Publication details

The parisite-(Ce) enigma: challenges in the identification of fluorcarbonate minerals

Authors

ZEUG Manuela NASDALA Lutz ENDE Martin HABLER Gerlinde HAUZENBERGER Christoph CHANMUANG N. Chutimun ŠKODA Radek TOPA Dan WILDNER Manfred WIRTH Richard

Year of publication 2021
Type Article in Periodical
Magazine / Source Mineralogy and Petrology
MU Faculty or unit

Faculty of Science

Citation
Web https://doi.org/10.1007/s00710-020-00723-x
Doi http://dx.doi.org/10.1007/s00710-020-00723-x
Keywords Parisite-(Ce); Rontgenite-(Ce); Fluorcarbonate; Polycrystal; Raman spectroscopy; Stacking pattern
Description 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.

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