THE CRYSTAL CHEMISTRY OF MALINKOITE, NaBSiO4, AND LISITSYNITE, KBSi2O6

The crystal structure of malinkoite, NaBSiO4, a 13.8964(4) Å, c 7.7001(2) Å, P63, Z = 18, Dx = 2.922 g cm–3, from the Khibina–Lovozero complex, Kola peninsula, Russia, has been solved by direct methods and refined to an R index of 3.8 % using 2094 unique observed (|Fo |> 4F) reflections collected...

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Main Authors: Elena V. Sokolova, Frank, C. Hawthorne, Alexander P. Khomyakov
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.3933
http://rruff.info/doclib/cm/vol39/CM39_159.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.486.3933 2023-05-15T17:05:02+02:00 THE CRYSTAL CHEMISTRY OF MALINKOITE, NaBSiO4, AND LISITSYNITE, KBSi2O6 Elena V. Sokolova Frank C. Hawthorne Alexander P. Khomyakov The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.3933 http://rruff.info/doclib/cm/vol39/CM39_159.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.3933 http://rruff.info/doclib/cm/vol39/CM39_159.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://rruff.info/doclib/cm/vol39/CM39_159.pdf text ftciteseerx 2016-01-08T08:12:54Z The crystal structure of malinkoite, NaBSiO4, a 13.8964(4) Å, c 7.7001(2) Å, P63, Z = 18, Dx = 2.922 g cm–3, from the Khibina–Lovozero complex, Kola peninsula, Russia, has been solved by direct methods and refined to an R index of 3.8 % using 2094 unique observed (|Fo |> 4F) reflections collected with a single-crystal diffractometer fitted with a CCD detector and MoK X-radiation. Malinkoite is a framework borosilicate with a structure consisting of six-membered rings of regularly alternating (SiO4) and (BO4) tetrahedra, and Na located in the large channels extending along [001]. There are three unique Si sites, each occupied by Si and each coordinated by four O atoms in a tetrahedral arrangement, with <Si–O> distances of 1.625, 1.622 and 1.622 Å, respectively. There are three unique B sites, each occupied by B and each coordinated by four O atoms in a tetrahedral arrangement, with distances of 1.476, 1.476 and 1.473 Å, respectively. There are five unique Na sites, each completely occupied by Na. Three of the Na sites are [9]-coordinated, with <Na–O> distances of 2.626, 2.642 and 2.630 Å, respectively; the remaining two Na sites are [6]-coordinated, with <Na–O> distances of 2.444 and 2.440 Å, respectively. The (SiO4) and (BO4) tetrahedra link to form six-membered rings of two different configurations based on the following sequences of up (U) and down (D) linkages: UDUDUD and UUDUDD in the ratio of 1:2. Nine-coordinated Na polyhedra are located in big cages formed by stacking of UDUDUD rings. Stacking of UUDUDD rings produces smaller cages occupied by [6]-coordinated Na. In accord with the ratio of two types of rings, there are twelve Na octahedra and six [9]-coordinated Na polyhedra per unit cell in malinkoite. The Text kola peninsula Unknown Kola Peninsula Lovozero ENVELOPE(35.016,35.016,68.006,68.006)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description The crystal structure of malinkoite, NaBSiO4, a 13.8964(4) Å, c 7.7001(2) Å, P63, Z = 18, Dx = 2.922 g cm–3, from the Khibina–Lovozero complex, Kola peninsula, Russia, has been solved by direct methods and refined to an R index of 3.8 % using 2094 unique observed (|Fo |> 4F) reflections collected with a single-crystal diffractometer fitted with a CCD detector and MoK X-radiation. Malinkoite is a framework borosilicate with a structure consisting of six-membered rings of regularly alternating (SiO4) and (BO4) tetrahedra, and Na located in the large channels extending along [001]. There are three unique Si sites, each occupied by Si and each coordinated by four O atoms in a tetrahedral arrangement, with <Si–O> distances of 1.625, 1.622 and 1.622 Å, respectively. There are three unique B sites, each occupied by B and each coordinated by four O atoms in a tetrahedral arrangement, with distances of 1.476, 1.476 and 1.473 Å, respectively. There are five unique Na sites, each completely occupied by Na. Three of the Na sites are [9]-coordinated, with <Na–O> distances of 2.626, 2.642 and 2.630 Å, respectively; the remaining two Na sites are [6]-coordinated, with <Na–O> distances of 2.444 and 2.440 Å, respectively. The (SiO4) and (BO4) tetrahedra link to form six-membered rings of two different configurations based on the following sequences of up (U) and down (D) linkages: UDUDUD and UUDUDD in the ratio of 1:2. Nine-coordinated Na polyhedra are located in big cages formed by stacking of UDUDUD rings. Stacking of UUDUDD rings produces smaller cages occupied by [6]-coordinated Na. In accord with the ratio of two types of rings, there are twelve Na octahedra and six [9]-coordinated Na polyhedra per unit cell in malinkoite. The
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Elena V. Sokolova
Frank
C. Hawthorne
Alexander P. Khomyakov
spellingShingle Elena V. Sokolova
Frank
C. Hawthorne
Alexander P. Khomyakov
THE CRYSTAL CHEMISTRY OF MALINKOITE, NaBSiO4, AND LISITSYNITE, KBSi2O6
author_facet Elena V. Sokolova
Frank
C. Hawthorne
Alexander P. Khomyakov
author_sort Elena V. Sokolova
title THE CRYSTAL CHEMISTRY OF MALINKOITE, NaBSiO4, AND LISITSYNITE, KBSi2O6
title_short THE CRYSTAL CHEMISTRY OF MALINKOITE, NaBSiO4, AND LISITSYNITE, KBSi2O6
title_full THE CRYSTAL CHEMISTRY OF MALINKOITE, NaBSiO4, AND LISITSYNITE, KBSi2O6
title_fullStr THE CRYSTAL CHEMISTRY OF MALINKOITE, NaBSiO4, AND LISITSYNITE, KBSi2O6
title_full_unstemmed THE CRYSTAL CHEMISTRY OF MALINKOITE, NaBSiO4, AND LISITSYNITE, KBSi2O6
title_sort crystal chemistry of malinkoite, nabsio4, and lisitsynite, kbsi2o6
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.3933
http://rruff.info/doclib/cm/vol39/CM39_159.pdf
long_lat ENVELOPE(35.016,35.016,68.006,68.006)
geographic Kola Peninsula
Lovozero
geographic_facet Kola Peninsula
Lovozero
genre kola peninsula
genre_facet kola peninsula
op_source http://rruff.info/doclib/cm/vol39/CM39_159.pdf
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http://rruff.info/doclib/cm/vol39/CM39_159.pdf
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