RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES3001, doi:10.2205/2006ES000204, 2006

Figure 18. Correlations between characteristics of coercivity spectra and
concentrations of magnetic minerals: (a, c, e) position of the first maximum
(mT); (b, d, f) relative height of a minimum; (a, b) magnetite+titanomagnetite;
(c, d) hemoilmenite; (e, f) goethite. The red squares and blue diamonds refer to
sandy-clayey deposits and limestones, respectively.

Citation: Pechersky, D. M., A. F. Grachev, D. K. Nourgaliev, V. A. Tsel'movich, and Z. V. Sharonova (2006), Magnetolithologic and Magnetomineralogical Characteristics of Deposits at the Mesozoic/Cenozoic Boundary: Gams Section (Austria), Russ. J. Earth Sci., 8, ES3001, doi:10.2205/2006ES000204.
Copyright 2006 by the Russian Journal of Earth Sciences
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