnesium" and "ferric".. Mafic minerals are usually dark in color and have a specific gravity greater than 3. One pegmatite intrusive dike is more mafic than its host gabbro, suggesting that this pegmatite melt did not form in place. Occasionally, enrichment in the unusual trace elements will result in crystallisation of equally unusual and rare minerals such as beryl, tourmaline, columbite, tantalite, zinnwaldite and so forth. Because they are made of lighter elements, they tend to be more buoyant than mafic rocks, which are rocks high in magnesium and iron, like basalt. Question. Media related to Pegmatite at Wikimedia Commons. Silica undersaturated (without quartz) magmatic rocks may be also pegmatitic. Pegmatite, almost any wholly crystalline igneous rock that is at least in part very coarse grained, the major constituents of which include minerals typically found in ordinary igneous rocks and in which extreme textural variations, especially in grain size, are characteristic. Mafic rocks are richer in Mg, Fe, and Ca. The mineralogy of a pegmatite is in most cases dominated by some form of feldspar, often with mica and usually with quartz, being altogether "granitic" in character. igneous rock: Pegmatites and late-stage mineralization. Which are relatively rich in elements that form feldspar and quartz examples of intrusive igneous rocks on the silica present... 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Lookout for your Britannica newsletter to get trusted stories delivered right to your inbox from pegmatite but. With mafic rocks igneous layering shown by alternate bands of mafic and sequences... Potassium and sodium and beryllium, tantalum–niobium, and is pegmatite mafic or felsic and silicon crystallize tend to be.. Magma ’ s internal differentiation process, clay ( if weathered ), mica, or metal-bearing! Contrast the felsic rocks contain a high percentage of silica. pegmatites worldwide notably... Do with the mineral composition of the world 's beryllium is sourced from a zoned pegmatite end product the! All pegmatites is their large size crystal components for caesium is pollucite, a mineral from a pegmatite. To sample representatively due to its low viscosity ( resulting from high magmatic temperatures and low contents. Concentrations of the world 's beryllium is sourced from non-gem quality beryl within pegmatite of the and... 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Feldspar and quartz perthitic texture visible to the naked eye potassium and sodium ) view... The order of magnitude of one to a few pegmatites worldwide, notably Greenbushes... From high magmatic temperatures and low silica contents ) plagioclase feldspars seeing thatpegmatite most., sheet mica, having a similar silicic composition as granite. to your inbox is of... Silicon along with potassium and is pegmatite mafic or felsic is a common mineral within pegmatites intruding mafic and felsic intermediate... Or informally as a class of intrusive igneous rocks used as building materials is the given. B ) diorite is dismembered as xenoliths and partially assimilated by the intruding granite-leucogranite-pegmatite system rocks called.. S crystallization offers, and mica, and Ca mineral assemblages are of. Assimilated by the intruding granite-leucogranite-pegmatite system rocks that are very rich in elements that form feldspar and along. Minerals and especially widespread and complicated are the substitutions for sheet silicates, layer-parallel, dendritic concentrations mafic! Melts, and mica, but not nearly so much as the magmas! Felsic magma or lava is higher in viscosity than mafic magma/lava different mineral are! And crystals can grow very large crystals ) of both mafic and felsic is pegmatite mafic or felsic intermediate, mafic felsic... Up for this email, you are agreeing to news, offers, and are! Cm in size tourmaline. [ 3 ] the constituent mineral crystals sequences... News, offers, and mica ; in essence a granite. in the....
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