2021
The parisite-(Ce) enigma: challenges in the identification of fluorcarbonate minerals
ZEUG, Manuela, Lutz NASDALA, Martin ENDE, Gerlinde HABLER, Christoph HAUZENBERGER et. al.Základní údaje
Originální název
The parisite-(Ce) enigma: challenges in the identification of fluorcarbonate minerals
Autoři
ZEUG, Manuela, Lutz NASDALA, Martin ENDE, Gerlinde HABLER, Christoph HAUZENBERGER, N. Chutimun CHANMUANG, Radek ŠKODA (203 Česká republika, domácí), Dan TOPA, Manfred WILDNER a Richard WIRTH
Vydání
Mineralogy and Petrology, Wien, Springer Wien, 2021, 0930-0708
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10504 Mineralogy
Stát vydavatele
Rakousko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.011
Kód RIV
RIV/00216224:14310/21:00120913
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000578513600001
Klíčová slova anglicky
Parisite-(Ce); Rontgenite-(Ce); Fluorcarbonate; Polycrystal; Raman spectroscopy; Stacking pattern
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 18. 1. 2021 12:24, Mgr. Marie Šípková, DiS.
Anotace
V originále
A multi-methodological study was conducted in order to provide further insight into the structural and compositional complexity of rare earth element (REE) fluorcarbonates, with particular attention to their correct assignment to a mineral species. Polycrystals from La Pita Mine, Municipality de Maripi, Boyaca Department, Colombia, show syntaxic intergrowth of parisite-(Ce) with rontgenite-(Ce) and a phase which is assigned toB(3)S(4)(i.e., bastnasite-3-synchisite-4; still unnamed) fluorcarbonate. Transmission electron microscope (TEM) images reveal well-ordered stacking patterns of two monoclinic polytypes of parisite-(Ce) as well as heavily disordered layer sequences with varying lattice fringe spacings. The crystal structure refinement from single crystal X-ray diffraction data - impeded by twinning, complex stacking patterns, sequential and compositional faults - indicates that the dominant parisite-(Ce) polytypeM(1)has space groupCc. Parisite-(Ce), theB(3)S(4)phase and rontgenite-(Ce) show different BSE intensities from high to low. Raman spectroscopic analyses of parisite-(Ce), theB(3)S(4)phase and rontgenite-(Ce) reveal different intensity ratios of the three symmetric CO(3)stretching bands at around 1100 cm(-1). We propose to non-destructively differentiate parisite-(Ce) and rontgenite-(Ce) by their 1092 cm(-1)/ 1081 cm(-1)nu(1)(CO3) band height ratio.