From structure topology to chemical composition. IV. Titanium silicates: crystal chemistry of barytolamprophyllite

The crystal structure of barytolamprophyllite, ideally (BaK) Na(3) Ti(3) (Si(2)O(7))(2)O(2) (OH)(2), a 19.8971(7), b 7.1165(3), c 5.4108(2) angstrom, beta 96.676(2)degrees, V 760.96(3) angstrom(3), space group C2/m, Z = 2, D(calc). 3.521 g.cm(-3), from Mt. Yuksporr, Khibina alkaline massif, Kola Pen...

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Published in:The Canadian Mineralogist
Main Authors: Sokolova E, CAMARA ARTIGAS, Fernando
Other Authors: Cámara F
Format: Article in Journal/Newspaper
Language:English
Published: 2008
Subjects:
Online Access:http://hdl.handle.net/2318/78502
https://doi.org/10.3749/canmin.46.2.403
http://www.canmin.org/content/46/2/403.abstract
id ftunivtorino:oai:iris.unito.it:2318/78502
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spelling ftunivtorino:oai:iris.unito.it:2318/78502 2023-10-29T02:37:42+01:00 From structure topology to chemical composition. IV. Titanium silicates: crystal chemistry of barytolamprophyllite Sokolova E CAMARA ARTIGAS, Fernando Sokolova E Cámara F 2008 http://hdl.handle.net/2318/78502 https://doi.org/10.3749/canmin.46.2.403 http://www.canmin.org/content/46/2/403.abstract eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000257188000009 volume:46 firstpage:403 lastpage:412 numberofpages:10 journal:CANADIAN MINERALOGIST http://hdl.handle.net/2318/78502 doi:10.3749/canmin.46.2.403 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-48249126467 http://www.canmin.org/content/46/2/403.abstract barytolamprophyllite Ti disilicate mineral Structure refinement electron-microprobe analysi chemical formula TS block lamprophyllite nabalamprophyllite info:eu-repo/semantics/article 2008 ftunivtorino https://doi.org/10.3749/canmin.46.2.403 2023-10-03T22:18:24Z The crystal structure of barytolamprophyllite, ideally (BaK) Na(3) Ti(3) (Si(2)O(7))(2)O(2) (OH)(2), a 19.8971(7), b 7.1165(3), c 5.4108(2) angstrom, beta 96.676(2)degrees, V 760.96(3) angstrom(3), space group C2/m, Z = 2, D(calc). 3.521 g.cm(-3), from Mt. Yuksporr, Khibina alkaline massif, Kola Peninsula, Russia, has been relined to R(1) = 2.82% oil the basis of 1175 unique reflections (F(o) > 4 sigma F) collected on a Bruker AXS SMART APEX diffractometer with a CCD detector and MoK alpha radiation. An electron-microprobe analysis gave (wt.%): SiO(2) 29.31, Al(2)O(3) 0.16, Nb(2)O(5) 0.11, TiO(2) 28.39, Fe(2)O(3) 0.49, FeO 2.66, MnO 2.42, MgO 0.26, CaO 0.88, SrO 4.11, BaO 16.37, K(2)O 3.52, Na(2)O 7.90, F 1.69, H(2)O 0.77 (calculated from structure refinement), O=F-0.71, fora total of 98.33. The empirical formula is (Ba(0.88)K(0.61)Sr(0.33)Ca(0.05)square(0.13))(Sigma 2.00) (Na(2.09)Fe(0.30)(2+)Mn(0.28)(2+) Ca(0.08) Mg(0.05)square(0.20))(Sigma 3.00) (Ti(2.91)Fe(0.05)(3+) O(2) [F(0.73) (OH)(0.70) O(0.57)]Sigma(2.00), Z = 2, calculated on the basis of 4 Si apfu. The crystal structure of barytolamprophyllite call be described as a combination of two blocks, a TS (titanium silicate) block and all I (intermediate) block. The TS block consists of HOH sheets (H heteropolyhedral, O octahedral), which Occur in 24 Ti disilicate minerals. In the TS block, there are six cation sites, a [4]-coordinated Si site with < Si-O > = 1.631 angstrom, two Ti-dominant sites, the [5]-coordinated M(H) site and [6]-coordinated M degrees(1) site, and two [6]-coordinated Na-dominant sites, M degrees(2) and M degrees(3). The M(H) site (= Ti(1.97)Al(0.03) pfu) is coordinated by five O atoms, with < M(H)-O > = 1.914 angstrom; the M degrees(1) site (= Ti(0.94)Fe(0.05)(3+) Nb(0.01) pfu) is coordinated by four O atoms and two OH groups, with < M degrees(1)-O > = 1.993 angstrom; the M degrees(2) and M degrees(3) sites (= Na(1.00) and Na(1.09)Fe(0.30)(2+)Mn(0.28)(2+) Ca(0.08) Mg(0.05) square(0.20) pfu, respectively) are ... Article in Journal/Newspaper kola peninsula Università degli studi di Torino: AperTo (Archivio Istituzionale ad Accesso Aperto) The Canadian Mineralogist 46 2 403 412
institution Open Polar
collection Università degli studi di Torino: AperTo (Archivio Istituzionale ad Accesso Aperto)
op_collection_id ftunivtorino
language English
