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Tectonostratigraphic complexes of the southern Kronotskii paleoarc (Eastern Kamchatka): Structure,age, and composition |
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| Authors: | N V Tsukanov T N Palechek A V Soloviev D P Savelyev |
| Institution: | 1. Shirshov Institute of Oceanology, Russian Academy of Sciences, pr. Nakhimovskii 36, Moscow, 117997, Russia 2. Geological Institute, Russian Academy of Sciences, per. Pyzhevskii 7, Moscow, 119017, Russia 3. Institute of Volcanology and Seismology, Far East Branch, Russian Academy of Sciences, bul. Piipa 9, Petropavlovsk-Kamchatskii, 683006, Russia |
| Abstract: | The eastern peninsulas of Kamchatka are mostly composed of tectonostratigraphic complexes, which were formed within the Late Cretaceous-Eocene Kronotskii-Kamchatka arc. The accretion of this paleoarc to the Kamchatka margin of northeastern Asia in the terminal Cenozoic represented the last collisional event in the formation of the present-day structure of Kamchatka. The article presents new data on the age, composition, and structure of the tectonostratigraphic complexes constituting the southern segment of the Kronotskii-Kamchatka paleoarc. It is shown that the oldest rocks of these complexes are the Campanian in age and represented by volcano-sedimentary rocks that were formed in different geodynamic environments. The investigated igneous rocks are attributed to two types: (1) the tholeiite series of a mid-oceanic ridge (MOR) (Vetlovaya Complex); (2) tholeiite and calc-alkaline series of island arcs (Shipunskii Sequence of the Kronotskii Group). |
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