Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
The mineralogy of the historical Mochalin Log REE deposit, South Urals, Russia. Part I. New gatelite-group minerals ferriperboeite-(La), (CaLa 3)(Fe 3+Al 2Fe 2+)[Si 2O 7][SiO 4] 3O(OH) 2and perboeite-(La), (CaLa 3)(Al 3Fe 2+)[Si 2O 7][SiO 4] 3O(OH) 2. / Kasatkin, Anatoly V.; Zubkova, Natalia V.; Pekov, Igor V.; Chukanov, Nikita V.; Škoda, Radek; Polekhovsky, Yury S.; Agakhanov, Atali A.; Belakovskiy, Dmitriy I.; Kuznetsov, Aleksey M.; Britvin, Sergey N.; Pushcharovsky, Dmitry Yu.
в: Mineralogical Magazine, Том 84, № 4, 01.08.2020, стр. 593-607.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - The mineralogy of the historical Mochalin Log REE deposit, South Urals, Russia. Part I. New gatelite-group minerals ferriperboeite-(La), (CaLa 3)(Fe 3+Al 2Fe 2+)[Si 2O 7][SiO 4] 3O(OH) 2and perboeite-(La), (CaLa 3)(Al 3Fe 2+)[Si 2O 7][SiO 4] 3O(OH) 2
AU - Kasatkin, Anatoly V.
AU - Zubkova, Natalia V.
AU - Pekov, Igor V.
AU - Chukanov, Nikita V.
AU - Škoda, Radek
AU - Polekhovsky, Yury S.
AU - Agakhanov, Atali A.
AU - Belakovskiy, Dmitriy I.
AU - Kuznetsov, Aleksey M.
AU - Britvin, Sergey N.
AU - Pushcharovsky, Dmitry Yu.
N1 - Funding Information: Acknowledgements. We are grateful to the Associate Editor Mike Rumsey for his thorough revision that substantially improved the manuscript. Henrik Friis and an anonymous reviewer, Structures Editor Peter Leverett and Principal Editor Stuart Mills are acknowledged for valuable comments. This study was supported by the Russian Foundation for Basic Research, grant no. 18-05-00332 (in part of XRD structure studies and crystal chemistry). This work was partly performed in accordance with the state task, state registration no. ААА-А19-119092390076-7 for N.V.C. The technical support by the SPbSU X-Ray Diffraction Resource Center in the powder XRD study is acknowledged.
PY - 2020/8/1
Y1 - 2020/8/1
N2 - The paper opens a series devoted to the mineral diversity of the Mochalin Log rare earth element (REE) deposit, South Urals, Russia. There is a brief outline of the history of studies and geology of the deposit as well as the description of two new isostructural gatelite-group minerals, ferriperboeite-(La) (CaLa3)(Fe3+Al2Fe2+)[Si2O7][SiO4]3O(OH)2 and perboeite-(La) (CaLa3)(Al3Fe2+)[Si2O7][SiO4]3O(OH)2. Both minerals occur in polymineralic nodules and are associated with one another and allanite-(Ce), allanite-(La), bastnäsite-(Ce), bastnäsite-(La), ferriallanite-(Ce), ferriallanite-(La), ferriperboeite-(Ce), perboeite-(Ce), törnebohmite-(Ce) and törnebohmite-(La). The new minerals form isolated anhedral grains up to 0.3 mm [ferriperboeite-(La)] and 0.5 mm [perboeite-(La)] across and granular aggregates up to 1.5 mm × 0.5 mm [ferriperboeite-(La)] and 3 mm × 1 mm [perboeite-(La)]. Both minerals are brownish-black with vitreous lustre. Dcalc = 4.510 [ferriperboeite-(La)] and 4.483 [perboeite-(La)] g cm-3. They are optically biaxial (+); ferriperboeite-(La): α = 1.788(5), β = 1.790(5), γ = 1.810(5) and 2Vmeas = 40(10)°; perboeite-(La): α = 1.778(8), β = 1.783(8), γ = 1.805(8) and 2Vmeas = 40(10)°. Chemical data [wt.%, electron-microprobe; Fe3+:Fe2+ ratio from charge-balance requirements, H2O by stoichiometry; ferriperboeite-(La)/perboeite-(La)] are: CaO 4.91/4.81, ThO2 0.00/0.32, La2O3 23.75/22.16, Ce2O3 19.69/20.05, Pr2O3 0.85/1.09, Nd2O3 1.48/2.18, MgO 1.47/1.38, Al2O3 10.68/11.25, MnO 1.07/0.92, FeO 3.04/3.35, Fe2O3 5.31/3.78, TiO2 0.19/0.19, SiO2 27.47/27.35, F 0.11/0.23, H2O 1.61/1.54, -O = F -0.05/-0.10, total 101.58/100.50. The empirical formulae based on O20(OH,F)2 are for ferriperboeite-(La): (Ca0.95La1.58Ce1.30Nd0.10Pr0.06)Σ3.99(Al2.27Fe3+0.72Fe2+0.46Mg0.40Mn0.16Ti0.03)Σ4.040Si4.96O20[(OH)1.94F0.06]; and for perboeite-(La): (Ca0.94Th0.01La1.49Ce1.34Nd0.14Pr0.07)Σ3.99(Al2.42Fe3+0.52Fe2+0.51Mg0.38Mn0.14 Ti0.03)Σ4.00Si4.99O20[(OH)1.87F0.13]. Both minerals are monoclinic, P21/m; the unit-cell parameters [ferriperboeite-(La)/perboeite-(La)] are: a = 8.9458(2)/8.9652(4), b = 5.72971(13)/5.7306(2), c = 17.6192(3)/17.6770(9) Å, β = 115.9497(19)/116.053(6)°, V = 812.06(3)/815.88(6) Å3 and Z = 2/2. The crystal structures are solved on a single crystal and converged to R = 0.0355 [ferriperboeite-(La)] and 0.0750 [perboeite-(La)]. Ferriperboeite-(La) and perboeite-(La) are named as the La-analogues of ferriperboeite-(Ce) and perboeite-(Ce), respectively.