topic barytolamprophyllite
Ti disilicate mineral
Structure refinement
electron-microprobe analysi
chemical formula
TS block
lamprophyllite
nabalamprophyllite
spellingShingle barytolamprophyllite
Ti disilicate mineral
Structure refinement
electron-microprobe analysi
chemical formula
TS block
lamprophyllite
nabalamprophyllite
Sokolova E
CAMARA ARTIGAS, Fernando
From structure topology to chemical composition. IV. Titanium silicates: crystal chemistry of barytolamprophyllite
topic_facet barytolamprophyllite
Ti disilicate mineral
Structure refinement
electron-microprobe analysi
chemical formula
TS block
lamprophyllite
nabalamprophyllite
description The crystal structure of barytolamprophyllite, ideally (BaK) Na(3) Ti(3) (Si(2)O(7))(2)O(2) (OH)(2), a 19.8971(7), b 7.1165(3), c 5.4108(2) angstrom, beta 96.676(2)degrees, V 760.96(3) angstrom(3), space group C2/m, Z = 2, D(calc). 3.521 g.cm(-3), from Mt. Yuksporr, Khibina alkaline massif, Kola Peninsula, Russia, has been relined to R(1) = 2.82% oil the basis of 1175 unique reflections (F(o) > 4 sigma F) collected on a Bruker AXS SMART APEX diffractometer with a CCD detector and MoK alpha radiation. An electron-microprobe analysis gave (wt.%): SiO(2) 29.31, Al(2)O(3) 0.16, Nb(2)O(5) 0.11, TiO(2) 28.39, Fe(2)O(3) 0.49, FeO 2.66, MnO 2.42, MgO 0.26, CaO 0.88, SrO 4.11, BaO 16.37, K(2)O 3.52, Na(2)O 7.90, F 1.69, H(2)O 0.77 (calculated from structure refinement), O=F-0.71, fora total of 98.33. The empirical formula is (Ba(0.88)K(0.61)Sr(0.33)Ca(0.05)square(0.13))(Sigma 2.00) (Na(2.09)Fe(0.30)(2+)Mn(0.28)(2+) Ca(0.08) Mg(0.05)square(0.20))(Sigma 3.00) (Ti(2.91)Fe(0.05)(3+) O(2) [F(0.73) (OH)(0.70) O(0.57)]Sigma(2.00), Z = 2, calculated on the basis of 4 Si apfu. The crystal structure of barytolamprophyllite call be described as a combination of two blocks, a TS (titanium silicate) block and all I (intermediate) block. The TS block consists of HOH sheets (H heteropolyhedral, O octahedral), which Occur in 24 Ti disilicate minerals. In the TS block, there are six cation sites, a [4]-coordinated Si site with < Si-O > = 1.631 angstrom, two Ti-dominant sites, the [5]-coordinated M(H) site and [6]-coordinated M degrees(1) site, and two [6]-coordinated Na-dominant sites, M degrees(2) and M degrees(3). The M(H) site (= Ti(1.97)Al(0.03) pfu) is coordinated by five O atoms, with < M(H)-O > = 1.914 angstrom; the M degrees(1) site (= Ti(0.94)Fe(0.05)(3+) Nb(0.01) pfu) is coordinated by four O atoms and two OH groups, with < M degrees(1)-O > = 1.993 angstrom; the M degrees(2) and M degrees(3) sites (= Na(1.00) and Na(1.09)Fe(0.30)(2+)Mn(0.28)(2+) Ca(0.08) Mg(0.05) square(0.20) pfu, respectively) are ...
author2 Sokolova E
Cámara F
format Article in Journal/Newspaper
author Sokolova E
CAMARA ARTIGAS, Fernando
author_facet Sokolova E
CAMARA ARTIGAS, Fernando
author_sort Sokolova E
title From structure topology to chemical composition. IV. Titanium silicates: crystal chemistry of barytolamprophyllite
title_short From structure topology to chemical composition. IV. Titanium silicates: crystal chemistry of barytolamprophyllite
title_full From structure topology to chemical composition. IV. Titanium silicates: crystal chemistry of barytolamprophyllite
title_fullStr From structure topology to chemical composition. IV. Titanium silicates: crystal chemistry of barytolamprophyllite
title_full_unstemmed From structure topology to chemical composition. IV. Titanium silicates: crystal chemistry of barytolamprophyllite
title_sort from structure topology to chemical composition. iv. titanium silicates: crystal chemistry of barytolamprophyllite
publishDate 2008
url http://hdl.handle.net/2318/78502
https://doi.org/10.3749/canmin.46.2.403
http://www.canmin.org/content/46/2/403.abstract
genre kola peninsula
genre_facet kola peninsula
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000257188000009
volume:46
firstpage:403
lastpage:412
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journal:CANADIAN MINERALOGIST
http://hdl.handle.net/2318/78502
doi:10.3749/canmin.46.2.403
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-48249126467
http://www.canmin.org/content/46/2/403.abstract
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