Shkatulkalite, a Rare Mineral from the Lovozero Massif, Kola Peninsula: A Re-Investigation

The crystal structure of shkatulkalite has been solved from the crystal from the Lovozero alkaline massif, Kola Peninsula, Russia. The mineral is monoclinic, P2/m, a = 5.4638(19), b = 7.161(3), c = 15.573(6) Å, β = 95.750(9)°, V = 606.3(4) Å3, R1 = 0.080 for 1551...

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Main Authors: Andrey A. Zolotarev, Ekaterina A. Selivanova, Sergey V. Krivovichev, Yevgeny E. Savchenko, Taras L. Panikorovskii, Lyudmila M. Lyalina, Leonid A. Pautov, Victor N. Yakovenchuk
Format: Article
Language:English
Published: MDPI AG 2018-07-01
Series:Minerals
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Online Access:http://www.mdpi.com/2075-163X/8/7/303
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author Andrey A. Zolotarev
Ekaterina A. Selivanova
Sergey V. Krivovichev
Yevgeny E. Savchenko
Taras L. Panikorovskii
Lyudmila M. Lyalina
Leonid A. Pautov
Victor N. Yakovenchuk
author_facet Andrey A. Zolotarev
Ekaterina A. Selivanova
Sergey V. Krivovichev
Yevgeny E. Savchenko
Taras L. Panikorovskii
Lyudmila M. Lyalina
Leonid A. Pautov
Victor N. Yakovenchuk
author_sort Andrey A. Zolotarev
collection DOAJ
description The crystal structure of shkatulkalite has been solved from the crystal from the Lovozero alkaline massif, Kola Peninsula, Russia. The mineral is monoclinic, P2/m, a = 5.4638(19), b = 7.161(3), c = 15.573(6) Å, β = 95.750(9)°, V = 606.3(4) Å3, R1 = 0.080 for 1551 unique observed reflections. The crystal structure is based upon the HOH blocks consisting of one octahedral (O) sheet sandwiched between two heteropolyhedral (H) sheets. The blocks are parallel to the (001) plane and are separated from each other by the interlayer space occupied by Na1 atoms and H2O groups. The Na2, Na3, and Ti sites are located within the O sheet. The general formula of shkatulkalite can be written as Na5(Nb1−xTix)2(Ti1−yMn2+y)[Si2O7]2O2(OH)2·nH2O, where x + y = 0.5 and x ≈ y ≈ 0.25 for the sample studied. Shkatulkalite belongs to the seidozerite supergroup and is a member of the lamprophyllite group. The species most closely related to shkatulkalite are vuonnemite and epistolite. The close structural relations and the reported observations of pseudomorphs of shkatulkalite after vuonnemite suggest that, at least in some environments, shkatulkalite may form as a transformation mineral species.
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spelling doaj.art-98d108d940bd4d8abc969e2bb8fc2ee12022-12-22T02:55:58ZengMDPI AGMinerals2075-163X2018-07-018730310.3390/min8070303min8070303Shkatulkalite, a Rare Mineral from the Lovozero Massif, Kola Peninsula: A Re-InvestigationAndrey A. Zolotarev0Ekaterina A. Selivanova1Sergey V. Krivovichev2Yevgeny E. Savchenko3Taras L. Panikorovskii4Lyudmila M. Lyalina5Leonid A. Pautov6Victor N. Yakovenchuk7Department of Crystallography, Institute of Earth Sciences, Saint Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, RussiaGeological Institute, Kola Science Centre, Russian Academy of Sciences, Fersmana 14, 184209 Apatity, RussiaDepartment of Crystallography, Institute of Earth Sciences, Saint Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, RussiaGeological Institute, Kola Science Centre, Russian Academy of Sciences, Fersmana 14, 184209 Apatity, RussiaDepartment of Crystallography, Institute of Earth Sciences, Saint Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, RussiaGeological Institute, Kola Science Centre, Russian Academy of Sciences, Fersmana 14, 184209 Apatity, RussiaFersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Av. 18/2, 115162 Moscow, RussiaGeological Institute, Kola Science Centre, Russian Academy of Sciences, Fersmana 14, 184209 Apatity, RussiaThe crystal structure of shkatulkalite has been solved from the crystal from the Lovozero alkaline massif, Kola Peninsula, Russia. The mineral is monoclinic, P2/m, a = 5.4638(19), b = 7.161(3), c = 15.573(6) Å, β = 95.750(9)°, V = 606.3(4) Å3, R1 = 0.080 for 1551 unique observed reflections. The crystal structure is based upon the HOH blocks consisting of one octahedral (O) sheet sandwiched between two heteropolyhedral (H) sheets. The blocks are parallel to the (001) plane and are separated from each other by the interlayer space occupied by Na1 atoms and H2O groups. The Na2, Na3, and Ti sites are located within the O sheet. The general formula of shkatulkalite can be written as Na5(Nb1−xTix)2(Ti1−yMn2+y)[Si2O7]2O2(OH)2·nH2O, where x + y = 0.5 and x ≈ y ≈ 0.25 for the sample studied. Shkatulkalite belongs to the seidozerite supergroup and is a member of the lamprophyllite group. The species most closely related to shkatulkalite are vuonnemite and epistolite. The close structural relations and the reported observations of pseudomorphs of shkatulkalite after vuonnemite suggest that, at least in some environments, shkatulkalite may form as a transformation mineral species.http://www.mdpi.com/2075-163X/8/7/303shkatulkalitetitanosilicatecrystal structureKola PeninsulaLovozero alkaline massiftransformation mineral speciesvuonnemitetitaniumniobium
spellingShingle Andrey A. Zolotarev
Ekaterina A. Selivanova
Sergey V. Krivovichev
Yevgeny E. Savchenko
Taras L. Panikorovskii
Lyudmila M. Lyalina
Leonid A. Pautov
Victor N. Yakovenchuk
Shkatulkalite, a Rare Mineral from the Lovozero Massif, Kola Peninsula: A Re-Investigation
Minerals
shkatulkalite
titanosilicate
crystal structure
Kola Peninsula
Lovozero alkaline massif
transformation mineral species
vuonnemite
titanium
niobium
title Shkatulkalite, a Rare Mineral from the Lovozero Massif, Kola Peninsula: A Re-Investigation
title_full Shkatulkalite, a Rare Mineral from the Lovozero Massif, Kola Peninsula: A Re-Investigation
title_fullStr Shkatulkalite, a Rare Mineral from the Lovozero Massif, Kola Peninsula: A Re-Investigation
title_full_unstemmed Shkatulkalite, a Rare Mineral from the Lovozero Massif, Kola Peninsula: A Re-Investigation
title_short Shkatulkalite, a Rare Mineral from the Lovozero Massif, Kola Peninsula: A Re-Investigation
title_sort shkatulkalite a rare mineral from the lovozero massif kola peninsula a re investigation
topic shkatulkalite
titanosilicate
crystal structure
Kola Peninsula
Lovozero alkaline massif
transformation mineral species
vuonnemite
titanium
niobium
url http://www.mdpi.com/2075-163X/8/7/303
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