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Published/Copyright: December 30, 2019
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Experimental quantification of the Fe-valence state at amosite-asbestos boundaries using acSTEM dual-electron energy-loss spectroscopy by R. Vigliaturo, S. Pollastri, R. Gieré, A.F. Gualtieri, and G. Dražić (December, vol. 104, p. 1820–1828, 2019) Article DOI: https://doi.org/10.2138/am-2019-7218 Erratum DOI: https://doi.org/10.2138/am-2020-E105124

Chemical and textural relations of britholite- and apatite-group minerals from hydrothermal REE mineralization at the Rodeo de los Molles deposit, Central Argentina by M. Lorenz, U. Altenberger, R.B. Trumbull, R. Lira, M. López de Luchi, C. Günter, and S. Eidner (December, vol. 104, p. 1840–1850, 2019) Article DOI: https://doi.org/10.2138/am-2019-6969 Erratum DOI: https://doi.org/10.2138/am-2020-E105125

Table 3 in this article should appear as below. American Mineralogist regrets this error.

Table 3

ROI characteristics summary

Valence state
ROI thickness (nm)White-line intensity ratio (windows)Geometrical model(Pollastri 2015)XPS
Universal curve (2eV)2 eV4 eV8 eV1st2ndBulk (Mössbauer)
Short amosite Mean16.252.442.332.472.572.492.352.082.67
(7.69)(0.31)(0.38)(0.31)(0.25)(0.44)(0.48)(0.04)
Long amosite Mean25.302.192.012.162.172.212.15
(9.77)(0.05)(0.07)(0.19)(0.20)(0.10)(0.14)
  1. Note: Valence states obtained using progressively larger integrating windows for short and long amosite fibers, the standard deviation (σn–1) is given in parentheses.

Figure 5 in this article should appear as below. Additionally, two references were left out, and they are listed below. American Mineralogist regrets these errors.

Figure 5 Electron microprobe analyses of fluorbritholite-(Ce) and fluorapatite minerals from Rodeo de los Molles plottet on a classification diagram of apatite-supergroup minerals (after Pasero et al. 2010; Uher et al. 2015). The few points in the britholite field are from highly altered grains within the transition zone between the vein mineralization and the surrounding fenite (see Fig. 2b). INT1 and INT2 on the legend, for intergrowth type 1 and 2, see text. (Color online.)
Figure 5

Electron microprobe analyses of fluorbritholite-(Ce) and fluorapatite minerals from Rodeo de los Molles plottet on a classification diagram of apatite-supergroup minerals (after Pasero et al. 2010; Uher et al. 2015). The few points in the britholite field are from highly altered grains within the transition zone between the vein mineralization and the surrounding fenite (see Fig. 2b). INT1 and INT2 on the legend, for intergrowth type 1 and 2, see text. (Color online.)

References cited

Anenburg, M., Burnham, A.D., and Mavrogenes, J.A. (2018) REE redistribution textures in altered fluorapatite: Symplectites, veins, and phosphate-silicatecarbonate assemblages from the Nolans Bore P-REE-Th deposit, Northern Territory, Australia. The Canadian Mineralogist, 56(3), 331–354.10.3749/canmin.1700038Search in Google Scholar

Pandur, K., Ansdell, K.M., and Kontak, D.J. (2015) Graphic-textured inclusions in apatite: Evidence for pegmatitic growth in a REE-enriched carbonatitic system. Geology, 43(6), 547–550.10.1130/G36613.1Search in Google Scholar

Published Online: 2019-12-30
Published in Print: 2020-01-28

© 2020 Walter de Gruyter GmbH, Berlin/Boston

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