RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES6004, doi:10.2205/2008ES000306, 2008

Figure 8. The correlation between the contents of metallic iron (Fe) and goethite (a),
metallic iron (Fe) and titanomagnetite+magnetite (TM+MT) (b), metallic iron (Fe) and
M800 (c),
and metallic iron (Fe) and the peaks on the
Mi(T) curves (d) in the Kvirinaki sediments.

Citation: Pechersky, D. M., D. K. Nurgaliev, and V. M. Trubikhin (2008), Native iron in Miocene sediments, Russ. J. Earth Sci., 10, ES6004, doi:10.2205/2008ES000306.
Copyright 2008 by the Russian Journal of Earth Sciences
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