Author Correction: Feedback between megathrust earthquake cycle and plate convergence. [PDF]
Martin de Blas J +3 more
europepmc +1 more source
An organizational capability framework for earthquake recovery
Engineering and construction capability affects the cost and pace of post-disaster recovery. An organizational capability framework for effective earthquake recovery was developed after studying longitudinally 15 engineering and construction ...
Chang-Richards, Alice +3 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
Subduction zone megathrust earthquakes [PDF]
Susan L. Bilek, Thorne Lay
openaire +1 more source
Generating tsunami risk knowledge at community level as a base for planning and implementation of risk reduction strategies [PDF]
More than 4 million Indonesians live in tsunami-prone areas along the southern and western coasts of Sumatra, Java and Bali. Although there now exists a Tsunami Early Warning Center in Jakarta, installed after the devastating 2004 tsunami, it is ...
K. Zosseder +16 more
core +3 more sources
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
Frictional behaviour of megathrust fault gouges under in-situ subduction zone conditions
Subduction zone megathrusts generate the largest earthquakes and tsunamis known. Understanding and modelling “seismogenesis” on such faults requires an understanding of the frictional processes that control nucleation and propagation of seismic slip ...
den Hartog, S.A.M.
core
Stress loading following a Mw7.8 megathrust earthquake in the northern Ecuadorian forearc
Whether driven by fluids or aseismic slip, seismic swarms release stress. In the Ecuadorian subduction zone, the 2016 Pedernales Mw7.8 megathrust earthquake caused aftershocks associated with afterslip.
Aracely Garcia +8 more
core +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

