Results 111 to 120 of about 1,235 (207)
Back to full interseismic plate locking decades after the giant 1960 Chile earthquake
Great megathrust earthquakes arise from the sudden release of strain accumulated during centuries of interseismic plate convergence. Here, the authors reconstruct interseismic strain accumulation since the 1960 Chile earthquake, finding a transient ...
Daniel Melnick +8 more
doaj +1 more source
Author Correction: Feedback between megathrust earthquake cycle and plate convergence. [PDF]
Martin de Blas J +3 more
europepmc +1 more source
Characterizations of tsunami hazards along the Cascadia subduction zone hinge on uncertainties in megathrust rupture models used for simulating tsunami inundation.
Witter, RC +4 more
core +1 more source
Demand-supply balance of disaster medical care in Osaka City based on damage estimation for a Nankai Trough megathrust earthquake: A geographic information system-based analysis. [PDF]
Yamamoto H +4 more
europepmc +1 more source
Tectonic control on great earthquake periodicity in south-central Chile
Multi-millennial records of great megathrust earthquakes have highlighted differences in periodicity and recurrence behavior. Understanding tectonic processes responsible for these differences is relevant for fault mechanics and hazard models.
Diego Aedo +3 more
doaj +1 more source
Long aseismic slip duration of the 2006 Java tsunami earthquake based on GPS data
The Java earthquake occurred on July 17, 2006 with magnitude 7.8 associated to the subduction process of Indo-Australian plate and Sundaland block off southwestern coast of Java.
Rio Raharja +4 more
doaj +1 more source
Subduction zone megathrust earthquakes [PDF]
Susan L. Bilek, Thorne Lay
openaire +1 more source
Slow slip events (SSEs) release tectonic strain without causing sudden ground shaking. SSEs have been observed at many subduction zones, some dynamically triggered by stress changes due to the passage of seismic waves.
Guoli Li +3 more
doaj +1 more source
Unusually large tsunamis frequent a currently creeping part of the Aleutian megathrust
Current models used to assess earthquake and tsunami hazards are inadequate where creep dominates a subduction megathrust. Here we report geological evidence for large tsunamis, occurring on average every 300–340 years, near the source areas of the 1946 ...
Robert C. Witter +9 more
doaj +1 more source
Co-seismic uplift provides significant effects on rocky intertidal assemblages. However, previous studies mainly focused on analysing invertebrate assemblages before and after the uplift event and are conducted in the Pacific Ocean region.
Widyastuti, Ernawati +4 more
core +1 more source

