Publication Year: 2019
DOI: https://doi.org/10.1007/978-3-030-35906-5
Abstract: Not available
Authors:
Publication Year: 2012
DOI: https://doi.org/10.1016/j.tecto.2012.09.027
Abstract: Not available
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Publication Year: 2016
DOI: https://doi.org/10.1016/j.rgg.2016.03.003
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Publication Year: 2014
DOI: https://doi.org/10.1134/s0016852114040062
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Publication Year: 2014
DOI: https://doi.org/10.1134/s1069351314030057
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Publication Year: 2019
DOI: https://doi.org/10.1007/s00024-019-02128-0
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Publication Year: 2013
DOI: https://doi.org/10.3103/s0145875213010067
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Publication Year: 2008
DOI: https://doi.org/10.1134/s1028334x08090274
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Publication Year: 2017
DOI: https://doi.org/10.1134/s0016852117030086
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Publication Year: 2015
DOI: https://doi.org/10.1134/s1075701515010043
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DOI: https://doi.org/10.1016/j.rgg.2014.01.019
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Publication Year: 2009
DOI: https://doi.org/10.1134/s1069351309110111
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DOI: https://doi.org/10.1016/j.rgg.2008.01.004
Abstract: Not available
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Publication Year: 2022
DOI: https://doi.org/10.3390/app13010290
Abstract: In seismically Kamchatka causes of anomalous acoustic-deformation disturbance occurrences before strong earthquakes. The peninsula model is based on the assumption that the Earth’s crust refers, in the first approximation can be considered as a homogeneous pre-seismic isotropic elastic half-space, and an earthquake source can be considered anomalies as a displacements Show more
Authors:
Publication Year: 1988
DOI: https://doi.org/10.1016/0264-3707(88)90019-1
Abstract: Not available
Authors:
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