The Penzhina-West Kamchatka folded zone and the Ukelayat-Sredinnyi block in the structure of the Koryak Highland and Kamchatka |
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| Authors: | S E Aprelkov S V Podpruzhenko |
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| Institution: | (1) Institute of Volcanology and Seismology, Far East Branch, Russian Academy of Sciences, Petropavlovsk-Kamchatskii, Russia;(2) The Regional Agency for Mineral Resources of the Kamchatka Region and the Koryak Autonomous Okrug, Ministry of Natural Resources, Petropavlovsk-Kamchatskii, Russia |
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| Abstract: | The regional tectonic structure is considered with characterizing the Penzhina-West Kamchatka folded zone as an intracontinental rift and the Ukelayat-Sredinnyi block as a separated part of the Omolon Massif. It is assumed that the Malka-Petropavlovsk (Nachiki) zone of transverse uplifts is a southern continuation of the Penzhina-West Kamchatka folded zone. |
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| Keywords: | geology deep structure tectonics Koryak Highland Kamchatka |
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