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X-Ray fluorescence analysis using synchrotron radiation of manganese minerals from marine and lake bottom sediments

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Bulletin of the Russian Academy of Sciences: Physics Aims and scope

Abstract

We perform X-ray fluorescence analysis of ferromanganese crusts from regions of the Okhotsk and Bering Seas and the Lake Miassovo (Southern Urals) with different geological structures using synchrotron radiation combined with X-ray diffraction and infrared spectroscopy (SR XRF). The consistency of the minor element composition to the structural patterns of manganese minerals of investigated samples is demonstrated.

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Authors and Affiliations

  1. Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, 630090, Russia

    T. N. Moroz, N. A. Palchik, A. V. Dar’in & T. N. Grigorieva

Authors
  1. T. N. Moroz
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  2. N. A. Palchik
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  3. A. V. Dar’in
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  4. T. N. Grigorieva
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Corresponding author

Correspondence to T. N. Moroz.

Additional information

Original Russian Text © T.N. Moroz, N.A. Palchik, A.V. Dar’in, T.N. Grigorieva, 2013, published in Izvestiya Rossiiskoi Akademii Nauk. Seriya Fizicheskaya, 2013, Vol. 77, No. 2, pp. 216–219.

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Moroz, T.N., Palchik, N.A., Dar’in, A.V. et al. X-Ray fluorescence analysis using synchrotron radiation of manganese minerals from marine and lake bottom sediments. Bull. Russ. Acad. Sci. Phys. 77, 195–198 (2013). https://doi.org/10.3103/S1062873813020238

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