RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES1003, doi:10.2205/2015ES000547, 2015

Figure 1. Thermomagnetic curves showing the temperature dependencies of saturation magnetization (left-hand plots). $I_{s1}$ and $I_{s2}$ are the first and second heating, respectively. $I_{n}$ is the thermomagnetic curves of natural remanent magnetization. $I_{rt}$ is the thermomagnetic curves of thermal remanent magnetization (right-hand plots). For each curve, curves of its second derivative are shown, and the temperatures of kinks on the curves of natural remanent magnetization are presented. The values of $I_{s}$, $I_{n}$, and $I_{rt}$ are in $10^3$ A/m.

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Citation: Popov K. V., B. A. Bazylev, V. P. Shcherbakov, V. A. Tsel'movich, N. N. Kononkova (2015), Thermomagnetic analysis of ultramafic rocks: A case study of dunite from the Pekul'ney Complex, Chukotka, NE Russia, Russ. J. Earth Sci., 15, ES1003, doi:10.2205/2015ES000547.
 

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