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

Table 4. Temperatures of Kinks on the Thermomagnetic Curves of our Samples
Sample Saturation
magnetization
curves		Natural remanent
magnetization
curves
$I_{s1}$ $I_{s2}$ $I_{n}$ $I_{rt}$
NP06-20/1 190
420
540 460
595 590 645 600
NP06-51/2 170
400
560
590 590 655 590
NP06-32/1 175
275
435
550 500
590 590 630 590
NP06-26/2 220
280
375
385 340 445
530 430 550 490
595 590 635 600
NP06-54/2 235
395 320 440
540 425 535? 500
600 595? 635 595
NP06-43/4 185
390 295 550 475
600 595? 670 600
NP06-54/3 140
400 300 540 470
595 595 640 600
NP06-57/2 265
415 400
560 530
600 600 635 580
NP06-20/2 250
460
555 500
595 595 630 595
NP06-23/3 265
385 320 415
540 470 560? 500
600 600 645 590
NP06-46/2 375 335 250
540 520 570? 485
595 595 655 595
NP06-49/2 255
400 375 420
520 485 570 480
595 595 640 590
NP06-53/2 400 300 260
535 470 540 500
595 595 630 600

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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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