Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, a group-III Ti-disilicate mineral from the Khibiny Alkaline Massif, Kola Peninsula, Russia: description and crystal structure
Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, is a Group-III TS-block mineral from the Kirovskii mine, Mount Kukisvumchorr, Khibiny alkaline massif, Kola Peninsula, Russia. The mineral occurs as transparent platy crystals 2–10 μm thick and up to 180 μm across. It is colorless to very pale tan, with a...
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ftunivtorino:oai:iris.unito.it:2318/155526 2023-10-29T02:37:41+01:00 Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, a group-III Ti-disilicate mineral from the Khibiny Alkaline Massif, Kola Peninsula, Russia: description and crystal structure CAMARA ARTIGAS, Fernando Sokolova E Abdu YA Hawthorne FC Cámara F Sokolova E Abdu YA Hawthorne FC 2014 STAMPA http://hdl.handle.net/2318/155526 https://doi.org/10.3749/canmin.1400043 http://www.canmin.org/ eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000350778700010 volume:52 issue:4 firstpage:745 lastpage:762 numberofpages:18 journal:CANADIAN MINERALOGIST http://hdl.handle.net/2318/155526 doi:10.3749/canmin.1400043 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84927558757 http://www.canmin.org/ info:eu-repo/semantics/closedAccess saamite new mineral Khibiny alkaline massif Kola Peninsula Russia crystal structure Group III Ti-disilicate TS block info:eu-repo/semantics/article 2014 ftunivtorino https://doi.org/10.3749/canmin.1400043 2023-10-03T22:22:04Z Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, is a Group-III TS-block mineral from the Kirovskii mine, Mount Kukisvumchorr, Khibiny alkaline massif, Kola Peninsula, Russia. The mineral occurs as transparent platy crystals 2–10 μm thick and up to 180 μm across. It is colorless to very pale tan, with a white streak and a vitreous luster. The mineral formed in a pegmatite as a result of hydrothermal activity. Associated minerals are natrolite, barytolamprophyllite, kazanskyite, nechelyustovite, hydroxylapatite, belovite-(La), belovite-(Ce), gaidonnayite, nenadkevichite, epididymite, apophyllite-(KF), and sphalerite. Saamite has perfect cleavage on {001}, uneven fracture and a Mohs hardness ca. 3. Its calculated density is 3.243 g/cm3. Saamite is biaxial positive with α 1.760, β 1.770, γ 1.795 (λ 589 nm), 2Vmeas. = 69(2)°, 2Vcalc. = 65°, with medium dispersion, r > v. It is nonpleochroic. Saamite is triclinic, space group PFormula , a 5.437(2), b 7.141(3), c 21.69(1) Å, α 92.97(1), β 96.07(1), γ 90.01(1)°, V 836.3(11) Å3. The strongest lines in the X-ray powder-diffraction pattern [d(Å)(I)(hkl)] are: 21.539(100)(001), 2.790(15)(122), 2.692(14)(008), 3.077(13)(007), 7.180(11)(003), 2.865(11)(1Formula 2), 1.785(9)(1Formula 4), 2.887(9)(Formula 22, 0Formula 7, 115), and 1.785(9)(0Formula 1, 1Formula 7, 040, Formula Formula 8, 230, 23Formula ). Chemical analysis by electron microprobe gave Nb2O5 12.24, TiO2 20.37, SiO2 29.07, Al2O3 0.08, FeO 0.32, MnO 5.87, MgO 0.04, BaO 11.31, SrO 2.51, CaO 1.76, K2O 0.77, Na2O 8.39, H2O 5.77, F 1.71, O = F −0.72, sum 99.49 wt.%; H2O was determined from structure refinement and its presence was confirmed by IR spectroscopy. The empirical formula based on 20 (O + F) atoms pfu is (Ba0.61Sr0.20K0.13□0.06)Σ1(□0.74Ca0.26)Σ1Formula (Ti2.09Nb0.76Mn0.13Mg0.01Al0.01)Σ3Si3.97O19.26H5.26F0.74, Z = 2. The simplified formula is as follows: Ba(□,Ca)Ti(Nb,Ti)(Na,Mn)3(Ti,Nb)(Si2O7)2O2(OH,F)2(H2O)2. The IR spectrum of saamite contains the following bands: ~1605, 1645, ~1747 and ~3420 cm−1. The crystal ... Article in Journal/Newspaper kola peninsula Università degli studi di Torino: AperTo (Archivio Istituzionale ad Accesso Aperto) The Canadian Mineralogist 52 4 745 762 |
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Università degli studi di Torino: AperTo (Archivio Istituzionale ad Accesso Aperto) |
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ftunivtorino |
language |
English |
topic |
saamite new mineral Khibiny alkaline massif Kola Peninsula Russia crystal structure Group III Ti-disilicate TS block |
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saamite new mineral Khibiny alkaline massif Kola Peninsula Russia crystal structure Group III Ti-disilicate TS block CAMARA ARTIGAS, Fernando Sokolova E Abdu YA Hawthorne FC Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, a group-III Ti-disilicate mineral from the Khibiny Alkaline Massif, Kola Peninsula, Russia: description and crystal structure |
