Active Faults in the Kerch Peninsula: New Results


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This paper reports recently obtained research data on active faults in the Kerch Peninsula. The compiled Map of Active Faults demonstrates foci of Late Holocene strong earthquakes. This map is a regional seismotectonic model of strong earthquake foci, and a detailed basis for prediction of spatial seismic hazards. According to the research results, the Kerch Peninsula is characterized by the features of classical morphostructures, while the morphology of recent peninsula contours is caused by large active fault zones.

作者简介

A. Ovsyuchenko

Schmidt Institute of Physics of the Earth, Russian Academy of Sciences

Email: alsn@ifz.ru
俄罗斯联邦, Moscow, 123995

R. Vakarchuk

Schmidt Institute of Physics of the Earth, Russian Academy of Sciences

Email: alsn@ifz.ru
俄罗斯联邦, Moscow, 123995

A. Korzhenkov

Schmidt Institute of Physics of the Earth, Russian Academy of Sciences

Email: alsn@ifz.ru
俄罗斯联邦, Moscow, 123995

A. Larkov

Schmidt Institute of Physics of the Earth, Russian Academy of Sciences

Email: alsn@ifz.ru
俄罗斯联邦, Moscow, 123995

A. Sysolin

Schmidt Institute of Physics of the Earth, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: alsn@ifz.ru
俄罗斯联邦, Moscow, 123995

E. Rogozhin

Schmidt Institute of Physics of the Earth, Russian Academy of Sciences

Email: alsn@ifz.ru
俄罗斯联邦, Moscow, 123995

A. Marakhanov

Schmidt Institute of Physics of the Earth, Russian Academy of Sciences

Email: alsn@ifz.ru
俄罗斯联邦, Moscow, 123995

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