Results 71 to 80 of about 2,593,108 (178)
In the context of increasing evidence of plate interface coupling variability in subduction zones, there is a need to extend the short time window given by instrumental data and to gather data over multiple time and spatial scales.
J. Weil‐Accardo +8 more
doaj +1 more source
Abstract Active faults exhibit complex geometric features, with rupture processes controlled by the coupled effects of tectonic loading, fault geometry, and internal displacement heterogeneity. To elucidate the interrelationship between long‐term deformation, stress redistribution, and rupture evolution, we constructed a three‐dimensional numerical ...
X. F. Guo, Y. Aoki, J. H. Li
wiley +1 more source
We represent the active deformation of the Aegean region with an elastic‐kinematic block model composed of a finite number of rotating crustal blocks whose boundaries coincide with major active structures. A total of 832 GPS velocities and 146 earthquake
K. Chousianitis +4 more
semanticscholar +1 more source
The seismic hazard related to megathrust earthquakes in the Ryukyus (southern Japan) is poorly constrained as no large earthquake has been reported there.
S. Debaecker +11 more
doaj +1 more source
Abstract We present heat flow estimates beneath the forearc slopes off Hyuga‐nada and Cape Muroto in the Nankai Trough, where the Philippine Sea plate subducts beneath the southwestern Japan. Using seismic reflection data, we identified Bottom Simulating Reflectors and derived heat flow ranging from 20 to >140 mW/m2.
Masataka Kinoshita +4 more
wiley +1 more source
The Hellenic subduction system is the primary locus of Nubia‐Eurasia convergence, yet the distribution of strain accumulation along it is still debated.
K. Chousianitis +4 more
semanticscholar +1 more source
The Coupling Cloud: A community database of megathrust kinematic coupling models
Kinematic coupling models inverted from geodetic data are widely used to evaluate how slip deficit is distributed along subduction megathrusts during the interseismic period, and are central to earthquake and tsunami hazard assessment.
Bar Oryan +48 more
doaj +1 more source
Mapping Global GNSS Vertical Velocities to Solid Earth Figure Change
Abstract The Earth's figure evolves in response to glacial isostatic adjustment (GIA), surface‐mass redistribution, and rotational and mantle‐driven processes. While temporal changes in the geoid's flattening are monitored through low‐degree gravity field harmonics, the geometric response of the solid Earth can be assessed independently from GNSS ...
C. Kotsakis
wiley +1 more source
Replication Data for: Interseismic Megathrust Coupling at the Osa Peninsula, Costa Rica
This dataset includes input files used to conduct the inverse modeling and run synthetic tests in the manuscript "Interseismic Megathrust Coupling at the Osa Peninsula, Costa Rica" submitted to Journal of Geophysical Research: Solid ...
Hill, Emma +4 more
core +1 more source
Dynamically Triggered Changes of Plate Interface Coupling in Southern Cascadia [PDF]
In subduction zones, frictional locking on the subduction interface produces year-by-year surface deformation that is measurable with GPS. During the interseismic period of the earthquake cycle, lasting hundreds of years between major earthquakes, these ...
Charles Williams +9 more
core +1 more source

