Results 191 to 200 of about 3,598 (283)
Abstract Earthflows are landslides in fine‐grained materials that alternate long dormant phases of very slow movement with short paroxysmal stages of rapid motion. These rapid phases are highly destructive, often causing severe damage to buildings and infrastructure.
M. Berti +11 more
wiley +1 more source
Abstract This study proposes a deep‐learning–based regional earthquake early warning model, the Taiwan Transformer Shaking Alert Model (TT‐SAM). The model adopts peak ground velocity (PGV) as its primary ground shaking prediction unit, aiming to better reflect actual structural damage and thereby enhance the practical utility and accuracy of the ...
Yu‐Heng Chen +3 more
wiley +1 more source
Structured generative modelling of earthquake response spectra with hierarchical latent variables in hyperbolic geometry. [PDF]
Wright A, Fayaz J.
europepmc +1 more source
Abstract Debris flows over riverbeds generate intense basal force fluctuations that radiate seismic signals, offering a key tool for remotely monitoring their dynamics. In steep, highly erosive mountainous channels, bedrock is often covered by a thin layer of loose sediments, which significantly reduce seismic energy.
Bo Pang +4 more
wiley +1 more source
Study on the distribution characteristics and seismic hazard evaluation of loess seismic landslides in the southern Ningxia area. [PDF]
Yang S +5 more
europepmc +1 more source
Abstract Assessing seismic and tsunami hazards along coastlines requires understanding past earthquakes and their recurrence along active submarine faults. Subaqueous paleoseismology commonly relies on sediment cores and seismic reflection data, but these methods may be limited by local site conditions or data quality.
Frédérique Leclerc +7 more
wiley +1 more source
A hybrid quantitative approach for assessment of geotechnical hazards in rock tunnels using finite element and variation coefficient methods. [PDF]
Ghorbani S.
europepmc +1 more source
Subduction Parameters Controlling the Occurrence of Shallow and Deep Slow‐Slip Events (SSEs)
Abstract Slow‐slip events (SSEs) are transient aseismic fault‐slip phenomena that release tectonic stresses in a variety of tectonic environments, including subduction zones. In subduction margins, SSEs commonly occur along the plate interface at shallow (<20 km) and deep (30–60 km) depths.
Mario Arroyo‐Solórzano +4 more
wiley +1 more source
Fuzzy C-Means clustering and LSTM-based magnitude prediction of earthquakes in the Aegean region of Türkiye. [PDF]
Aloraini B +3 more
europepmc +1 more source
Two‐Layer Anisotropy Beneath Subduction Zones: Bayesian Inversion
Abstract Shear‐wave splitting measurements have the potential to constrain multiple layers of anisotropy and thereby enhance depth resolution. Using the formulation of Silver and Savage (1994, https://doi.org/10.1111/j.1365‐246x.1994.tb04027.x), previous studies have employed deterministic grid‐search approaches to identify best‐fitting two‐layer ...
Cheng‐Chien Peng +2 more
wiley +1 more source

