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Kaneva, Ekaterina, Bogdanov, Alexander, Radomskaya, Tatiana, Belozerova, Olga, Shendrik, Roman (2023) Crystal-chemical characterisation and spectroscopy of fluorcarletonite and carletonite. Mineralogical Magazine, 87 (3) 356-368 doi:10.1180/mgm.2023.15

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Reference TypeJournal (article/letter/editorial)
TitleCrystal-chemical characterisation and spectroscopy of fluorcarletonite and carletonite
JournalMineralogical Magazine
AuthorsKaneva, EkaterinaAuthor
Bogdanov, AlexanderAuthor
Radomskaya, TatianaAuthor
Belozerova, OlgaAuthor
Shendrik, RomanAuthor
Year2023 (June)Volume87
Page(s)356-368Issue3
PublisherMineralogical Society
DOIdoi:10.1180/mgm.2023.15Search in ResearchGate
Classification
Not set
LoC
Not set
Mindat Ref. ID16508526Long-form Identifiermindat:1:5:16508526:7
GUID26dce6d7-5e99-4524-b1a6-62061cd93c6d
Full ReferenceKaneva, Ekaterina, Bogdanov, Alexander, Radomskaya, Tatiana, Belozerova, Olga, Shendrik, Roman (2023) Crystal-chemical characterisation and spectroscopy of fluorcarletonite and carletonite. Mineralogical Magazine, 87 (3) 356-368 doi:10.1180/mgm.2023.15
Plain TextKaneva, Ekaterina, Bogdanov, Alexander, Radomskaya, Tatiana, Belozerova, Olga, Shendrik, Roman (2023) Crystal-chemical characterisation and spectroscopy of fluorcarletonite and carletonite. Mineralogical Magazine, 87 (3) 356-368 doi:10.1180/mgm.2023.15
In(2023, June) Mineralogical Magazine Vol. 87 (3) Mineralogical Society
Abstract/NotesThe minerals of carletonite group, fluorcarletonite, KNa4Ca4[Si8O18](CO3)4(F,OH)·H2O and carletonite, Na4Ca4[Si8O18](CO3)4(OH,F)·H2O, were investigated using a multi-method approach. A detailed comparative chemical study of the minerals was carried out using electron probe microanalysis and Fourier transform infrared spectroscopy. Using X-ray techniques and the results obtained, geometrical and distortion characteristics of the mineral structures are calculated and the successful crystal-structure refinement of these two natural compounds are given. Using spectroscopic and luminescence methods and ab initio calculations, it is shown that hole defects (CO3)•– are responsible for the colouration of the samples studied. Luminescence due to 5d–4f transition in Ce3+ ions is observed in both investigated compounds. Moreover, luminescence attributed to intrinsic luminescence, corresponding to the decay of electronic excitations of (CO3)2– complexes in the carletonite sample, is registered for the first time in phyllosilicates. An analysis of the optical absorption spectra and g-tensor values suggests that (CO3)•– defects in the crystal structure are localised in the C1 positions. Identification of these specific properties for these sheet silicates, with a two-dimensional infinite tetrahedral polymerisation, indicates that carletonites could be prospective materials for novel phosphors and luminophores.

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

()
Gagné (2015) Acta Crystallographica Comprehensive derivation of bond-valence parameters for ion pairs involving oxygen B71, 562
(2018) CrysAlisPro Software system, version 1.171.39.46
Wang (2020) Nature Communications Solar-blind ultraviolet-C persistent luminescence phosphors 11, 1
(2007) APEX2
Not Yet Imported: Open Ceramics - journal-article : 10.1016/j.oceram.2021.100150

If you would like this item imported into the Digital Library, please contact us quoting Journal ID
Neese (2012) Wiley Interdisciplinary Reviews: Computational Molecular Science The ORCA program system 2, 73
Chao (1972) American Mineralogist The crystal structure of carletonite, KNa4Ca4Si8O18(CO3)4(F,OH)⋅H2O, a double-sheet silicate 57, 765
Kasay (2021) Transactions of the Institute of Mining and Metallurgy B: Applied Earth Science A review of the geological settings, ages and economic potentials of carbonatites in the Democratic Republic of Congo 130, 143
Chao (1971) Hilaire, Quebec. American Mineralogist Carletonite, KNa4Ca4Si8O18(CO3)4(F,OH)⋅H2O, a new mineral from Mount St 56, 1855

Mineral Pages

MineralCitation Details
Carletonite
Fluorcarletonite


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