Engineers frequently use simplified seismic slope displacement procedures to evaluate the performance of earth structures and natural slopes. Current practices typically adopt Newmark‐type and semi‐empirical seismic displacement prediction models (SDPMs) to estimate the seismic slope displacements (D) based on ground motion intensity measures at a ...
Ali Fallah Yeznabad +3 more
wiley +1 more source
Water budget in flat vs. steep subduction: implication for volcanism and potential for H2 production
In this study, we model the processes of (de)hydration and melting within subduction zones using a thermo-mechanical modeling approach. Multiple 2D simulations are conducted to investigate how the subduction angle influences the water budget in oceanic ...
Gauthier Alexis +3 more
doaj +1 more source
Fluid sources and overpressures within the central Cascadia Subduction Zone revealed by a warm, high-flux seafloor seep. [PDF]
Philip BT +7 more
europepmc +1 more source
The temporal distribution of aftershock sequences in the subduction zones of the Pacific [PDF]
Θεόδωρος Μ. Τσάπανος
openalex +1 more source
Regional‐to‐Global Tectonic and Trench‐Morphology Effects of Oceanic Plateau Subduction
Abstract Regional geodynamic modeling has shown that oceanic plateau subduction can modify the slab behavior. However, few studies have explored these interactions beyond 100 Myr in 3‐D spherical models. Using 3‐D spherical mantle convection models with self‐consistent plate‐like behavior, we investigate how the geometry and rheological properties of ...
Yang Liu +3 more
wiley +1 more source
Aseismic slip and recent ruptures of persistent asperities along the Alaska-Aleutian subduction zone. [PDF]
Zhao B +5 more
europepmc +1 more source
Holocene faulting in the Bellingham forearc basin: Upper‐plate deformation at the northern end of the Cascadia subduction zone [PDF]
Harvey M. Kelsey +3 more
openalex +1 more source
Abstract We investigate the spatiotemporal evolution of foreshocks preceding the 2025 Mw 8.8 Kamchatka earthquake by applying single‐station analysis to waveforms recorded at the nearest seismic station. Our results reveal a southwestward migration of foreshocks toward the mainshock epicenter through multiple stages, with a migration speed of ∼7.0 km ...
Ji Zhang +3 more
wiley +1 more source
Triggering an unexpected earthquake in an uncoupled subduction zone. [PDF]
Herman MW, Furlong KP.
europepmc +1 more source
Constraints from the dehydration of antigorite on high-conductivity anomalies in subduction zones [PDF]
Duojun Wang +5 more
openalex +1 more source

