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Paramagnetism of Rock-Forming Dolerite Minerals of Intraformational Trap Intrusions in West Yakutia as the Basis for Dolerite Correlation

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Abstract

This paper shows that the mineral composition of dolerites affects their specific paramagnetic susceptibility. Two methods for calculating the specific paramagnetic susceptibility were proposed: one used the thermomagnetic analysis (TMA) curve and the other the Mi(B) curve. There was no significant difference between the results obtained with these two approaches. Application of the proposed methods to dolerite core samples showed that specific paramagnetic susceptibility can be used as the basis for correlation of sills. The composition of titanomagnetites in dolerites can be used as an accessory parameter.

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Authors and Affiliations

  1. Institute of Geology and Petroleum Technologies, 420008, Kazan, Russia

    Sh. Z. Ibragimov, D. M. Kuzina & I. I. Nugmanov

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  1. Sh. Z. Ibragimov
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  2. D. M. Kuzina
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  3. I. I. Nugmanov
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Correspondence to Sh. Z. Ibragimov, D. M. Kuzina or I. I. Nugmanov.

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The study was financed by a subsidy allocated as part of the state support to Kazan (Volga Region) Federal University in order to improve its competitiveness among the world’s leading research and educational centers.

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Ibragimov, S.Z., Kuzina, D.M. & Nugmanov, I.I. Paramagnetism of Rock-Forming Dolerite Minerals of Intraformational Trap Intrusions in West Yakutia as the Basis for Dolerite Correlation. Izv., Phys. Solid Earth 56, 687–694 (2020). https://doi.org/10.1134/S1069351320050031

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