Block Motion Changes in Japan Triggered by the 2011 Great Tohoku Earthquake [PDF]
, 2017 Plate motions are governed by equilibrium between basal and edge forces. Great earthquakes may induce differential static stress changes across tectonic plates, enabling a new equilibrium state.
Loveless, John P., Meade, Brendan J.
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Coseismic slip distribution of the 1946 Nankai earthquake and aseismic slips caused by the earthquake [PDF]
Earth, Planets and Space, 2014 Coseismic slip distribution on the fault plane of the 1946 Nankai earthquake (Mw 8.3) was estimated from inversion of tsunami waveforms. The following three improvements from the previous study (Satake, 1993) were made. (1) Larger number of smaller subfaults is used; (2) the subfaults fit better to the slab geometry; and (3) more detailed bathymetry ...
Tanioka, Yuichiro, Satake, Kenji
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Introduction to special section: Active Fault-Related Folding: Structural Evolution, Geomorphologic Expression, Paleoseismology, and Seismic Hazards [PDF]
, 2007 N/
Avouac, Jean-Philippe, Dolan, James F.
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New constraints on the uplift of October 9, 1995 Jalisco-Colima earthquake (Mw 8) based on the analysis of tsunami records at Manzanillo and Navidad, Mexico [PDF]
Geofísica Internacional, 2000 Tsunami records registered during the October 9, 1995 Jalisco-Colima earthquake (Mw 8) by two tide gauges and one pressure gauge are analyzed to estimate the coseismic subsidence at Manzanillo and Navidad Bay.
J. Pacheco +3 more
doaj
Progress in Earth and Planetary Science, 2022 The transition process from coseismic to early postseismic phenomena within a half-day remains a significant topic for understanding the slip budget and friction properties of the fault.
Yusuke Tanaka +2 more
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An aseismic slip pulse in northern Chile and along-strike variations in seismogenic behavior [PDF]
, 2006 We use interferometric synthetic aperture radar, GPS, and seismic observations spanning 5 to 18 years to reveal a detailed kinematic picture of the spatiotemporal evolution of fault slip in a region corresponding to the 30 July 1995 M_w 8.1 subduction ...
Pritchard, M. E., Simons, M.
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Diffuse deformation explains the magnitude-dependent coseismic shallow slip deficit
, 2023 Abstract Continental earthquakes produce both localized slip on faults and diffuse deformation in the surrounding medium, up to 1-2 kilometers from the faults. However, the origin of the diffuse deformation and its role in the rupture process are still debated.
Solene Antoine +3 more
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Earthquake rupture extents and coseismic slips promoted by damaged fault zones [PDF]
Journal of Geophysical Research: Solid Earth, 2016 AbstractHere we investigate the effects of damage fault zones on rupture propagation by conducting a series of 3‐D dynamic rupture simulations on a planar vertical strike‐slip fault. We find that damage fault zones can promote rupture extent and increase earthquake potency.
Huihui Weng +3 more
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Remote SensingOn 7 January 2025, an Mw 7.0 earthquake struck Dingri County, Shigatse, Tibet. This was the largest event in the region in recent years. Analysis of the Dingri earthquake is urgent for understanding the coseismic slip and early postseismic deformation ...
Di Liang +7 more
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Buried shallow fault slip from the South Napa earthquake revealed by near-field geodesy. [PDF]
, 2017 Earthquake-related fault slip in the upper hundreds of meters of Earths surface has remained largely unstudied because of challenges measuring deformation in the near field of a fault rupture.
Brooks, Benjamin +14 more
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