Results 161 to 170 of about 51,259 (279)
Cave reservoir characterization method driven by GA-KPCA and geological knowledge. [PDF]
Ren W, Chen H, Wang R, Zhang T, Li L.
europepmc +1 more source
Fault Volume Digital Twin to Reproduce the Full Slip Spectrum, Scaling, and Statistical Laws
Abstract Seismological and geodetic observations of fault zones reveal diverse slip dynamics, scaling, and statistical laws. Existing mechanisms explain some but not all of these behaviors. We show that incorporating an off‐fault damage zone—characterized by distributed fractures surrounding a main fault—can reproduce many key features observed in ...
M. Almakari +9 more
wiley +1 more source
Seismic reflectivity inversion with mixed L1-L2 norm regularization. [PDF]
Yang J, Dai R, Ma Y.
europepmc +1 more source
Abstract Eddy‐resolving numerical simulations are conducted to investigate the effects of density contrast between the confluent flows on hydrodynamics, coherent structures and mixing downstream of the confluence between the Negro and Solimões Rivers, Brazil, which is characterized by both a large discharge (>100,000 m3/s) and a large aspect‐ratio (W/D
C. Jiang +3 more
wiley +1 more source
Application of varied datum in time-to-depth conversion for high resolution coal seam micromorphology characterization. [PDF]
Zhang Q, Liu D, Chang S, Cai Y, Zhang S.
europepmc +1 more source
High resolution seismic profiles in Hood Canal and southern Puget Sound, Washington [PDF]
P. D. Snavely +5 more
openaire +1 more source
Abstract Submarine landslides occur globally and have the potential to damage seafloor infrastructure and trigger tsunamis. Recently, diatomaceous weak layers have been hypothesized to play a role in triggering submarine landslides on passive continental margins by generating overpressure.
Wyatt Scott, Julia S. Reece
wiley +1 more source
Extensive fluid overpressure in the shallow slow earthquake zone of Nankai Trough off Muroto mapped with high-resolution P-wave velocity. [PDF]
Flores PCM +5 more
europepmc +1 more source
Abstract Stishovite (SiO2), a key phase in subducted mid‐ocean ridge basalt (MORB), undergoes a ferroelastic transition to a CaCl2‐type structure, potentially explaining localized shear wave velocity (VS) anomalies in the shallow to mid‐lower mantle. However, the phase boundary determining this transition remains debated.
Ewa Krymarys +6 more
wiley +1 more source
Comprehensive assessment of ground motion amplification in stratified soils with different layer configurations and types. [PDF]
Ziar A, Basari E.
europepmc +1 more source

