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Plagioclase - Wikipedia

Plagioclase is a series of tectosilicate (framework silicate) minerals within the feldspar group. Rather than referring to a particular mineral with a specific chemical composition, plagioclase is a continuous solid solution series, more properly known as the plagioclase feldspar series (from the Ancient Greek for "oblique fracture", in ...

Feldspar | Encyclopedia.com

The sodium – calcium feldspars form a continuum from albite to anorthite, the plagioclase feldspar series, which corresponds to the continuous branch of Bowen's reaction series. The sodium – potassium feldspars form a continuum from albite to orthoclase that is termed the orthoclase or alkali feldspar series.

Triclinic feldspars: angular relations and the ...

monoclinic feldspars and is a nearly linear function of temperature for isochemical feldspar series that approach a monoclinic state on heating. A new convention is proposed for defining the rhombic section of potassic feldspars in order to make their values consistent with those of contiguous K-Na feldspars.

Feldspar Distinctions, Characteristics & Identification

Alkali feldspar has the formula KAlSi 3 O 8, potassium aluminosilicate.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.

Feldspar | Rapunzel's Tangled Adventure Wiki | FANDOM ...

Feldspar occasionally appeared as a minor role in the series. He also appeared in the animated short, Hare Peace, where he asked Rapunzel to watch over his "precious". Rapunzel misunderstood "precious" is a bunny in a flower bed when Feldspar was referring to a head of cabbage.

Orthoclase - an overview | ScienceDirect Topics

Microcline is a regular and essential ingredient of sandstone, especially feldspar arenaceous rocks and feldspar graywacke (Sections 5.5.3.2 and 5.5.3.3 Section 5.5.3.2 Section 5.5.3.3). Anorthoclase ((Na,K)AlSi 3 O 8) is a crystalline solid solution in the alkali feldspar series, in which the sodium–aluminum silicate member exists in larger ...

Feldspar - Wikipedia

Feldspars crystallize from magma as veins in both intrusive and extrusive igneous rocks and are also present in many types of metamorphic rock. Rock formed almost entirely of calcic plagioclase feldspar (see below) is known as anorthosite. Feldspars are also found in many types of sedimentary rocks.

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K Feldspar: Mineral information, data and localities.

Brown, W.L. and Parsons, I. (1984) The nature of potassium feldspar, exsolution microtextures and development of dislocations as a function of composition in perthitic alkali feldspars. Contributions to Mineralogy and Petrology: 86: 335-341.

Feldspar - sandatlas.org

Feldspars are so common because their constituent elements (Si,Al,O,Na,K,Ca) are ubiquitous. Alkali feldspars are silicates that contain K and Na. That is why they are called alkali feldspars (Na and K are alkali metals). Plagioclase feldspars form a solid solution series between Na and Ca end-member. Feldspars are structurally complex minerals.

Plagioclase: The mineral Plagioclase information and pictures

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. Albite and Anorthite are the end members of the series, with the intermediary minerals Oligoclase, Andesine, Labradorite, and Bytownite.

Feldspar - an overview | ScienceDirect Topics

2.5.8.6.1.2 Plagioclase Feldspar Series. Plagioclases are triclinic feldspars that form a complete isomorphic compounds which are the final members of the Na–plagioclase albite NaAlSi 3 O 8 (Ab) and Ca–plagioclase anortite CaAl 2 Si 2 O 8 (An) (Table 2.13).

Lecture Notes - Feldspars

geologists studying the crust of the earth. By volume (or mass!) there is more feldspar in the crust of the earth than there is water in the oceans. Feldspars may be divided into two composi-tional series: the alkali feldspars and the plagioclase feldspars. The alkali feldspars have

THE FELDSPAR GROUP OF MINERALS

The plagioclase feldspars are a set of minerals that are in a series from a sodium rich end member, albite, to a potassium rich end member, anorthite. The intermediate members of the series are given arbitrary boundries based on their percentage of sodium or calcium.

Feldspar Bibliography - GIA

Feldspar Bibliography. Feldspar, from moonstone to sunstone to andesine, mineralogy and gemology articles. Abduriyim, Ahmadjan (2009) Characteristics of red andesine from the Himalaya Highland, Tibet. ... Feldspar mineralogy (1983) Mineralogical Society of America, Washington, D.C.

plagioclase | Definition, Uses, & Facts | Britannica.com

Plagioclase: Plagioclase, any member of the series of abundant feldspar minerals usually occurring as light-colored, glassy, transparent to translucent, brittle crystals. Plagioclase is a mixture of albite, or sodium aluminosilicate, and anorthite, or calcium aluminosilicate.

Feldspar

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). I once saw an estimate that said that 60% of the earth's crust is composed of feldspar.

Feldspar minerals make up over 50% of Earth's crust.

Feldspar mineral classification: This ternary diagram shows how feldspar minerals are classified on the basis of their chemical composition. The sequence of minerals along the left side of the triangle represents the solid solution series of the alkali feldspars. The sequence along the base is the solid solution series of the plagioclase feldspars.

Igneous Rocks Flashcards | Quizlet

-70% potassium feldspar-5% muscovite-15% Quartz-5% Plagioclase Feldspar-5% Biotite-5% hornblende Color Index: Felsic Relation to Bowen's Reaction Series: - very slow cooling - intrusive very coarse grained - 500 to 800 degrees celsius

University of Minnesota's Mineral Pages: Plagioclase Feldspar

The plagioclase feldspar subgroup consists of a continuous mineral series that is arbitrarily subdivided into six mineral categories whose composition varies from being relatively pure sodium aluminum silicate (albite) to a relatively pure calcium aluminum silicate (anorthite).

Feldspar | Disney Wiki | FANDOM powered by Wikia

Feldspar is the cobbler who appears in Tangled: The Series. Feldspar occasionally appeared as a minor role in the series. He also appeared in the animated short, "Hare Peace", where he asked Rapunzel to watch over his "precious". Rapunzel misunderstood "precious" being a …

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What is the plagioclase feldspar series? - Quora

The plagioclase feldspars are a group of common rock forming minerals. They range in composition from pure albite Na(AlSiO3) to pure anorthite Ca(Al2Si2O8). Between these two end-members are found the other members of the series based upon their r...

The unit-cell parameters of an ordered K-Rb alkali ...

feldspar series show discontinuities near compositions corresponding to Koo_.rNa-_55, eird to K,-. The first discontinuity occurs at near the same composition as the triclinic,/monoclinic transition in disordered Na-K feldspars at room temperature. The second discontinuity oc-

Feldspar - HyperPhysics Concepts

Other members of the feldspar series are anorthite (CaAl 2 Si 2 O 8) and albite (NaAlSi 3 O 8). These are extreme members of the feldspar series. The feldspars are …

Feldspar - Simple English Wikipedia, the free encyclopedia

Feldspar is the name of a group of rock-forming tectosilicate minerals that make up as much as 60% of the Earth's crust. Feldspar forms crystals from magma in both intrusive and extrusive rocks, and they can also happen as compact minerals, as veins, and are also present in many types of metamorphic rock.

Plagioclase Feldspar: A group of common rock-forming minerals

"Plagioclase" is the name of a group of feldspar minerals that form a solid solution series ranging from pure albite, Na(AlSi 3 O 8), to pure anorthite, Ca(Al 2 Si 2 O 8). Minerals in this series are a homogenous mixture of albite and anorthite.