RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES1003, doi:10.2205/2015ES000547, 2015
Figure 2. Histogram of kink temperatures on the thermomagnetic curves of the natural remanent magnetization $I_{n}(T)$ of our samples (based on data in Table 4); $n$ is the number of kinks. Arrows show the temperature ranges of the metamorphic recrystallization of the dunite calculated from the composition of its metamorphic Cr-spinel.
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.
Copyright 2015 by the Geophysical Center RAS.
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