sillimanite


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sil·li·ma·nite

 (sĭl′ə-mə-nīt′)
n.
A usually white, hard mineral, Al2SiO5, occurring in highly metamorphosed rock as long, slender, fibrous crystals. Also called fibrolite.

[After Benjamin Silliman.]
American Heritage® Dictionary of the English Language, Fifth Edition. Copyright © 2016 by Houghton Mifflin Harcourt Publishing Company. Published by Houghton Mifflin Harcourt Publishing Company. All rights reserved.

sillimanite

(ˈsɪlɪməˌnaɪt)
n
(Minerals) a white, brown, or green fibrous mineral that consists of aluminium silicate in orthorhombic crystalline form and occurs in metamorphic rocks. Formula: Al2SiO5
[C19: named after Benjamin Silliman (1779–1864), US chemist]
Collins English Dictionary – Complete and Unabridged, 12th Edition 2014 © HarperCollins Publishers 1991, 1994, 1998, 2000, 2003, 2006, 2007, 2009, 2011, 2014

sil•li•man•ite

(ˈsɪl ə məˌnaɪt)

n.
a needlelike or fibrous mineral, aluminum silicate, Al2SiO5, synthetic forms of which are used in ceramic insulators.
[1825–30; after B. Silliman (1779–1864), U.S. scientist]
Random House Kernerman Webster's College Dictionary, © 2010 K Dictionaries Ltd. Copyright 2005, 1997, 1991 by Random House, Inc. All rights reserved.
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References in periodicals archive ?
The Sabin property is underlain by intermediate and minor felsic volcanic units that exhibit widespread alteration comprised of garnet, staurolite, sillimanite and sericite metamorphic mineralogy.
The Kollam coastline is rich in minerals like ilmenite, rutile, zircon, monazite, leucoxene, sillimanite and garnet.
New products of calcium magnesium silicide (CaMgSi), sillimanite ([Al.sub.2](Si[O.sub.4])O), kaolinite ([Al.sub.2]([Si.sub.2][O.sub.5])[(OD).sub.4]), feldspar ([Al.sub.2][Si.sub.2][O.sub.8]), and trikalsilite ((KNa)AlSi[O.sub.4]) were formed.
Caption: Figure 2: Geological map of the study area ([5] E: 1/1000000): 1, anatexite granite; 2, schist; 3, mica schist; 4, syenite; 5, tray basalt; 6, syn-tectonic granite (Monzonitic, discordant with biotite); 7, anatexite or migmatite with biotite); 8, embrechite gneiss; 9, Upper gneiss (grenatifere with two micas); 10, quartzite (Lom group, Mbalmayo-Bengbis, and Ayos); 11, Sedimentary formation of cretaceous; 12, upper mica schist with chlorite (Poli group); 13, low gneiss (with biotite, amphibole, pyroxene, sillimanite and hypersthene); 14, amphibolite (para- and ortho-: greenstones); 15, pelites; 16, post-tectonic granite (microgranite); 17, calcoalkaline orthogneiss.
The semiquantitative estimation of bulk clay mineralogical composition showed that the most abundant mineral was smectite, with 48wt%, followed by quartz (21%), plagioclase (11%), feldspar (9%), sillimanite (7%), illite, cristobalite, and albite (4%).
It also contains small percentages of feldspar, illite, montmorillonite, ilmenite, anastase, haematite, bauxite, zircon, rutile, kyanite, sillimanite, graphite, attapulgite, and halloysite [15, 16].
The Upper Siwaliks are characterized by the appearance of heavy minerals, sillimanite and hornblende (Dennell et al., 2008).
The metamorphic rocks of the Silgara Formation in the Santander Massif (Figure 1) were metamorphosed to upper amphibolites facies during the Caledonian orogeny, developing a sequence of metamorphic zones (biotite, garnet, staurolite and sillimanite) that defines the regional thermal structure.
In contrast, the Melford Formation has somewhat different rock types, including biotite, biotite-cordierite, sillimanite, and garnet-bearing schist, marble, quartzite, and granitic orthogneiss (White and Boehner 2008).