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

2008ES000306-fig10.html
Figure 10. The comparison of the intervals of elevated concentrations of metallic iron particles for the Khalats (a) and Kvirinaki (b) sections on the expanded scale. Black horizontal dashed lines denote the boundaries of the metallic iron content of ge 0.001%; red horizontal solid lines stand for the boundaries of the C5Ar and C5An magnetic chrons.

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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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