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

Figure 7. The correlation between the contents of goethite and
M800 (a),
titanomagnetite+magnetite (TM+MT) and
M800 (b), titanomagnetite+magnetite (TM+MT)
and goethite (c), goethite 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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