Compositional dependence of intensity tensor and electric field gradient tensor for Fe<sup>2+</sup> at <i>M</i>2 sites of enstatites by single crystal Mössbauer spectroscopy
Author:
Affiliation:
1. Graduate School of Science, Osaka Metropolitan University
2. Institute for Integrated Radiation and Nuclear Science, Kyoto University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/118/1/118_221015/_pdf
Reference14 articles.
1. Bancroft, G.M., Burns, R.G. and Stone, A.J. (1968) Applications of the Mössbauer effect to silicate mineralogy-II. Iron silicates of unknown and complex crystal structure. Geochimica et Cosmochimica Acta, 32, 547-559.
2. Cameron, M. and Papike, J.J. (1980) Crystal chemistry of silicate pyroxenes. In Pyroxenes (Prewitt, C.T. Ed.). pp. 525, Reviews in Mineralogy and Geochemistry, 7, Mineralogical Society of America, Washington D.C., 5-92.
3. Deer, W.A., Howie, R.A. and Zussman, J. (1978) Rock forming minerals. 2A, Single chain silicates. pp. 3, Longman, London.
4. Dowty, E. and Lindsley, D.H. (1973) Mössbauer spectra of synthetic hedenbergite-ferrosilite pyroxenes. American Mineralogist, 58, 850-868.
5. Dufek, P., Blaha, P. and Schwarz, K. (1995) Determination of the Nuclear Quadrupole Moment of 57Fe. Physical Review Letters, 75, 3545-3548.
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