New data on S-bearing katoite from Tadano, Fukushima Prefecture, Japan: an implication of the presence of both (SO<sub>3</sub>)<sup>2−</sup> and (SO<sub>4</sub>)<sup>2−</sup> in the garnet structure
Author:
Affiliation:
1. Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST)
2. Department of Geology and Paleontology, National Museum of Nature and Science
3. The University Museum, The University of Tokyo
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/118/1/118_220724/_pdf
Reference26 articles.
1. Antao, S.M. (2015) Crystal chemistry of birefringent hydrogrossular. Physics and Chemistry of Minerals, 42, 455-474.
2. Banno, Y., Bunno, M. and Tsukimura, K. (2018) A reinvestigation of holotype wadalite from Tadano, Fukushima Prefecture, Japan. Mineralogical Magazine, 82, 1023-1031.
3. Cohen-Addad, C. (1970) Etude du composé Ca3Fe2(SiO4)1.15(OH)7.4 par absorption infrarouge et diffraction des rayons X et des neutrons. Acta Crystallographica, A27, 68-70.
4. Deer, W.A., Howie, R.A. and Zussman, J. (1997) Rock-forming minerals. 1A (second edition), Orthosilicates. pp. 919, The Geological Society, London.
5. Galuskin, E.V., Gazeev, V.M., Lazic, B., Armbruster, T., et al (2009) Chegemite Ca7(SiO4)3(OH)2 - a new humite-group calcium mineral from the Northern Caucasus, Kabardino-Balkaria, Russia. European Journal of Mineralogy, 21, 1045-1059.
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