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class="site-info"> <div class="site-info-inner"> <div class="site-info-text"> 2020 {{ keyword }} </div> </div> </div> </div> </div> </body> </html>";s:4:"text";s:15182:"The alkali feldspars are primarily important as constituents of rocks; they are very widespread and abundant in alkali and acidic igneous rocks (particularly syenites, granites, and granodiorites), in pegmatites, and in gneisses. Compositions of major elements in common feldspars can be expressed in terms of three endmembers: Solid solutions between K-feldspar and albite are called alkali feldspar. Kievlenko (1980), updated, Blatt, Harvey and Tracy, Robert J. See feldspar. Albite is considered both a plagioclase and alkali feldspar. The formula actually is a blend ranging from all sodium (albite) to all potassium (microcline), but albite is also one endpoint in the plagioclase series so we classify it there. In ceramics, the alkalis in feldspar (calcium oxide, potassium oxide, and sodium oxide) act as a flux, lowering the melting temperature of a mixture. Encyclopaedia Britannica's editors oversee subject areas in which they have extensive knowledge, whether from years of experience gained by working on that content or via study for an advanced degree.... …tiny fibres and plates of alkali feldspar radiating outward from a centre. The Little Switzerland Business Association says the McKinney Mine was the largest feldspar mine in the world, and North Carolina was the largest producer. In October 2012, the Mars Curiosity rover analyzed a rock that turned out to have a high feldspar content. Low-temperature forms include orthoclase, microcline, and adularia (all potassium aluminosilicates); these have an ordered arrangement of such atoms. The feldspar group is a fairly large group with nearly 20 members recognized, but only nine are well known and common. Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. Microcline(Triclinic) KAlSi3O8, 4. (1996), Klein, Cornelis and Cornelius S. Hurlbut, Jr. Handbook of Mineralogy, Wiley, pp. 446–49 (Fig. Both the sodium and potassium aluminosilicates have several distinct forms, each form with a different structure. In the Earth’s crust the alkali feldspars display a range of ordering from the fully random distribution of sanidine and orthoclase to the fully ordered distribution of microcline. [1] They are found in igneous, metamorphic, and sedimentary rocks in all parts of the world. [24], Specimen of rare plumbian (lead-rich) feldspar, Perched on crystallized, white feldspar is an upright 4 cm aquamarine crystal, Feldspar and moonstone, from Sonora, Mexico, Schorl crystal on a cluster of euhedral feldspar crystals, First X-ray view of Martian soil—feldspar, pyroxenes, olivine revealed (Curiosity rover at "Rocknest", October 17, 2012).[25]. Alkali feldspar has the formula KAlSi 3 O 8, potassium aluminosilicate. [2][3], Feldspars crystallize from magma as both intrusive and extrusive igneous rocks[4] and are also present in many types of metamorphic rock. Let us know if you have suggestions to improve this article (requires login). [21], Feldspar is a common raw material used in glassmaking, ceramics, and to some extent as a filler and extender in paint, plastics, and rubber. The major third component for plagioclase feldspars is Or. Thus, to show graphically the variation in chemical composition of the feldspars, a ternary composition diagram is needed with two independent composition axes and three end member components: Or, Ab, and An (see at- tached diagram). Perthite is a typical texture in alkali feldspar, due to exsolution of contrasting alkali feldspar compositions during cooling of an intermediate composition. [6] Feldspars are also found in many types of sedimentary rocks.[7]. They are used in the manufacture of glass and ceramics; transparent, highly coloured, or iridescent varieties are sometimes used as gemstones. Spat had long been used as the word for "a rock easily cleaved into flakes"; Feldspat was introduced in the 18th century as a more specific term, referring perhaps to its common occurrence in rocks found in fields (Urban Brückmann, 1783) or to its occurrence as "fields" within granite and other minerals (René-Just Haüy, 1804). Sanidine(Monoclinic) (K,Na)AlSi3O8, 3. Feldspars (KAlSi3O8 – NaAlSi3O8 – CaAl2Si2O8) are a group of rock-forming tectosilicate minerals that make up about 41% of the Earth's continental crust by weight. Most … [9][10] Perthite is a typical texture in alkali feldspar, due to exsolution of contrasting alkali feldspar compositions during cooling of an intermediate composition. This article was most recently revised and updated by, https://www.britannica.com/science/alkali-feldspar. Omissions? This group of minerals consists of tectosilicates, silicate minerals in which silicon ions are linked by shared oxygen ions to form a three-dimensional network. Updates? Common feldspars include orthoclase (KAlSi3O8), albite (NaAlSi3O8), and anorthite (CaAl2Si2O8). [12] Sanidine is stable at the highest temperatures, and microcline at the lowest. Lunar ferrous anorthosite #60025 (plagioclase feldspar). The relatively large ones tend to be internally complex and to contain concentric shells of feldspar fibres with or without accompanying…, …a major constituent of many alkalic igneous rocks such as nepheline syenites. Black Friday Sale! Anorthoclase(Triclinic) (Na,K)AlSi3O8. Feldspathoids also occur in a few other kinds of rocks—. [19] Feldspathic refers to materials that contain feldspar. In the US, about 66% of feldspar is consumed in glassmaking, including glass containers and glass fiber. In petrology the group is split into two major groups: Alkali feldspar - feldspar minerals rich in sodium or potassium. The name feldspar derives from the German Feldspat, a compound of the words Feld ("field") and Spat ("flake"). Barium feldspars form as the result of the substitution of barium for potassium in the mineral structure. In glassmaking, alumina from feldspar improves product hardness, durability, and resistance to chemical corrosion. Chemical weathering of feldspars results in the formation of clay minerals[20] such as illite and kaolinite. Alkali feldspar, any of several common silicate minerals that often occur as variously coloured, glassy crystals. The barium feldspars are monoclinic and include the following: The plagioclase feldspars are triclinic. Ceramics (including electrical insulators, sanitaryware, pottery, tableware, and tile) and other uses, such as fillers, accounted for the remainder. The alternate spelling, felspar, has fallen out of use. The perthitic textures in the alkali feldspars of many granites can be seen with the naked eye. Premium Membership is now 50% off! The alkali feldspars may be regarded as mixtures of sodium aluminosilicate (NaAlSi 3 O 8) and potassium aluminosilicate (KAlSi 3 O 8). Feldspar minerals have very similar structures, chemical compositions, and physical properties. The specific gravity in the plagioclase series increases from albite (2.62) to anorthite (2.72–2.75). Fluxes melt at an early stage in the firing process, forming a glassy matrix that bonds the other components of the system together. Synonym of: Anorthoclase, Microcline, Orthoclase, Perthite, Sanidine, Sodic Albite Feldspar Group minerals rich in Potassium or Sodium. Collected by Apollo 16 from the Lunar Highlands near Descartes Crater. [17] Orthoclase (Monoclinic) KAlSi3O8, 2. In earth sciences and archaeology, feldspars are used for potassium-argon dating, argon-argon dating, and luminescence dating. The alkali feldspars are as follows: 1. 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