Results 161 to 170 of about 1,357,139 (273)
Comparison of coseismic velocity changes estimated by cross-correlation of ambient seismic noise for earthquakes in south Korea and Japan. [PDF]
Umer F, Chung TW, Iqbal MZ, Iqbal S.
europepmc +1 more source
Research on a Deep Learning‐Based Inversion Method for Surface Wave Dispersion Spectra
Abstract The near‐surface shear‐wave velocity structure is crucial for geological engineering and near‐surface exploration. Surface wave inversion is a key technique for obtaining the velocity structure, but traditional methods suffer from limitations such as heavy reliance on the initial model, high computational cost, and susceptibility to local ...
Yunwei Zhang, Yanyang Song, Xiaofei Chen
wiley +1 more source
Matrix imaging as a tool for high-resolution monitoring of deep volcanic plumbing systems with seismic noise. [PDF]
Giraudat E +5 more
europepmc +1 more source
Geophonino-W: A Wireless Multichannel Seismic Noise Recorder System for Array Measurements. [PDF]
Soler-Llorens JL +4 more
europepmc +1 more source
Adapting a Pretrained LLM to Rapidly Recover Earthquake Magnitude and Location
Abstract Determining earthquake magnitude and location through fast, automated methods is fundamental for seismic monitoring. Recent studies have shown that Large Language Models (LLMs) can operate as pattern‐recognition systems capable of handling novel domains and purely numerical tasks.
Aurora Bassani +6 more
wiley +1 more source
3-D intrinsic attenuation tomography using ambient seismic noise applied to La Palma Island (Canary Islands). [PDF]
Cabrera-Pérez I +9 more
europepmc +1 more source
ABSTRACT We developed a new experimental setup for measuring and modelling stress‐induced anisotropy and nonlinearity in cylindrical rock samples. Multidirectional ultrasonic velocity measurements were conducted under laboratory conditions and during triaxial‐stress testing to capture dynamic rock properties. This is done by placing endcap transducers (
Gabriel Gallardo‐Giozza +3 more
wiley +1 more source

