RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES6006, doi:10.2205/2008ES000304, 2008

Figure 5. Correlation between paramagnetic magnetization (
Mp ) and concentration of
ferromagnetic Fe-hydroxides (goethite), magnetite, titanomagnetite, and metallic iron in
sediments. The data for the Gams, Koshak, Klyuchi, Teplovka, Tetritskaro, and Khalats sections
are combined
[Molostovsky et al., 2006;
Pechersky et al., 2006a, 2006b;
Pechersky, 2008];
(D. M. Pechersky et al., in press, 2008a,b).

Citation: Pechersky, D. M. (2008), Metallic iron in sediments at the Mesozoic-Cenozoic (K/T) boundary, Russ. J. Earth Sci., 10, ES6006, doi:10.2205/2008ES000304.
Copyright 2008 by the Russian Journal of Earth Sciences
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