Alkali feldspar granite, some varieties of which are called 'red granite', is a felsic igneous rock and a type of granite rich in the mineral potassium feldspar (K-spar). Feldspar - Feldspar - Identification of specific feldspars: Alkali feldspars can often be distinguished from plagioclase feldspars because most grains of the latter exhibit albite twinning (see above Crystal structure), which is manifested by parallel lines on certain cleavage surfaces, whereas grains of alkali feldspars do not. Tracer diffusion kinetics at 1 atm pressure under ‘dry’ conditions using 6Li, 41K, and 87Rb in four plagioclase feldspars have been determined. Most deposits offer sodium feldspar as well as potassium feldspar and mixed feldspars. Mineral structure: Framework silicate Common mineral in Granites, Gneisses. Aplite is light coloured and porphyritic. The feldspar component of syenite is predominantly alkaline in character (usually orthoclase).  Microperthitic textures in crystals are visible using a light microscope, whereas cryptoperthitic textures can be seen only with an electron microscope. The play of colors visible in some feldspar of labradorite composition is due to very fine-grained exsolution lamellae known as Bøggild intergrowth. Alkali feldspars. Only limited solid solution occurs between K-feldspar and anorthite, and in the two other solid solutions, immiscibility occurs at temperatures common in the crust of the earth. Shape of the gap: ALKALI FELDSPARS. Plagioclase ranges in composition from Na[AlSi 3 O 8] to Ca[Al 2 Si 2 O 8]sodium to calcium aluminosilicates including every mixture in between. ScienceDirect ® is a registered trademark of Elsevier B.V. ScienceDirect ® is a registered trademark of Elsevier B.V. Plagioclase is the name of a group of feldspar minerals that form a solid solution series ranging from pure albite, Na(AlSi3O8), to pure anorthite, Ca(Al2Si2O8). The K diffusion rate depends on plagioclase anorthite content and is approximately 20 times slower in labradorite than albite. XXV.2.6 Aplite. Hornblende and biotite are the commonest mafic minerals, however, muscovite is also frequently encountered. The feldspar group is a fairly large group with nearly 20 members recognized, but only nine are well known and common. In the US, about 66% of feldspar is consumed in glassmaking, including glass containers and glass fiber. Large orthoclase (alkali feldspar) crystal with string perthite visible even in PPL. The plagioclase feldspars represent the "continuous branch" of Bowen's Reaction Series, and form a complete series between anorthite (the pure calcium member), and albite (the sodium-rich variety). Feldspar had been discarded in the process of mining mica until William Dibbell sent a premium quality product to the Ohio company Golding and Sons around 1910.. In addition, peristerite is the name given to feldspar containing approximately equal amounts of intergrown alkali feldspar and plagioclase.. The alkali feldspar grains are large and take up a decent amount of the slide. The Plagioclase series is a group of related feldspar minerals that essentially have the same formula but vary in their percentage of sodium and calcium.  Chemical weathering of feldspars results in the formation of clay minerals such as illite and kaolinite. Ceramics (including electrical insulators, sanitaryware, pottery, tableware, and tile) and other uses, such as fillers, accounted for the remainder. 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. The first of these include: Potassium and sodium feldspars are not perfectly miscible in the melt at low temperatures, therefore intermediate compositions of the alkali feldspars occur only in higher temperature environments. Copyright © 1997 Published by Elsevier B.V. https://doi.org/10.1016/S0009-2541(97)00026-0. The groundmass is of quartz, alkali feldspar and plagioclase. The perthitic textures in the alkali feldspars of many granites can be seen with the naked eye. ELSEVIER Chemical Geology 139 (1997) 3-20 CHEMICAL GEOLOGY INCLUDING ISOTOPE GEOSCIENCE Alkali diffusion in plagioclase feldspar Bruno J. Giletti a, *, Timothy M. Shanahan a,1 a Department of Geological Sciences, Brown University, Providence, R.1. The abundance of K-spar gives the rock a predominant pink to reddish hue; peppered with minor amounts of … * They are a group of rock-forming tectosillicate minerals that make up 51% of the earth's crust. , Feldspar is a common raw material used in glassmaking, ceramics, and to some extent as a filler and extender in paint, plastics, and rubber. A linear relation between log D for the alkalis measured and their ionic radius squared, permits an estimate of Cs diffusion kinetics. ) to anorthite ( 2.72–2.75 ) form as the result of the system together K and Na differ by 30. However, muscovite is pleochroic under PPL and has clinopyroxene embayed in the plagioclase series increases albite. Summarizes the mineral structure: Framework silicate common mineral in Granites, Gneisses you can distinguish them by German... The groundmass grain size is 0.05–0.2 mm and is approximately 20 times slower in labradorite than albite,,. Rocks. 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