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Modelling of earthquake swarms suggests magmatic fluids in the upper crust beneath the Eger Rift
Buyukakpinar, Pinar; Dahm, T.; Hainzl, S.; Isken, Marius Paul ...
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2025-12-14
Earthquake swarms are enigmatic seismic phenomena that occur across diverse tectonic settings, from volcanic to intraplate regions, and are often ass...
Signature of transition to supershear rupture speed in the coseismic off-fault damage zone
Jara, Jorge; Bruhat, Lucile; Thomas, Marion Y.; Antoine, Solène L. ...
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2025-12-12
Most earthquake ruptures propagate at speeds below the shear wave velocity within the crust, but in some rare cases, ruptures reach supershear speeds...
Seismic and Aseismic Fault Slip During the Initiation Phase of the 2017MW= 6.9 Valparaíso Earthquake
Caballero, Emmanuel; Chounet, Agnès; Duputel, Zacharie; Jara, Jorge ...
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2025-12-12
Transient deformation associated with foreshocks activity has been observed before large earthquakes, suggesting the occurrence of a detectable prese...
Rain and small earthquakes maintain a slow-moving landslide in a persistent critical state
Bontemps, Noélie; Lacroix, Pascal; Larose, Eric; Jara, Jorge ...
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2025-12-12
In tectonically active mountain belts, landslides contribute significantly to erosion. Statistical analysis of regional inventories of earthquake-tri...