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Collision of the Kronotskiy arc at the NE Eurasia margin and structural evolution of the Kamchatka–Aleutian junction

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Abstract

Structural evolution of the Kamchatka–Aleutian junction area in late Mesozoic and Tertiary was generally controlled by (1) the processes of subduction in Kronotskiy and Proto-Kamchatka subduction zones and (2) collision of the Kronotskiy arc against NE Eurasia margin. Two structural zones of the pre-Pliocene age and six structural assemblages are recognized in studied region. 1: Eastern ranges zone comprises SE-vergent thrust folded belt, which evolved in accretionary and collisional setting. Two structural assemblages (ER1 and ER2), developed there, document shortening in the NW–SE direction and in the N–S direction, respectively. 2: Eastern Peninsulas zone generally corresponds to Kronotskiy arc terrane. Four structural assemblages are recognized in this zone. They characterize (1) precollisional deformations in the accretionary wedge (EP1) and in the fore-arc basin and volcanic belt (EP2), and (2) syn-collisional deformation of the entire Kronotskiy terrane in plunging folds (EP3) and deformations in the foreland basin (EP4). Analysis of paleomagnetic declinations versus present day structural strike in the Kronotskiy arc terrane shows that originally the arc was trending from west to east. Relative position of the accretionary wedge, fore-arc basin and volcanic belt, as well as northward dipping thrusts in accretionary wedge indicate, that a northward dipping subduction zone was located south of the arc. The accretionary wedge developed from the Late Cretaceous through the Eocene, and it implies that the subduction zone maintained its direction and position during this time. It implies that Kronotskiy arc was neither a part of the Pacific nor Kula plates and was located on an individual smaller plate, which included the arc and Vetlovka back-arc basin. Motion of the Kronotskiy arc towards Eurasia was connected only with NW-directed subduction at Kamchatka margin since Middle Eocene (42–44 Ma). Emplacement of the Kronotskiy arc at the Kamchatka margin occurred between Late Eocene and Early Miocene. This is based on the age of syn-collisional plunging folds in Kronotskiy terrane, and provenance data for the Upper Eocene to Middle Miocene Tyushevka basin, which indicate in situ evolution of the basin with respect to Kamchatka. Collision was controlled by the common motion of the Kronotskiy arc with Pacific plate towards the northwest, and by the motion of the Eurasian margin towards the south. The latter motion was responsible for the southward deflection of the western part of the Kronotskiy arc (EP3 structures), and for oblique transpressional structures in the collisional belt (ER2 structures).

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Acknowledgements

The authors are grateful to Nikolay Seliverstov for his great help in organizing several field seasons in Kamchatka. This article benefited from discussions with Boris Baranov, John Garver, William Harbert, Elena Konstantinovskaia, Wolfgang Kramer, Alexander Lander, Nataliya Levashova, Onno Oncken, and Michail Shapiro. We thank Eric Geist for his review and constructive comments. The study was supported by German Science Foundation grant GA 511/2 and Russian Foundation for Basic Research grant 05-05-64158. The fieldworks and work on the manuscript were also generously supported by the GeoForschungsZentrum Potsdam.

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  1. P. P. Shirshov Institute of Oceanology, Moscow, Russia

    Dmitriy V. Alexeiev & Nikolay V. Tsukanov

  2. Federal Institute for Geosciences and Natural Resources, Hannover, Germany

    Christoph Gaedicke

  3. Friedrich-Schiller University Jena, Institute of Earth Sciences, Jena, Germany

    Ralf Freitag

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  1. Dmitriy V. Alexeiev
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Alexeiev, D.V., Gaedicke, C., Tsukanov, N.V. et al. Collision of the Kronotskiy arc at the NE Eurasia margin and structural evolution of the Kamchatka–Aleutian junction. Int J Earth Sci (Geol Rundsch) 95, 977–993 (2006). https://doi.org/10.1007/s00531-006-0080-z

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