We have developed a new imaging technique of subsurface heterogeneities that uses Sp-waves from natural earthquakes. This technique can be used as a first screening tool in frontier exploration areas before conventional active exploration. Analyzing Sp-waves from 28 earthquakes (Mj 2.0 to 4.2) recorded by two permanent seismic stations, we built an image of the distributions of velocity discontinuities in southeastern offshore Hokkaido, Japan, where intraplate earthquakes in the Pacific plate frequently occur. Our results indicated the presence of three horizontally continuous, distinct discontinuities corresponding to geologic boundaries estimated in a previous study.We also derived the frequency-dependent quality factor Q for P- and S-wav...
Deep tectonic tremors occur at the downdip extent of the seismogenic zone due to fluid processes. Be...
Large-amplitude surface waves from the 2011 Tohoku-Oki earthquake triggered many seismic events acro...
Earthquakes in subduction zones occur in the slab mantle, in the subducting crust, on the subduction...
This thesis presents five studies that apply geophysical tools to image and interpret the heterogene...
This thesis investigates the potential of passive seismic methods that make use of body waves, and e...
Inhomogeneities in the earth (fractures, layering, shape, composition) are responsible for seismic w...
Global phases are seismic waves that travel through the earth's core before emerging at the surface....
The subducting Pacific plate acts an efficient waveguide for high-frequency signals and often produc...
Passive seismic surveys have long been applied in the context of exploration studies. Our research f...
This manuscript reports the results of research using both conventional and unconventional energy so...
Reflectivity imaging of local earthquake seismograms has revealed the structure of the Hikurangi sub...
Seismic surveys are used to create visual representations of subsurface geology by detecting the ref...
Near-source path effects imprint the wave field emanating from a seismic source and, if not well res...
International audienceWe perform a multicomponent analysis to evaluate the validity and limits of no...
Global phases, viz. seismic phases that travel through the Earth?s core, can be used to locally imag...
Deep tectonic tremors occur at the downdip extent of the seismogenic zone due to fluid processes. Be...
Large-amplitude surface waves from the 2011 Tohoku-Oki earthquake triggered many seismic events acro...
Earthquakes in subduction zones occur in the slab mantle, in the subducting crust, on the subduction...
This thesis presents five studies that apply geophysical tools to image and interpret the heterogene...
This thesis investigates the potential of passive seismic methods that make use of body waves, and e...
Inhomogeneities in the earth (fractures, layering, shape, composition) are responsible for seismic w...
Global phases are seismic waves that travel through the earth's core before emerging at the surface....
The subducting Pacific plate acts an efficient waveguide for high-frequency signals and often produc...
Passive seismic surveys have long been applied in the context of exploration studies. Our research f...
This manuscript reports the results of research using both conventional and unconventional energy so...
Reflectivity imaging of local earthquake seismograms has revealed the structure of the Hikurangi sub...
Seismic surveys are used to create visual representations of subsurface geology by detecting the ref...
Near-source path effects imprint the wave field emanating from a seismic source and, if not well res...
International audienceWe perform a multicomponent analysis to evaluate the validity and limits of no...
Global phases, viz. seismic phases that travel through the Earth?s core, can be used to locally imag...
Deep tectonic tremors occur at the downdip extent of the seismogenic zone due to fluid processes. Be...
Large-amplitude surface waves from the 2011 Tohoku-Oki earthquake triggered many seismic events acro...
Earthquakes in subduction zones occur in the slab mantle, in the subducting crust, on the subduction...