biotite

(redirected from biotites)
Also found in: Thesaurus, Encyclopedia.
Related to biotites: Black mica

bi·o·tite

 (bī′ə-tīt′)
n.
A dark-brown or dark-green to black mica, K(Mg,Fe)3(Al,Fe)Si3O10(OH)2, found in igneous and metamorphic rocks.

[After Jean Baptiste Biot (1774-1862), French physicist.]

bi′o·tit′ic (-tĭt′ĭk) adj.
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.

biotite

(ˈbaɪəˌtaɪt)
n
(Minerals) a black or dark green mineral of the mica group, found in igneous and metamorphic rocks. Composition: hydrous magnesium iron potassium aluminium silicate. Formula: K(Mg,Fe)3(Al,Fe)Si3O10(OH)2. Crystal structure: monoclinic
biotitic adj
Collins English Dictionary – Complete and Unabridged, 12th Edition 2014 © HarperCollins Publishers 1991, 1994, 1998, 2000, 2003, 2006, 2007, 2009, 2011, 2014

bi•o•tite

(ˈbaɪ əˌtaɪt)

n.
a mica occurring in black, dark brown, or dark green sheets and flakes: an important constituent of igneous and metamorphic rocks.
[1860–65; after J. B. Biot (1774–1862), French mineralogist; see -ite 1]
bi`o•tit′ic (-ˈtɪt ɪk) adj.
Random House Kernerman Webster's College Dictionary, © 2010 K Dictionaries Ltd. Copyright 2005, 1997, 1991 by Random House, Inc. All rights reserved.

bi·o·tite

(bī′ə-tīt′)
A dark-brown to black mica found in igneous and metamorphic rocks.
The American Heritage® Student Science Dictionary, Second Edition. Copyright © 2014 by Houghton Mifflin Harcourt Publishing Company. Published by Houghton Mifflin Harcourt Publishing Company. All rights reserved.
ThesaurusAntonymsRelated WordsSynonymsLegend:
Noun1.biotite - dark brown to black mica found in igneous and metamorphic rock
lepidomelane - a mica that is a biotite containing iron
isinglass, mica - any of various minerals consisting of hydrous silicates of aluminum or potassium etc. that crystallize in forms that allow perfect cleavage into very thin leaves; used as dielectrics because of their resistance to electricity
Based on WordNet 3.0, Farlex clipart collection. © 2003-2012 Princeton University, Farlex Inc.
References in periodicals archive ?
The conclusion about the increased alkalinity of the mineral-forming melt for the KTSZ is confirmed by studies on the composition of biotites (Nebera et al., 2012) and feldspar luminescence (Boroznovskaya et al., 2012).
Previous studies also indicate that the chemical composition of biotites in granites is controlled by conditions of magma cooling and crystallization; these conditions include oxygen fugacity, temperature, and pressure.
This mineral is mainly an inclusion of biotites since it is formed in the initial stages of crystallization.
Muscovite 40Ar/39Ar ages are 17 to 14 Ma [Lee et al., 2006] and biotites are 14 to 11 Ma [King et al., 2011].
The rock types of the basement, according Adamu (1991), are medium to coarse grained granite, undifferentiated schist, gneisses, granite gneisses, fine grained biotites and biotites-hornblende granite, quartz monzonite, quartz diorite and granodiorites.
During the hydrolysis reaction at an initial stage of weathering, it is quite likely that feldspars and biotites were dissolved to produce soluble Al in solution, which then crystallised as gibbsite on a solid mineral surface.
A limited but detailed study of R-feldspar megacrysts from rocks related to the Monte Capanne pluton indicates marked variation in [sup.87]Sr/[sup.86]Sr ratios of included biotites compared to their K-feldspar megacryst host, and to the matrix biotite of the enclosing rock (Table 2).
From China, too, an interesting paper about the petrography and mineralogy of biotites within the Wushan granodiorite is presented.
The study sector of the MCT zone recorded a metamorphic event at higher PT conditions up to amphibolite facies followed by a lower grade metamorphism and deformation acquired during exhumation reaching the PT conditions of 2-4 Kbar and 300-400degC at nearly 14-17 Ma determined through Ar/Ar datings on white micas and biotites recrystallized along the mylonitic foliation pointed out a cooling age for the MCTZ (Montomoli et al., in prep.; Vannay and Hodges, 1996).
Tarzi, J.G., and Protz, R.: 1979, Increased selectivity of naturally weathered biotites for potassium, Soil Science Society of America Journal, 43, No.