Scattering behaviour at Merapi volcano (Java) revealed from an active seismic experiment
U Wegler, BG Lühr - Geophysical Journal International, 2001 - academic.oup.com
The seismic structure of the stratovolcano Merapi (Java, Indonesia) was studied using an
active seismic experiment. Three 3km long seismic profiles each consisting of up to 30 three …
active seismic experiment. Three 3km long seismic profiles each consisting of up to 30 three …
Seismic wave scattering in volcanoes
E Del Pezzo - Advances in geophysics, 2008 - Elsevier
Volcano‐tectonic earthquakes produce high‐frequency seismograms characterized by
impulsive shear mechanism; their seismogram coda reflects the random inhomogeneity of …
impulsive shear mechanism; their seismogram coda reflects the random inhomogeneity of …
Attenuation of short-period seismic waves at Mt Vesuvius, Italy
We analysed short-period seismograms from about 250 very local events recorded by a
network of high dynamic range short-period seismic stations deployed on Mt Vesuvius to …
network of high dynamic range short-period seismic stations deployed on Mt Vesuvius to …
Hydrothermal fluids and where to find them: Using seismic attenuation and anisotropy to map fluids beneath Uturuncu volcano, Bolivia
Map** fluid accumulation in the crust is pertinent for numerous applications including
volcanic hazard assessment, geothermal energy generation, and mineral exploration. Here …
volcanic hazard assessment, geothermal energy generation, and mineral exploration. Here …
Global comparisons of earthquake source spectra
S Chen, GM Atkinson - Bulletin of the Seismological …, 2002 - pubs.geoscienceworld.org
A key question in earthquake seismology is whether earthquake sources in different tectonic
regions are functionally equivalent in terms of radiated ground motion. This article compares …
regions are functionally equivalent in terms of radiated ground motion. This article compares …
Separation of intrinsic and scattering attenuation in the crust of central and eastern Alborz region, Iran
In this study, more than 380 local earthquakes (2< ML< 4.5) have been used to estimate the
direct-shear waves (Q d), coda (Q c), intrinsic (Q i) and scattering quality factor (Q Sc) in the …
direct-shear waves (Q d), coda (Q c), intrinsic (Q i) and scattering quality factor (Q Sc) in the …
Frequency-dependent attenuation of body and coda waves in the Andaman Sea Basin
We estimated frequency-dependent attenuation of coda waves () and body waves (and) in
1.5–24 Hz by applying the single isotropic scattering theory and the extended coda …
1.5–24 Hz by applying the single isotropic scattering theory and the extended coda …
Variation of coda wave attenuation in the Alborz region and central Iran
More than 340 earthquakes recorded by the Institute of Geophysics, University of Tehran
(IGUT) short period stations from 1996 to 2004 were analysed to estimate the S-coda …
(IGUT) short period stations from 1996 to 2004 were analysed to estimate the S-coda …
Estimation of Q p and Q s of Kinnaur Himalaya
The attenuation characteristics of the Kinnaur area of the North West Himalayas were
studied using local earthquakes that occurred during 2008–2009. Most of the analyzed …
studied using local earthquakes that occurred during 2008–2009. Most of the analyzed …
Numerically calculated 3D space-weighting functions to image crustal volcanic structures using diffuse coda waves
Seismic coda measurements retrieve parameters linked to the physical characteristics of
rock volumes illuminated by high frequency scattered waves. Space weighting functions …
rock volumes illuminated by high frequency scattered waves. Space weighting functions …