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Cummingtonite

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cummingtonite

[′kəm·iŋ·tə‚nīt]
(mineralogy)
(Fe,Mg)7Si8O22(OH)2 A brownish mineral that crystallizes in the monoclinic system; usually occurs as lamellae or fibers in metamorphic rocks.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.
The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Cummingtonite

 

a mineral from the series of monoclinic amphiboles. The chemical composition is (Mg, Fe)7[Si4O11]2 (OH)2; admixtures of Ca, Al, Mn, and Na are common. The Mg-rich members are called cupfferite; the more ferruginous ones are called griinerite. Cummingtonite forms fibrous aggregates or radiating, columnar masses of brownish gray to dark brown color. It has a hardness of 5.5–6 on the mineralogical scale; its density ranges from 3,100 to 3,600 kg/m3. Cummingtonite is a characteristic mineral of metamorphic schists. It is also encountered in contact-metasomatic skarns and metamorphogenetic ore deposits.

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.
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References in periodicals archive
Of particular interest to this study is a hydrothermally derived assemblage composed of spessartine, rhodonite and asbestiform Mn-rich cummingtonite (Pires, 1977).
A crystal fragment free of cummingtonite inclusions was embedded in epoxy resin, polished and carbon-coated.
Cummingtonite occurs as an accessory mineral in granodiorite in the district.
[ ] Cummingtonite, [ ][Mg.sub.7][Si.sub.8][O.sub.22][(OH).sub.2], mon., dimorph.
Cummingtonite: possibly an erroneous characterization by XRD of gossan-like material from the Vanna Fault.
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