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Rock magnetic and petrographical–mineralogical studies of the dredged rocks from the submarine volcanoes of the Sea-of-Okhotsk slope within the northern part of the Kuril Island Arc

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Abstract

The rock magnetic properties of the samples of dredged rocks composing the submarine volcanic edifices within the Sea-of-Okhotsk slope of the northern part of the Kuril Island Arc are studied. The measurements of the standard rock magnetic parameters, thermomagnetic analysis, petrographical studies, and microprobe investigations have been carried out. The magnetization of the studied rocks is mainly carried by the pseudo-single domain and multidomain titanomagnetite and low-Ti titanomagnetite grains. The high values of the natural remanent magnetization are due to the pseudo-single-domain structure of the titanomagnetite grains, whereas the high values of magnetic susceptibility are associated with the high concentration of ferrimagnetic grains. The highest Curie points are observed in the titanomagnetite grains of the igneous rocks composing the edifices of the Smirnov, Edelshtein, and 1.4 submarine volcanoes.

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Authors and Affiliations

  1. Institute of Volcanology and Seismology, Russian Academy of Sciences, bulv. Piip 9, 683006, Petropavlovsk-Kamchatskii, Russia

    V. A. Rashidov

  2. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, ul. B. Gruzinskaya 10, Moscow, 123995, Russia

    O. V. Pilipenko

  3. Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017, Russia

    V. V. Petrova

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  1. V. A. Rashidov
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  2. O. V. Pilipenko
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Original Russian Text © V.A. Rashidov, O.V. Pilipenko, V.V. Petrova, 2016, published in Fizika Zemli, 2016, No. 4, pp. 84–106.

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Rashidov, V.A., Pilipenko, O.V. & Petrova, V.V. Rock magnetic and petrographical–mineralogical studies of the dredged rocks from the submarine volcanoes of the Sea-of-Okhotsk slope within the northern part of the Kuril Island Arc. Izv., Phys. Solid Earth 52, 550–571 (2016). https://doi.org/10.1134/S1069351316040066

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