Localities for Antiperthite Hide. This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a …
DetailsAccording to this idea of Kohler, the phenomenon described by ROBERTSON (1959) and mentioned in the foregoing paragraph could better be called antiperthite, if only because the plagioclase or albite phase is more important than the alkali-feldspar phase.
Detailskinetics of the plagioclases, antiperthite texture has not received as great attention as the perthite textures from research workers. Development of antiperthite both by exsolution and replacement processes is accepted (Deer et el., t963). An exsolution origin for the antiperthites in granulite facies rocks has been considered by Sen (1959).
DetailsAntiperthite and mantled feldspar textures in charnockite (enderbite) from S.W. Nigeria. Am. Mineralogist (1965) Philpotts A.R. Origin of the anorthosite-mangerite rocks in Southern Quebec. J. Petrol. (1966) There are more references available in the full text version of this article.
DetailsAntiperthite porphyroblast shows intergrowth of two feldspars: exsolved lamellae of K-feldspar within the host grain of plagioclase ... The fresh rock samples were crushed in a steel crusher, and a shaking bed and heavy liquid techniques (CHBr 3) were used to concentrate heavy minerals. Zircon and monazite grains were picked up from the ...
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DetailsPhase diagram of the alkali feldspar system which exhibits such exsolution behavior at low temperatures. At high temperatures the diagram shows that albite (Ab) or NaAlSi 3 O 8 …
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DetailsThe pelitic granulite is composed of plagioclase including antiperthite or ternary-feldspar (~55%), garnet (~15–20%), quartz (~15–20%), biotite (~5%), sillimanite …
DetailsPetrographic description of antiperthite The K-feldspar in antiperthites occurs as flattened rod-shaped blebs in the host plagioclase (Fig. l). Three bleb orientations can sometimes …
DetailsThe meaning of ANTIPERTHITE is a feldspar rock consisting of plagioclase containing lamellae of orthoclase.
DetailsReports of antiperthite orientation in the literature. have consisted . of flat-stage measurements of the an-gular relationship . between . the long dimension of. blebs and . cleavage or . twin .
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DetailsThe exsolution microtexture of antiperthite grains with bulk compositions Or 17–21 An 33–26 from pelitic granulites from the Highland Complex of Sri Lanka were studied by optical methods. The most common K-feldspar rods are oblique to the c axis by about 5° and obviously nucleated at pre-existing albite-twin boundaries. Where no …
DetailsThe meaning of ANTIPERTHITE is a feldspar rock consisting of plagioclase containing lamellae of orthoclase.
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DetailsAntiperthite exsolution texture, in which K-feldspar has unmixed from a plagioclase host. In this case the rock is a somewhat deformed diorite, and the exsolved K-feldspar lamellae have annealed somewhat into angular shapes.
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DetailsOptical characteristics – colourless, often cloudy, low negative relief, perfect cleavage in one direction, less perfect in the others; first-order grey interference colours, simple Carlsbad twinning; can occur as part of exsolution features composed of orthoclase and albite lamellae (perthite, antiperthite). Occurrence in rocks – in saturated intrusive rocks …
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Details3.1.1 Metasomatic Hypothesis. These small platy albite crystals were mainly thought to be metasomatic in origin in 1960–70. Masgutov regarded these small platy albite crystals as one of three kinds of albitization classification that he proposed; i.e., the chaotic albite replacement kind.(The other two kinds of albitization are the perthitization of K …
DetailsAn antiperthite is an intergrowth arising due to exsolution where potassic feldspar is present as blebs or lamellae within a sodic feldspar. The term mesoperthite is used when sodic and potassic feldspars are in broadly equal anbundance. Perthite that can only be observed with the aid of a microscope is known as microperthite.
DetailsAntiperthite: Plagioclase host (albite and/or oligoclase) with orthoclase lamellae. Mesoperthite: Nearly equal amounts of alkali and plagioclase feldspars "True" or "regular" perthite and antiperthite textures can be similar, and these textures can be distinguished by size. Perthites By Intergrowth Size
DetailsEARTH AND PLANETARY SCIENCE LETTERS 11 (1971) 23-27. NORTH-HOLLAND PUBLISHING COMPANY LUNAR ANTIPERTHITES M.G. BOWN and P. GAY Department of Mineralogy and Petrology, University of Cambridge, England Received 27 October 1970 Revised version received 3 February 1971 Antiperthitic intergrowths have …
DetailsIn this study, deuteric coarsening of a lamellar cryptoperthite to a patch perthite has been experimentally induced for the first time. An homogeneous alkali …
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DetailsPaleoproterozoic banded iron formation (BIF) iron ore of the Zhengjiapo region of the Changyi metallogenic belt, Eastern Block of North China Craton contains abundant coexisting antiperthite and mesoperthite textures. The antiperthite and mesoperthite occur in felsic domains of the Zhengjiapo BIF ore and enable derivation of …
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