Modern Luminescence Spectroscopy of Minerals and Materials
By M. Gaft, R. Reisfeld, G. Panczer. 2005
464 citations recorded by the source corpus.
Subfields: Artificial Intelligence, Geochemistry and Petrology, Mechanics of Materials
View Paper: https://www.semanticscholar.org/paper/aed9daeedaf8e63b01fd4d6ebc8989317b1928e4
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In Artificial Intelligence
In Mechanics of Materials
Citations in the corpus
- Detection of structurally bound hydroxyl in fluorapatite from Apollo Mare basalt 15058,128 using TOF-SIMS (2010, background): “The primary constituent that causes photoluminescence signals in fluorapatite from 3300–3500 cm–1 (645–654 nm) is Sm3+ (Gaft et al. 2005).”
- GRENVILLE SKARN TITANITE: POTENTIAL REFERENCE MATERIAL FOR SIMS U–Th–Pb ANALYSIS (2010, background): “Spectra are dominated by groups of emission bands of REE centers (for band assignment, see Gaft et al. 2005).”
- Filling-in of near-infrared solar lines by terrestrial fluorescence and other geophysical effects: simulations and space-based observations from SCIAMACHY and GOSAT (2012, unknown): “There are many types of minerals with impurities that luminesce when excited by UV and visible light (Gaft et al., 2005).”