KASATKIN, Anatoly V., Natalia V. ZUBKOVA, Igor V. PEKOV, Nikita V. CHUKANOV, Radek ŠKODA, Atali A. AGAKHANOV, Dmitriy I. BELAKOVSKIY, Dmitriy A. KSENOFONTOV, Jakub PLÁŠIL, Aleksey M. KUZNETSOV, Sergey N. BRITVIN a Dmitry Yu. PUSHCHAROVSKY. The mineralogy of the historical Mochalin Log REE deposit, South Urals, Russia. Part III. Percleveite-(La), La2Si2O7, a new REE disilicate mineral. Mineralogical Magazine. Cambridge University Press, 2020, roč. 84, č. 6, s. 913-920. ISSN 0026-461X. Dostupné z: https://dx.doi.org/10.1180/mgm.2020.81.
Další formáty:   BibTeX LaTeX RIS
Základní údaje
Originální název The mineralogy of the historical Mochalin Log REE deposit, South Urals, Russia. Part III. Percleveite-(La), La2Si2O7, a new REE disilicate mineral
Autoři KASATKIN, Anatoly V., Natalia V. ZUBKOVA, Igor V. PEKOV, Nikita V. CHUKANOV, Radek ŠKODA (203 Česká republika, domácí), Atali A. AGAKHANOV, Dmitriy I. BELAKOVSKIY, Dmitriy A. KSENOFONTOV, Jakub PLÁŠIL, Aleksey M. KUZNETSOV, Sergey N. BRITVIN a Dmitry Yu. PUSHCHAROVSKY.
Vydání Mineralogical Magazine, Cambridge University Press, 2020, 0026-461X.
Další údaje
Originální jazyk angličtina
Typ výsledku Článek v odborném periodiku
Obor 10504 Mineralogy
Stát vydavatele Velká Británie a Severní Irsko
Utajení není předmětem státního či obchodního tajemství
WWW URL
Impakt faktor Impact factor: 2.062
Kód RIV RIV/00216224:14310/20:00118034
Organizační jednotka Přírodovědecká fakulta
Doi http://dx.doi.org/10.1180/mgm.2020.81
UT WoS 000611934400011
Klíčová slova anglicky crystal structure; Mochalin Log; new mineral; percleveite-(La); Raman spectrum; rare-earth disilicate; South Urals
Štítky rivok
Příznaky Mezinárodní význam, Recenzováno
Změnil Změnila: Mgr. Marie Šípková, DiS., učo 437722. Změněno: 4. 2. 2021 10:53.
Anotace
The new mineral percleveite-(La) (IMA2019-037), ideally La2Si2O7, was found in polymineralic nodules of the Mochalin Log REE deposit, Chelyabinsk Oblast, South Urals, Russia. It is associated with allanite-(Ce), allanite-(La), bastnasite-(Ce), bastnasite-(La), ferriallanite-(Ce), ferriallanite-(La), ferriperbOeite-(Ce), ferriperbOeite-(La), fluorbritholite-(Ce), hydroxylbastnasite-(Ce), perbOeite-(Ce), perbOeite-(La), tornebohmite-(Ce) and tornebohmite-(La). Percleveite-(La) occurs as isolated anhedral grains commonly up to 0.2 mm x 0.4 mm and very rarely up to 1 mm x 1 mm. The new mineral is transparent with greasy lustre. The mineral is very pale yellow to colourless in thin fragments to light yellow in aggregates. It is brittle, with imperfect {001} cleavage and an uneven fracture. Mohs' hardness is ca. 6. D-calc = 5.094 g cm(-3). Under the microscope, percleveite-(La) is non-pleochroic, optically uniaxial (+), omega = 1.825(10) and = 1.835(10). The Raman spectrum is given. Chemical data (wt.%, electron-microprobe) are: La2O3 36.80, Ce2O3 31.22, Pr2O3 1.57, Nd2O3 2.96, SiO2 26.73, total 99.28. The empirical formula based on 7 O apfu is (La1.02Ce0.86Nd0.08Pr0.04)(Sigma 2.00)Si2.00O7. Percleveite-(La) is tetragonal, P4(1); the unit-cell parameters are: a = 6.8482(3), c = 24.8550(13) angstrom, V = 1165.64(11) angstrom(3) and Z = 8. The strongest reflections in the powder X-ray diffraction pattern [d, angstrom(I)(hkl)] are: 4.194(18)(113), 3.564(16)(106), 3.349(16)(201,202), 3.157(100)(203,116,008), 3.043(22)(211), 2.934(39)(122), 2.893(29)(213) and 2.864(21)(117). The crystal structure of percleveite-(La) is solved from the single-crystal X-ray diffraction data [R = 0.0617 for 2831 unique reflections with I > 2 sigma(I)]. The new mineral is named as an analogue of percleveite-(Ce) with La predominance over the rare-earth elements.
VytisknoutZobrazeno: 29. 7. 2024 08:01