topic_facet |
saamite new mineral Khibiny alkaline massif Kola Peninsula Russia crystal structure Group III Ti-disilicate TS block |
description |
Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, is a Group-III TS-block mineral from the Kirovskii mine, Mount Kukisvumchorr, Khibiny alkaline massif, Kola Peninsula, Russia. The mineral occurs as transparent platy crystals 2–10 μm thick and up to 180 μm across. It is colorless to very pale tan, with a white streak and a vitreous luster. The mineral formed in a pegmatite as a result of hydrothermal activity. Associated minerals are natrolite, barytolamprophyllite, kazanskyite, nechelyustovite, hydroxylapatite, belovite-(La), belovite-(Ce), gaidonnayite, nenadkevichite, epididymite, apophyllite-(KF), and sphalerite. Saamite has perfect cleavage on {001}, uneven fracture and a Mohs hardness ca. 3. Its calculated density is 3.243 g/cm3. Saamite is biaxial positive with α 1.760, β 1.770, γ 1.795 (λ 589 nm), 2Vmeas. = 69(2)°, 2Vcalc. = 65°, with medium dispersion, r > v. It is nonpleochroic. Saamite is triclinic, space group PFormula , a 5.437(2), b 7.141(3), c 21.69(1) Å, α 92.97(1), β 96.07(1), γ 90.01(1)°, V 836.3(11) Å3. The strongest lines in the X-ray powder-diffraction pattern [d(Å)(I)(hkl)] are: 21.539(100)(001), 2.790(15)(122), 2.692(14)(008), 3.077(13)(007), 7.180(11)(003), 2.865(11)(1Formula 2), 1.785(9)(1Formula 4), 2.887(9)(Formula 22, 0Formula 7, 115), and 1.785(9)(0Formula 1, 1Formula 7, 040, Formula Formula 8, 230, 23Formula ). Chemical analysis by electron microprobe gave Nb2O5 12.24, TiO2 20.37, SiO2 29.07, Al2O3 0.08, FeO 0.32, MnO 5.87, MgO 0.04, BaO 11.31, SrO 2.51, CaO 1.76, K2O 0.77, Na2O 8.39, H2O 5.77, F 1.71, O = F −0.72, sum 99.49 wt.%; H2O was determined from structure refinement and its presence was confirmed by IR spectroscopy. The empirical formula based on 20 (O + F) atoms pfu is (Ba0.61Sr0.20K0.13□0.06)Σ1(□0.74Ca0.26)Σ1Formula (Ti2.09Nb0.76Mn0.13Mg0.01Al0.01)Σ3Si3.97O19.26H5.26F0.74, Z = 2. The simplified formula is as follows: Ba(□,Ca)Ti(Nb,Ti)(Na,Mn)3(Ti,Nb)(Si2O7)2O2(OH,F)2(H2O)2. The IR spectrum of saamite contains the following bands: ~1605, 1645, ~1747 and ~3420 cm−1. The crystal ... |
author2 |
Cámara F Sokolova E Abdu YA Hawthorne FC |
format |
Article in Journal/Newspaper |
author |
CAMARA ARTIGAS, Fernando Sokolova E Abdu YA Hawthorne FC |
author_facet |
CAMARA ARTIGAS, Fernando Sokolova E Abdu YA Hawthorne FC |
author_sort |
CAMARA ARTIGAS, Fernando |
title |
Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, a group-III Ti-disilicate mineral from the Khibiny Alkaline Massif, Kola Peninsula, Russia: description and crystal structure |
title_short |
Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, a group-III Ti-disilicate mineral from the Khibiny Alkaline Massif, Kola Peninsula, Russia: description and crystal structure |
title_full |
Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, a group-III Ti-disilicate mineral from the Khibiny Alkaline Massif, Kola Peninsula, Russia: description and crystal structure |
title_fullStr |
Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, a group-III Ti-disilicate mineral from the Khibiny Alkaline Massif, Kola Peninsula, Russia: description and crystal structure |
title_full_unstemmed |
Saamite, Ba□TiNbNa3Ti(Si2O7)2O2(OH)2(H2O)2, a group-III Ti-disilicate mineral from the Khibiny Alkaline Massif, Kola Peninsula, Russia: description and crystal structure |
title_sort |
saamite, ba□tinbna3ti(si2o7)2o2(oh)2(h2o)2, a group-iii ti-disilicate mineral from the khibiny alkaline massif, kola peninsula, russia: description and crystal structure |
publishDate |
2014 |
url |
http://hdl.handle.net/2318/155526 https://doi.org/10.3749/canmin.1400043 http://www.canmin.org/ |
genre |
kola peninsula |
genre_facet |
kola peninsula |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/WOS:000350778700010 volume:52 issue:4 firstpage:745 lastpage:762 numberofpages:18 journal:CANADIAN MINERALOGIST http://hdl.handle.net/2318/155526 doi:10.3749/canmin.1400043 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84927558757 http://www.canmin.org/ |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.3749/canmin.1400043 |
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