Results 251 to 260 of about 168,552 (354)
Temporary Seismic Array Installation in the Contursi Terme Hydrothermal System: A Step Toward Geothermal Assessment. [PDF]
Serlenga V +13 more
europepmc +1 more source
Abstract Episodes of volcanic tremor provide valuable insights into the dynamics of subsurface processes at active volcanoes. Previous studies have suggested that evolving tremor properties may relate to changes in the stress conditions of the plumbing system. However, a strong causative link has remained elusive.
A. S. Yates +6 more
wiley +1 more source
A method for instrumental seismic intensity assessment in Western China based on RF and MLP. [PDF]
Yang S +6 more
europepmc +1 more source
SIMULATION OF HAZARD CONSISTENT ACCELEROGRAMS COMPATIBLE WITH TARGET UHS FOR SEISMIC RISK ASSESSMENT
Irmela Zentner
openalex +1 more source
Abstract The Sagaing Fault (SF) accommodates major plate motion in Myanmar, yet large earthquakes along it have rarely been captured by modern geodetic and seismic observations. The 2025 Sagaing earthquake generated an exceptionally long rupture (∼535 km), offering a rare opportunity to investigate rupture dynamics along continental transform fault. We
Zhenjiang Liu +8 more
wiley +1 more source
Seismicity characteristics based on the spatiotemporal ETAS model in North China from the perspective of different cut-off magnitude. [PDF]
Bi J, Cao F, Ma Y.
europepmc +1 more source
Abstract Subsurface heterogeneity influences watershed hydrology strongly but remains difficult to characterize at catchment scales with sparse and costly field data. Geophysical surveys such as electromagnetic induction (EMI) provide local spatial subsurface images yet scaling them to watershed scales and converting EMI‐derived resistivity into ...
Hang Chen +4 more
wiley +1 more source
A soil classification for seismic hazard assessment and mitigation of the Algarve
J. Carvalho +4 more
openalex +1 more source
Flow‐Dependent Inertial Permeability Defines Crossover Between Darcy and Forchheimer Flow Regimes
Abstract We present mechanistic evidence that the Forchheimer inertial permeability coefficient (β $\beta $) is flow‐dependent in the weak‐to‐intermediate inertia crossover regime, governed by pore‐scale eddy growth‐to‐confinement dynamics. In contrast to classical theory, β $\beta $ attains steady‐state (βs ${\beta }_{s}$) asymptotically in the ...
Kuldeep Singh, Negin Sharifabad
wiley +1 more source

