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

Table 1. Sampling Sites of Rocks and Brief Characteristics of the Petrography of the Rocks and Spinel From Them
no. Sample Sampling site (block) DS Ol Cpx Spl FCr Mag
1 NP06-20/1 Central 55 + + – + +
2 NP06-51/2 Vodorazdel'nyi 100 – – + + +
3 NP06-32/1 Southern 50 + – – – +
4 NP06-26/2 Northern 60 + + – + +
5 NP06-54/2 Yanranskii 35 + + – + +
6 NP06-43/4 Central 85 + + + + +
7 NP06-54/3 Yanranskii 50 + + + + +
8 NP06-57/2 Krivorechenskii 55 + + + + +
9 NP06-20/2 Central 45 + + – – +
10 NP06-23/3 Central 55 + + – + +
11 NP06-46/2 Northern 65 + + + – +
12 NP06-49/2 Northern 50 + + + + +
13 NP06-53/2 Yanranskii 30 + + + + +
Note: DS is the degree of serpentinization in %, mineral symbols: Ol – olivine, Cpx – clinopyroxene, Spl – primary Cr-spinel, FCr – metamorphic Cr-spinel (ferrite-chromite), Mag – magnetite; signs "+" and "–" denote presence and absence, respectively, in a rock.

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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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