分光学と地質学の融合:光を通じて視る地球内部環境
Author:
Affiliation:
1. Graduate School of Environmental Studies, Nagoya University
Publisher
Japan Association of Mineralogical Sciences
Subject
Economic Geology,Geochemistry and Petrology
Link
https://www.jstage.jst.go.jp/article/gkk/52/1/52_230110a/_pdf
Reference39 articles.
1. Andò, S. and Garzanti, E. (2014): Raman spectroscopy in heavy-mineral studies. Geol. Soc., London, Spec. Pub., 386, 395-412.
2. Angel, R.J., Alvaro, M., Miletich, R. and Nestola, F. (2017a): A simple and eneralized P-T-V EoS for continuous phase transitions, implemented in EosFit and applied to quartz. Contrib. Mineral. Petrol., 172, 1-15.
3. Angel, R.J., Mazzucchelli, M.L., Alvaro, M. and Nestola, F. (2017b): EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry. Amer. Mineral., 102, 1957-1960.
4. Aoya, M., Kouketsu, Y., Endo, S., Shimizu, H., Mizukami, T., Nakamura, D. and Wallis, S. (2010): Extending the applicability of the Raman carbonaceous-material geothermometer using data from contact metamorphic rocks. J. Metamorph. Geol., 28, 895-914.
5. Beyssac, O., Bollinger, L., Avouac, J. and Goffe, B. (2004): Thermal metamorphism in the lesser Himalaya of Nepal determined from Raman spectroscopy of carbonaceous material. Earth Planet. Sci. Lett., 225, 233-241.
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1. An automatic peak deconvolution code for Raman spectra of carbonaceous material and a revised geothermometer for intermediate- to moderately high-grade metamorphism;Progress in Earth and Planetary Science;2024-06-25
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