RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES1003, doi:10.2205/2015ES000547, 2015
| Sample | $I_{n}$, | $\chi, 10^{-3}$ | Q | $I_{rs}/I_{s}$ | $I_{s}$, | $I_{rs}$, | $H_{c}$, | $H_{rc}$, | $H_{rc}/H_{c}$ | $T_{c}(I_{s}$), | $I_{st}/I_{so}$ | $C$, |
| A/m | SI units | $10^3$ A/m | $10^3$ A/m | mT | mT | ° C | vol % | |||||
| NP06-20/1 | 18.4 | 67.3 | 7.0 | 0.09 | 5.7 | 0.53 | 7.1 | 17.8 | 2.5 | 595 | 0.44 | 1.26 |
| NP06-51/2 | 4.5 | 57.7 | 1.98 | 0.08 | 3.26 | 0.24 | 5.8 | 16.4 | 2.8 | 590 | 0.60 | 0.72 |
| NP06-32/1 | 2.6 | 88.0 | 0.75 | 0.19 | 4.4 | 0.82 | 12.0 | 24.3 | 2.0 | 590 | 0.45 | 0.97 |
| NP06-26/2 | 0.9 | 70.4 | 0.03 | 0.16 | 4.34 | 0.69 | 11.7 | 22.6 | 1.9 | 595 | 0.45 | 0.96 |
| NP06-54/2 | 3.9 | 110. | 0.9 | 0.10 | 8.96 | 0.93 | 7.2 | 15.8 | 2.18 | 600 | 0.45 | 1.99 |
| NP06-43/4 | 21.0 | 49.0 | 10.9 | 0.14 | 4.65 | 0.64 | 9.6 | 18.5 | 1.92 | 600 | 0.46 | 1.03 |
| NP06-54/3 | 1.6 | 20.1 | 2.1 | 0.12 | 1.10 | 0.13 | 7.6 | 16.0 | 2.11 | 595 | 0.39 | 0.24 |
| NP06-57/2 | 1.4 | 32.6 | 1.1 | 0.13 | 4.38 | 0.58 | 9.4 | 20.8 | 2.22 | 600 | 0.61 | 0.97 |
| NP06-20/2 | 135 | 109. | 31.5 | 0.11 | 11.26 | 1.27 | 7.9 | 18.4 | 2.33 | 595 | 0.63 | 2.50 |
| NP06-23/3 | 0.34 | 37.9 | 0.2 | 0.13 | 3.59 | 0.48 | 9.6 | 20.3 | 2.12 | 600 | 0.59 | 0.79 |
| NP06-46/2 | 4.6 | 49.2 | 2.4 | 0.16 | 4.41 | 0.71 | 11.2 | 20.6 | 1.83 | 595 | 0.52 | 0.98 |
| NP06-49/2 | 13.6 | 47.1 | 7.4 | 0.23 | 4.54 | 1.04 | 13.0 | 19.6 | 1.5 | 595 | 0.41 | 1.00 |
| NP06-53/2 | 7.8 | 58.4 | 3.1 | 0.13 | 4.7 | 0.58 | 8.6 | 18.3 | 2.14 | 595 | 0.50 | 1.04 |
| Note: $I_{n}$ – natural remanent magnetization; $\chi$ – magnetic susceptibility; $Q$ – Koenigsberger ratio; $I_{s}$ – saturation magnetization; $I_{rs}$ – remanent saturation magnetization; $H_{c}$ – coercive force; $H_{rc}$ – remanent coercive force; $T_{c}$ – Curie temperature for magnetite; $I_{st}/I_{so}$ – ratio of the saturation magnetization of the sample after its heating to 700° C to its initial saturation magnetization; $C$ – volumetric percentage of magnetite in the sample calculated from the saturation magnetization value $I_{s}$. | ||||||||||||
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.