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

Figure 1. (a) The examples of TMA results.
Numbers on the plots are sample numbers: 24
and 38 are from the Khalats section, 399 and 402 are from the Kvirinaki section. Note a peak
related to transformation of pyrite to magnetite and hematite on the latter two.
(b) The examples of TMA results.
The 700-800oC interval TMA is highlighted
to illustrate the Curie temperatures of metallic iron for the same samples as Figure 1a.

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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