Results 101 to 110 of about 1,251 (185)
The shallow portion of megathrusts can exhibit various modes of failure: interseismic creep, triggered afterslip, or rupture during a tsunami(genic) earthquake, resulting in a potential hidden danger to onshore communities.
Qiang Qiu +5 more
doaj +1 more source
Coseismic Rupture and Postseismic Afterslip of the 2020 Nima Mw 6.4 Earthquake
On 22 July 2020, an Mw 6.4 earthquake occurred in Nima County in the Qiangtang Terrane of the central Tibetan Plateau. This event, caused by normal faulting, remains controversial in terms of its rupture process and causative fault due to the complex ...
Shaojun Wang, Ling Bai, Chaoya Liu
doaj +1 more source
Post-Seismic Deformation Related to the 2016 Central Italy Seismic Sequence From GPS Displacement Time-Series. [PDF]
Mandler E +5 more
europepmc +1 more source
International audienceWhen analyzing the rupture of a large earthquake, geodetic data are often critical. Yet, these data are generally characterized by either a good temporal (continuous GNSS) or a good spatial (InSAR and subpixel image correlation ...
Bletery, Q. +5 more
core +2 more sources
Triggering an unexpected earthquake in an uncoupled subduction zone. [PDF]
Herman MW, Furlong KP.
europepmc +1 more source
Variation in the thermal and dehydration regime below Central America: Insights for the seismogenic plate interface. [PDF]
Qu R +8 more
europepmc +1 more source
Shallow creep along strike‐slip faults is essential in releasing strain during earthquake cycles. However, its origin—whether inherent or triggered by earthquakes—remains debated. Using Interferometric Synthetic Aperture Radar phase‐gradient data, we map
Ziming Liu +3 more
doaj +1 more source
Post-seismic deformation mechanism of the July 2015 MW 6.5 Pishan earthquake revealed by Sentinel-1A InSAR observation. [PDF]
Wang S +5 more
europepmc +1 more source
Analysis of postseismic processes : afterslip, viscoelastic relaxation and aftershocks
Der Erdbebenzyklus ist in der Regel in drei Phasen unterteilt: die interseismische, die koseismische und die postseismische Phase. Der Großteil der interseismisch akkumulierten Spannung wird durch das Hauptbeben und die postseismischen Prozesse abgebaut.
openaire +1 more source
Afterslip following the 2023 Mw7.8 and Mw7.6 Kahramanmaraş earthquakes: observations and modeling
On February 6, 2023, two earthquakes of magnitude Mw7.8 and Mw7.6 struck in South Türkiye. The first mainshock occurred along the East Anatolian fault, at the boundary between the Anatolian and Arabian plates, and was followed 9 hours later by a second ...
Romain Jolivet +6 more
core +1 more source

