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Volcanic Rocks in the Udyl’ Segment of the Kiselevka–Manoma Accretionary Terrane (Sikhote-Alin): Petrogeochemistry, Formation Conditions, and Tectonic Setting

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Abstract

New petrogeochemical data were used to determine the conditions of the formation and tectonic setting of volcanic rocks of the Lake Udyl’ area. These rocks were compared with similar rocks in the region. The volcanic rocks of the Lake Udyl’ area are subdivided into two genetic types: (1) within-plate oceanic volcanic rocks ascribed to the accretionary volcanogenic–siliceous complex (Tithonian–Valanginian–Hauterivian–Barremian) similar to accretionary complexes in other segments of the Kiselevka–Manoma Terrane, and (2) suprasubduction-zone volcanic rocks from the island-arc volcanogenic-terrigenous complex (Valanginian–Hauterivian–Aptian–Albian–Cenomanian). A synthesis of new geological and petrogeochemical data, as well as previous geochronological and paleomagnetic data indicates the co-occurrence of genetically diverse complexes in the Udyl’ segment.

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ACKNOWLEDGMENTS

We are grateful to reviewers Yu.A. Martynov and M.I. Tuchkova for comments and advice, which were taken into account in the final version of the manuscript. We thank N.V. Karetnikova for the technical preparation of the manuscript.

Funding

The studies were carried out in the framework of the government-financed research program of the Kosygin Institute of Tectonics and Geophysics of the Far East Branch, Russian Academy of Sciences, and was financially supported by the Russian Foundation for Basic Research (project no. 18-05- 00117А).

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Voinova, I.P., Didenko, A.N., Kudymov, A.V. et al. Volcanic Rocks in the Udyl’ Segment of the Kiselevka–Manoma Accretionary Terrane (Sikhote-Alin): Petrogeochemistry, Formation Conditions, and Tectonic Setting. Russ. J. of Pac. Geol. 14, 399–414 (2020). https://doi.org/10.1134/S1819714020050085

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