An XRD, TEM and Raman study of experimentally annealed natural monazite
By A. Seydoux‐Guillaume, Richard Wirth, L. Nasdala, M. Gottschalk, J. Montel, Wilhelm Heinrich. 2002
134 citations recorded by the source corpus.
Subfields: Condensed Matter Physics, Geophysics, Materials Chemistry
View Paper: https://www.semanticscholar.org/paper/d357fbcb7321adb6979aaa5b9dad448dd113a29a
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In Geophysics
In Materials Chemistry
Citations in the corpus
- GRENVILLE SKARN TITANITE: POTENTIAL REFERENCE MATERIAL FOR SIMS U–Th–Pb ANALYSIS (2010, background): “To give an example of the latter effect, Seydoux-Guillaume et al. (2002) determined the FWHM of the main internal phosphate band [n1(PO4) near 970 cm–1] of an annealed sample of natural monazite at ~7 cm–1, whereas the n1(PO4) FWHM of chemically pure monazite is ~2 cm–1 (Nasdala et al. 2010).”
- Annealing radiation damage and the recovery of cathodoluminescence (2002, methodology): “…a gradual regeneration of moderately metamict minerals upon heattreatment (e.g., Colombo et al., 1999a; Zhang et al., 2000b), the three little to moderately metamict samples K1, K2 (Nasdala et al., 2001b) and Moacir (Seydoux-Guillaume et al., 2002a) were found to recover gradually with temperature.”