Earthquakes and their secondary geological disasters have a certain impact on the land
cover, which leads to the degradation of the ecological environment and the stability of the …

Slow slip events (SSEs) and other forms of slow and transient fault slip are becoming
increasingly recognized as important, due to their influence on seismicity and potential to …

Deformation and fluid flow in subduction zone forearcs are dynamically coupled, but our
quantitative understanding of their coupling is incomplete. In this work, we investigate the …

Great subduction zone earthquakes vary considerably in the updip extent of megathrust
rupture. It is unclear if this diversity reflects variations in interseismic strain accumulation …

Abstract Preseismic, coseismic, and 7.5 years of postseismic deformation of the 2003 Mw
8.0 Tokachi‐oki earthquake are modeled using land Global Navigation Satellite System …

Slow earthquakes predominant in Costa Rica indicate unstable faulting of segmented
Central American megathrusts, but the recurrence of episodic tremors and slips reported to …

Ground shaking caused by earthquakes is accompanied by seafloor and sub‐seafloor
formation fluid pressure variations in offshore areas, but there have been few collocated …

Fractures and faults in igneous oceanic crust affect hydrothermal circulation and hydration of
the oceanic plates. Seismic observations have provided information about lithospheric …

The Cascadia subduction megathrust off the Pacific Northwest follows an “end member”
seismogenic behavior, producing large (up to moment magnitude 9) but infrequent (every …

How does deformation after an earthquake affect megathrust stresses? Five years of surface
velocities following the 2012 moment magnitude 7.6 Nicoya, Costa Rica earthquake …