We image seismic intrinsic (Qi-1) and scattering (Qs-1) attenuation in Long Valley caldera, California, by analyzing more than 1700 vertical-component waveforms from local earthquakes. Observed energy envelopes are fit to the diffusion model (data files) and seismic attenuation images (anomalies files) are produced using two-dimensional space-weighting functions.Funding provided by: National Science FoundationCrossref Funder Registry ID: http://dx.doi.org/10.13039/100000001Award Number: NSF-1521855 Hazard SEE
The 1989 earthquake swarm beneath Mammoth Mountain, near Long Valley, California, was unique for the...
The 1989 earthquake swarm beneath Mammoth Mountain, near Long Valley, California, was unique for the...
The 1994 Northridge mainshock and its aftershocks show a complex pattern of peak accelerations at st...
We image seismic intrinsic (Q−1i) and scattering (Q−1s) attenuations in Long Valley Caldera, Califor...
Unrest at Long Valley caldera, California has been attributed to magma recharge or the ascent of hyd...
In this work we present intrinsic and scattering seismic attenuation 2-D images of Stromboli Volcan...
Abstract Lateral variation in crustal attenuation of California is calculated by inverting 25,330 sy...
Accurately predicting the seismic wavefield is important for physics-based earthquake hazard studies...
the installation of an array of 18 seismic stations along a line crossing the Los Angeles basin from...
Seismic coda measurements retrieve parameters linked to the physical characteristics of rock volumes...
In this work, we present regional maps of the inverse intrinsic quality factor (Qi −1), the inverse ...
In this dissertation, I study two fundamental topics in seismology, tidal triggering of earthquakes ...
Abstract To better understand the connection between earthquake production and geothermal/magmatic s...
Abstract The decrease of microearthquake activity is a controversial possible precursor for mainshoc...
successfully employed to image certain types of features in young silicic caldera environments. Howe...
The 1989 earthquake swarm beneath Mammoth Mountain, near Long Valley, California, was unique for the...
The 1989 earthquake swarm beneath Mammoth Mountain, near Long Valley, California, was unique for the...
The 1994 Northridge mainshock and its aftershocks show a complex pattern of peak accelerations at st...
We image seismic intrinsic (Q−1i) and scattering (Q−1s) attenuations in Long Valley Caldera, Califor...
Unrest at Long Valley caldera, California has been attributed to magma recharge or the ascent of hyd...
In this work we present intrinsic and scattering seismic attenuation 2-D images of Stromboli Volcan...
Abstract Lateral variation in crustal attenuation of California is calculated by inverting 25,330 sy...
Accurately predicting the seismic wavefield is important for physics-based earthquake hazard studies...
the installation of an array of 18 seismic stations along a line crossing the Los Angeles basin from...
Seismic coda measurements retrieve parameters linked to the physical characteristics of rock volumes...
In this work, we present regional maps of the inverse intrinsic quality factor (Qi −1), the inverse ...
In this dissertation, I study two fundamental topics in seismology, tidal triggering of earthquakes ...
Abstract To better understand the connection between earthquake production and geothermal/magmatic s...
Abstract The decrease of microearthquake activity is a controversial possible precursor for mainshoc...
successfully employed to image certain types of features in young silicic caldera environments. Howe...
The 1989 earthquake swarm beneath Mammoth Mountain, near Long Valley, California, was unique for the...
The 1989 earthquake swarm beneath Mammoth Mountain, near Long Valley, California, was unique for the...
The 1994 Northridge mainshock and its aftershocks show a complex pattern of peak accelerations at st...