Quantitative estimation of structural defects in silicate minerals by cathodoluminescence and its applications to earth and planetary science
Author:
Affiliation:
1. Graduate School of Science, Tohoku University, Frontier Research Institute for Interdisciplinary Sciences, Tohoku University
2. Present Address: Graduate School of Arts and Sciences, The University of Tokyo
Publisher
Japan Association of Mineralogical Sciences
Subject
Economic Geology,Geochemistry and Petrology
Link
https://www.jstage.jst.go.jp/article/gkk/48/2/48_190215/_pdf
Reference34 articles.
1. Boggs, Jr.S., Ktinsley, D.H., Goles, G.G., Setedolali, A. and Dypvik, H. (2001): Identification of shocked quartz by scanning cathodoluminescence imaging. Meteorit. Planet. Sci., 36, 783-791.
2. El Goresy, A., Chen, M., Gillet, P. and Dubrovinsky L.S. (2010): Shock-induced high-pressure phase-transition of labradorite to hollandite ‘(Na47-Ca51-K2)’ in Zagami and the assemblage hollandite ‘(Na80-Ca12-K8)’+ jadeite in L chondrites: Constraints to peak-shock pressures. Meteorit. Planet. Sci., 35, supplement, A51.
3. Finch, A. and Klein, J. (1999): The causes and petrological significance of cathodoluminescence emission from alkali feldspars. Contrib. Mineral. Petrol., 135, 234-243.
4. Fritz, J., Artemieva, N. and Greshake, A. (2005): Ejection of Martian meteorites, Meteorit. Planet. Sci., 40, 1393-1411.
5. Gaft, M., Reisfeld, R. and Panczer, G. (2005): Luminescence spectroscopy of minerals and materials. Springer Verlag 356.
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