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Preseismic and coseismic deformation associated with the Coyote Lake, California, earthquake
Journal of Geophysical Research: Solid Earth, 1981Supplement is available with entire article on microfiche. Orderfrom American Geophysical Union, 2000 Florida Avenue, N.W.,Washington, D.C. 20006. Document J79‐008; $01.00. Payment mustaccompany order.The Coyote Lake earthquake (ML = 5.9; August 6, 1979; epicenter about 100 km southeast of San Francisco) occurred on the Calaveras fault within a ...
N. E. King +3 more
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The Vertical Coseismic Deformation Field of the Samos-Izmir Earthquake (Mw6.9)
2021<p>The Samos-Izmir Earthquake (Mw=6.9) of October 30, 2020 is among the strongest earthquakes that occurred in recent years throughout the Eastern Aegean. The epicenter of this earthquake was 14 km away from Samos Island and 25 km away from G&#252;m&#252;ld&#252;r-&#304;zmir region.
Muharrem Hilmi Erkoç +7 more
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3D Green's functions for coseismic and postseismic deformation
2018Finite fault slip inversions are constrained by observational data of surface displacement and Green's functions calculated via a forward model of surface deformation. Although observational techniques in space geodesy have improved greatly in recent years, models of earthquake deformation generally do not include realistic Earth structure. Many finite
Langer, L. +3 more
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Material point method for large deformation analyses of coseismic landslides
2023Estimation of coseismic landslides is of particular importance for seismic hazards assessment and mitigation strategies. To realitically and efficiently simulate the complete landslide process during earthquake from triggering to post-failure large movements, a robust computational tool is necessary.
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In subduction zones, seismic imaging reveals increasing permanent active deformation toward the trench, particularly within accretionary systems. Yet, how these rock bodies deform coseismically and influence megathrust rupture behavior is elusive.
Manel Prada +3 more
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Manel Prada +3 more
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Coseismic deformations in bottom sediments of lakes in Eastern Fennoscandia
Морские и озёрные бассейны восточной периферии Балтийского щита в четвертичное времяThe paper reviews of the available scattered information, as well as new data obtained in recent years on traces of Holocene earthquakes in lakes associated with active fault structures in the Karelia and Kola region. We present lithological-stratigraphical, paleobotanical, chronometrical data, as well as the results of geophysical studies (ground ...
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Coseismic river response to fault surface deformation.
The interaction between active tectonics and river morphodynamics is a core principle in tectonic and fluvial geomorphology. Despite the potential hazard implications, coseismic river response (CRR) remains largely unexplored and is often overlooked in earthquake multi-hazard assessments.openaire +1 more source
Inversion of ocean surface currents to obtain coseismic seafloor deformation.
During an earthquake, the coseismic deformation of the ocean floor is transmitted through the water column. If the earthquake’s energy is sufficiently large, it can uplift the ocean surface, and the subsequent collapse due to gravity leads to the propagation of waves as a tsunami.Rodrigo Cifuentes-Lobos +2 more
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DEVELOPING COSEISMIC DEFORMATION MODELS FOR GEODETIC APPLICATIONS
2019Figueroa, Mara A +5 more
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