Tectonic stress accumulation in the region of the Kuril–Kamchatka Island Arc system


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The time variations in the tidal response of the medium in 2011–2015 according to the measurements at the global seismographic network (GSN) in Kamchatka are considered. Based on the data from the horizontal pendulums recording the eastward tilts at the station, it is established that there was a linear growth in the tidal tilt amplitudes up to May 24, 2013 due to the changes in the elastic moduli caused by tectonic stress accumulation. The growth phase was followed by the decline in the tidal tilt amplitudes induced by the release of stresses after the Sea-of-Okhotsk earthquake.

Sobre autores

M. Molodenskii

Schmidt Institute of Physics of the Earth

Autor responsável pela correspondência
Email: molodenskiy@mail.ru
Rússia, Moscow, 123995

S. Molodenskii

Schmidt Institute of Physics of the Earth

Email: molodenskiy@mail.ru
Rússia, Moscow, 123995

T. Begitova

Faculty of Mechanics and Mathematics

Email: molodenskiy@mail.ru
Rússia, Moscow, 119992

A. Zagoskin

Faculty of Mechanics and Mathematics

Email: molodenskiy@mail.ru
Rússia, Moscow, 119992

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