Quantitative estimation of structural defects in silicate minerals by cathodoluminescence and its applications to earth and planetary science

Author:

KAYAMA Masahiro12

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

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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