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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Original Russian Text © S.E. Aprelkov S.V. Podpruzhenko, 2009, published in Tikhookeanskaya Geologiya, 2009, Vol. 28, No. 4, pp. 90–104.
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Aprelkov, S.E., Podpruzhenko, S.V. The Penzhina-West Kamchatka folded zone and the Ukelayat-Sredinnyi block in the structure of the Koryak Highland and Kamchatka. Russ. J. of Pac. Geol. 3, 388–400 (2009). https://doi.org/10.1134/S181971400904006X
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DOI: https://doi.org/10.1134/S181971400904006X