Attenuated total reflection infrared (ATR–IR) spectroscopy of antigorite, chrysotile, and lizardite
Author:
Affiliation:
1. Graduate School of Environmental Studies, Nagoya University
2. Department of Earth and Planetary Environmental Science, the University of Tokyo
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/115/4/115_190807/_pdf
Reference35 articles.
1. Anbalagan, G., Sivakumar, G., Prabakaran, A.R. and Gunasekaran, S. (2010) Spectroscopic characterization of natural chrysotile. Vibrational Spectroscopy, 52(2), 122–127.
2. Bailey, S.W. and Banfield, J.F. (1995) Derivation and identification of nonstandard serpentine polytypes. American Mineralogist, 80, 1104–1115.
3. Balan, E., Saitta, A.M., Mauri, F., Lemaire, C. and Guyot, F. (2002a) First–principles calculation of the infrared spectrum of lizardite. American Mineralogist, 87, 1286–1290.
4. Balan, E., Mauri, F., Lemaire, C., Brouder, C., et al (2002b) Multiple Ionic–Plasmon Resonances in Naturally Occurring Multiwall Nanotubes: Infrared Spectra of Chrysotile Asbestos. Physical Review Letters, 89.
5. Balan, E., Delattre, S., Roche, D., Segalen, L., et al (2011) Line–broadening effects in the powder infrared spectrum of apatite. Physics and Chemistry of Minerals, 38, 111–122.
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