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turkestanite

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Journal Article
Published: 19 January 2023
Mineralogical Magazine (2023) 87 (2): 252–261.
...Ekaterina Kaneva; Tatiana Radomskaya; Olga Belozerova; Roman Shendrik Abstract The results of combined single-crystal X-ray diffraction, electron probe microanalysis, Fourier microspectroscopy, and photoluminescence spectroscopy study of crystals of turkestanite from the Dara-i-Pioz deposit, Tien...
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Journal Article
Published: 01 August 2010
Mineralogical Magazine (2010) 74 (4): 645–658.
...F. C. J. Vilalva; S. R. F. Vlach Abstract Turkestanite, a rare Th- and REE -bearing cyclosilicate in the ekanite–steacyite group was found in evolved peralkaline granites from the Morro Redondo Complex, south Brazil. It occurs with quartz, alkali feldspar and an unnamed Y-bearing silicate. Electron...
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Published: 01 August 2010
F ig . 5. Cationic 2 B Na + + K + + REE 3 + vs . 3 Ca 2+ + □ diagrams for turkestanite. ( a ) Major coupled substitution mechanism operating in our turkestanite data set. ( b ) Selected analyses of turkestanite from Papanduva Pluton and turkestanite, steacyite and iraqite compositions
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Published: 01 August 2010
F ig . 3. BSE images of the turkestanite crystals of the evolved peralkaline granites from the Papanduva Pluton: ( a ) turkestanite crystal shown in Fig. 2 a with an homogeneous core and transformed and fractured rims. Note the thin irregular mantle formed by fluorite, aegirine and (Y-Ca
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Published: 19 January 2023
Fig. 6. Photoluminescence spectra of turkestanite (1) and steacyite (2) under 405 nm excitation. Excitation spectra of uranyl ions (UO 2 ) 2+ in turkestanite (3) and steacyite (4) monitored at 520 nm. All spectra were measured at 90 K.
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Published: 19 January 2023
Fig. 3. Photomicrographs in transmitted light (a, d, g), back-scattered electron images (b, e, h), and μFTIR mapping in reflection regime (c, f, i) of polished turkestanite grains. Aeg – aegirine, Apt – apatite, Btv – baratovite, Cal – calcite, Pl – plagioclase, Tkt – turkestanite, and Epoxy
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Published: 01 April 2018
Fig. 4. BSE images of agpaitic minerals in GR-III: ( a – b ) euhedral laths of nacareniobsite-(Ce) containing mineral inclusions. ( c – d ) zoned euhedral turkestanite containing mineral inclusions. The core of the turkestanite shows bright U-rich veinlets and inclusions. Abbreviations: amp
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Published: 19 January 2023
Fig. 5. The infrared spectrum of turkestanite.
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Published: 19 January 2023
Table 6. Unit cell parameters, polyhedral site populations, and X-ray and EPMA mean atomic numbers (electrons, e – ) for the turkestanite studied compared to those reported for turkestanite by Kabalov et al. ( 1998 ), isostructural steacyite (Richard and Perrault, 1972 ) and arapovite
Journal Article
Published: 01 July 2015
American Mineralogist (2015) 100 (7): 1378–1385.
..., rinkite, thorite, turkestanite, and vesuvianite). The total absorbed α-doses ranged from 1.4 × 10 15 to 6.1 × 10 18 α-decay mg −1 for cerite and uraninite, respectively. The 222 Rn emanation coefficients varied from 5 × 10 −5 % (uraninite) to 2.5% (turkestanite). The 220 Rn emanation coefficients varied...
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Journal Article
Published: 01 August 2004
The Canadian Mineralogist (2004) 42 (4): 1005–1011.
... in large cages within the framework. The topology of the arapovite structure is identical to that of turkestanite, Th (Ca,Na) 2 (K 1– x □ x ) Si 8 O 20 (H 2 O) n , and steacyite, Th (Na,Ca) 2 (K 1– x □ x ) Si 8 O 20 , x ≈ 0.5. The topology of silicate minerals with [Si 8 O 20 ]8–units, including ekanite...
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Journal Article
Published: 01 February 2004
The Canadian Mineralogist (2004) 42 (1): 107–119.
... of quartz with subordinate pectolite, aegirine, stillwellite-(Ce), polylithionite, leucosphenite and reedmergnerite. More rarely, turkestanite, galena, calcite, kapitsaite-(Y), neptunite, sugilite, baratovite, bismuth, sphalerite, fluorite, pyrochlore, fluorapatite, and zeravshanite occur in the same rock...
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Published: 19 January 2023
Fig. 1. (a) The crystal structure of turkestanite, and (b) silicate double four-membered rings contained in the unit cell. Si tetrahedra are blue; A (Th/U) and B (Ca/Na) polyhedra are green and yellow, respectively. O atoms are red, K atoms ( C sites) are drawn in grey. The partially white
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Published: 19 January 2023
Table 2. Average chemical composition (wt.%) for the turkestanite grains investigated compared with those reported previously. * * Notes: D-P – Dara-i-Pioz massif, Dzh – Dzhelisu massif, Ppnd – Papanduva Pluton; b.d.l. – below detection limit; n.d. – not determined; and '–' – not reported.
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Published: 19 January 2023
Fig. 4. Perspective view of the turkestanite crystal structure projected down to an a axis with an aperture of channel I (a), down to b axis with an aperture of channel II (b), and down to c axis with an aperture of channel III (c). Si atoms are blue; Th and U are green and cyan
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Published: 19 January 2023
Table 7. Bond-valence sums for the turkestanite studied, using the parameters suggested by Gagnè and Hawthorne ( 2015 ). The sums for the A and B sites with mixed occupancies were calculated using fractional site occupancies, obtained by SCXRD. [×4] , [×8] : for the calculation
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Published: 19 January 2023
Table 4. Crystallographic coordinates, occupancies, and equivalent/isotropic atomic displacement parameters (Å 2 ) for the turkestanite sample studied.
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Published: 01 April 2018
Table 3. Average compositions of nacareniobsite-(Ce) and turkestanite in pegmatitic agpaitic (GR-III) dykes. Mineral Nacareniobsite-(Ce) Turkestanite   ( Fig. 4 a – b )   Unaltered ( Fig. 4 b ) Altered core ( Fig. 4 c – d ) Rim surrounding altered core ( Fig. 4 c – d ) n
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Published: 01 August 2010
F ig . 2. Representative optical photomicrographies of turkestanite crystals of granites from the Papanduva Pluton: ( a ) turkestanite crystal (Trk) section close to (001), showing a light, clean core and dark turbid rims, between quartz (Qz) and an isotropic (Y- REE )-bearing hydrated silicate
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Published: 01 August 2010
F ig . 7. (Ce/Ce * ) vs . La N /Sm N diagram contrasting turkestanite of sample MR-02(2) with those of MR-02A and MR-140 samples.