AB - The paper opens a series devoted to the mineral diversity of the Mochalin Log rare earth element (REE) deposit, South Urals, Russia. There is a brief outline of the history of studies and geology of the deposit as well as the description of two new isostructural gatelite-group minerals, ferriperboeite-(La) (CaLa3)(Fe3+Al2Fe2+)[Si2O7][SiO4]3O(OH)2 and perboeite-(La) (CaLa3)(Al3Fe2+)[Si2O7][SiO4]3O(OH)2. Both minerals occur in polymineralic nodules and are associated with one another and allanite-(Ce), allanite-(La), bastnäsite-(Ce), bastnäsite-(La), ferriallanite-(Ce), ferriallanite-(La), ferriperboeite-(Ce), perboeite-(Ce), törnebohmite-(Ce) and törnebohmite-(La). The new minerals form isolated anhedral grains up to 0.3 mm [ferriperboeite-(La)] and 0.5 mm [perboeite-(La)] across and granular aggregates up to 1.5 mm × 0.5 mm [ferriperboeite-(La)] and 3 mm × 1 mm [perboeite-(La)]. Both minerals are brownish-black with vitreous lustre. Dcalc = 4.510 [ferriperboeite-(La)] and 4.483 [perboeite-(La)] g cm-3. They are optically biaxial (+); ferriperboeite-(La): α = 1.788(5), β = 1.790(5), γ = 1.810(5) and 2Vmeas = 40(10)°; perboeite-(La): α = 1.778(8), β = 1.783(8), γ = 1.805(8) and 2Vmeas = 40(10)°. Chemical data [wt.%, electron-microprobe; Fe3+:Fe2+ ratio from charge-balance requirements, H2O by stoichiometry; ferriperboeite-(La)/perboeite-(La)] are: CaO 4.91/4.81, ThO2 0.00/0.32, La2O3 23.75/22.16, Ce2O3 19.69/20.05, Pr2O3 0.85/1.09, Nd2O3 1.48/2.18, MgO 1.47/1.38, Al2O3 10.68/11.25, MnO 1.07/0.92, FeO 3.04/3.35, Fe2O3 5.31/3.78, TiO2 0.19/0.19, SiO2 27.47/27.35, F 0.11/0.23, H2O 1.61/1.54, -O = F -0.05/-0.10, total 101.58/100.50. The empirical formulae based on O20(OH,F)2 are for ferriperboeite-(La): (Ca0.95La1.58Ce1.30Nd0.10Pr0.06)Σ3.99(Al2.27Fe3+0.72Fe2+0.46Mg0.40Mn0.16Ti0.03)Σ4.040Si4.96O20[(OH)1.94F0.06]; and for perboeite-(La): (Ca0.94Th0.01La1.49Ce1.34Nd0.14Pr0.07)Σ3.99(Al2.42Fe3+0.52Fe2+0.51Mg0.38Mn0.14 Ti0.03)Σ4.00Si4.99O20[(OH)1.87F0.13]. Both minerals are monoclinic, P21/m; the unit-cell parameters [ferriperboeite-(La)/perboeite-(La)] are: a = 8.9458(2)/8.9652(4), b = 5.72971(13)/5.7306(2), c = 17.6192(3)/17.6770(9) Å, β = 115.9497(19)/116.053(6)°, V = 812.06(3)/815.88(6) Å3 and Z = 2/2. The crystal structures are solved on a single crystal and converged to R = 0.0355 [ferriperboeite-(La)] and 0.0750 [perboeite-(La)]. Ferriperboeite-(La) and perboeite-(La) are named as the La-analogues of ferriperboeite-(Ce) and perboeite-(Ce), respectively.
KW - Ferriperboeite-(La)
KW - Mochalin Log
KW - South Urals
KW - crystal structure
KW - gatelite group
KW - new mineral
KW - perboeite-(La)
KW - rare-earth silicate
UR - http://www.scopus.com/inward/record.url?scp=85091406486&partnerID=8YFLogxK
U2 - 10.1180/mgm.2020.42
DO - 10.1180/mgm.2020.42
M3 - Article
VL - 84
SP - 593
EP - 607
JO - Mineralogical Magazine
JF - Mineralogical Magazine
SN - 0026-461X
IS - 4
ER -
ID: 61265947