[BOOK][B] Seismic wave propagation and scattering in the heterogeneous earth
The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …
natural earthquakes and man-made sources. In classical seismology, the earth is …
Repeating earthquakes
Repeating earthquakes, or repeaters, are identical in location and geometry but occur at
different times. They appear to represent recurring seismic energy release from distinct …
different times. They appear to represent recurring seismic energy release from distinct …
On the measurement of seismic traveltime changes in the time–frequency domain with wavelet cross-spectrum analysis
The spatial distribution of temporal variations in seismic wavespeed is key to understanding
the sources and physical mechanisms of various geophysical processes. The imaging of …
the sources and physical mechanisms of various geophysical processes. The imaging of …
Spurious velocity changes caused by temporal variations in ambient noise frequency content
Ambient seismic noise cross-correlations are now being used to detect temporal variations
of seismic velocity, which are typically on the order of 0.1 per cent. At this small level …
of seismic velocity, which are typically on the order of 0.1 per cent. At this small level …
Sudden drop of seismic velocity after the 2004 Mw 6.6 mid‐Niigata earthquake, Japan, observed with Passive Image Interferometry
Passive Image Interferometry (PII) is a seismological method employing ambient seismic
noise to monitor the temporal evolution of mean shear wave velocity within the Earth. First …
noise to monitor the temporal evolution of mean shear wave velocity within the Earth. First …
Seismic noise correlations to image structural and mechanical changes associated with the Mw 7.9 2008 Wenchuan earthquake
We locate temporal changes of seismic wave speed and scattering properties of the crust
associated with the 2008 Mw7. 9 Wenchuan earthquake. To that end, we analyze ambient …
associated with the 2008 Mw7. 9 Wenchuan earthquake. To that end, we analyze ambient …
Coseismic and postseismic elastic wave velocity variations caused by the 2008 Iwate‐Miyagi Nairiku earthquake, Japan
We analyze coseismic and postseismic velocity variations caused by the June 13, 2008
Iwate‐Miyagi Nairiku earthquake (MW= 6.9) using Passive Image Interferometry (PII) …
Iwate‐Miyagi Nairiku earthquake (MW= 6.9) using Passive Image Interferometry (PII) …
Time-lapse changes of seismic velocity in the shallow ground caused by strong ground motion shock of the 2000 Western-Tottori earthquake, Japan, as revealed from …
A large earthquake shock often drops the seismic velocity of the shallow ground. However, it
is not clear whether the dropped velocity recovers shortly after the earthquake shock or not …
is not clear whether the dropped velocity recovers shortly after the earthquake shock or not …
Diversity of fault zone damage and trap** structures in the Parkfield section of the San Andreas Fault from comprehensive analysis of near fault seismograms
MA Lewis, Y Ben-Zion - Geophysical Journal International, 2010 - academic.oup.com
We perform comprehensive analyses of trapped waves and signals of damaged fault zone
rocks associated with time delays of body waves along the Parkfield section of the San …
rocks associated with time delays of body waves along the Parkfield section of the San …
Catalog of small repeating earthquakes for the Japanese Islands
T Igarashi - Earth, Planets and Space, 2020 - Springer
Groups of repeating earthquakes, which occur in approximately the same location and
possess a similar focal mechanism, have been extracted in various tectonic environments …
possess a similar focal mechanism, have been extracted in various tectonic environments …