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Pleistocene-Holocene Monogenetic Volcanism at the Malko-Petropavlovsk Zone of Transverse Dislocations on Kamchatka: Geochemical Features and Genesis

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Abstract

The Malko-Petropavlovsk zone of transverse dislocations (MPZ) was formed on the extension of the deep Avachinsky transform fault in perpendicular relation to the subduction trench. It is a natural boundary between variously aged slabs in Kamchatka (103–105 Ma under Southern Kamchatka and 87–92 Ma under the Eastern volcanic belt). Monogenetic cinder cones in the MPZ are randomly distributed along these long-lived rupture zones. Here we present new geochemical and isotopic results of monogenetic volcanism in the MPZ. Based on whole rock and trace element geochemistry, Pb-Sr-Nd isotopic ratios of monogenetic cinder cone magmas were shown to tap the enriched mantle source (low 143Nd/144Nd isotopic ratios (0.512959–0.512999), and changed  as 87Sr/86Sr (0.703356–0.703451) and 206Pb/204Pb (18.30–18.45), 208Pb/207Pb (38.00–38.12) isotopic ratios). High Nb/Yb and La/Yb ratios, without significant inputs of the slab’s components (the lowest Ba, Th content), indicate decompression melting predominately. Calculations of the pressure (9–11 kbar) and temperature (1160–1240 °C) conditions using a glass thermobarometer suggest that magma of monogenetic cinder cones resided near the Moho boundary prior to eruption. This correlates with the crustal discontinuity under the MPZ according to geophysical observations (converted-wave seismic exploration and magnetotelluric sounding). The majority of well-preserved monogenetic cinder cones were formed in Holocene, after the last glaciation, but eruptions were not observed historically. This, however, suggests that similar eruptions in the MPZ may occur in the future. Given that the MPZ hosts major population centres of Kamchatka (Petropavlovsk, Elizovo, Vilyuchinks, and Paratunka: ~ 250,000 people or ~ 80% of the whole Kamchatkan population live in the major cities on the coastline of the MPZ), we highlight the urgent need to install a continuous monitoring system around the MPZ cones, geophysical investigation, and more serious attention from the local government and scientists. In particular, a detailed study of the MPZ regarding age, volume, and volcanic hazard assessment (pyroclastic vs extrusive) will help reduce potential risks of eruptions from monogenetic volcanoes for humans and infrastructures.

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Availability of data and material

The list of monogenic cinder cones (Supplementary file 1), their geochemical and isotopic measurements (Supplementary 2), and demonstration of the genesis of the long-lived transform fault under the MPZ (Supplementary 3) are available in Bergal-Kuvikas et al. (2021), “Monogenetic volcanism at Malko-Petropavlovsk zone of the transverse dislocation (Kamchatka)”, Mendeley Data, V1, https://doi.org/10.17632/8d69jr8yjv.1https://data.mendeley.com/datasets/8d69jr8yjv/draft?a=33739679-5dee-4b10-9d3f-ded4d55e79b8

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Acknowledgements

Personal acknowledges are to Bazanova L.I., Dirksen O.V., Melekestsev I.V., Delemen I.F. for discussions and consultations of main structure of geological setting in MPZ. Thank you Kulish R., Uteshev I., Petrov O., Bergal V. for helping in organizations field works. We appreciated critical and constructive reviews by Nemeth K. Marti J. and Rabinovich A. for editorial handling.

Funding

We are thankful for the grant 19-17-00241 from the Russian Science Foundation for support of OB-K and IB, and the megagrant of the Ministry of Education and Science of the Russian Federation (no. 14.W03.31.0033) for support of fieldworks.

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Authors and Affiliations

  1. Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia, 683006

    Olga Bergal-Kuvikas & Olga Khubaeva

  2. Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry RAS, Moscow, Russia, 119017

    Olga Bergal-Kuvikas, Andrey Chugaev & Yulia Larionova

  3. Fersman Mineralogical Museum RAS, Moscow, Russia, 115162

    Olga Bergal-Kuvikas & Ilya Bindeman

  4. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences RAS, Moscow, Russia, 123242

    Olga Bergal-Kuvikas & Olga Khubaeva

  5. Department of Earth Sciences, 1272 University of Oregon, Eugene, OR, 97403, USA

    Ilya Bindeman

  6. Vinogradov Institute of Geochemistry SB RAS, Irkutsk, 664033, Russia

    Alexander Perepelov

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  1. Olga Bergal-Kuvikas
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Contributions

All authors contributed to the study conception and design. OB-K wrote the original draft. IB reviewed and edited the draft. CA prepared lead isotopes and improved interpretation of isotopic data. LY estimated Sr–Nd isotopic ratios. PA obtained trace element geochemistry. KO worked with geophysical data and organized fieldwork.

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Correspondence to Olga Bergal-Kuvikas.

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Bergal-Kuvikas, O., Bindeman, I., Chugaev, A. et al. Pleistocene-Holocene Monogenetic Volcanism at the Malko-Petropavlovsk Zone of Transverse Dislocations on Kamchatka: Geochemical Features and Genesis. Pure Appl. Geophys. 179, 3989–4011 (2022). https://doi.org/10.1007/s00024-022-02956-7

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