The autocorrelation of the seismic transmission response of a layered medium(autocorrelogram), in the presence of a free surface, corresponds to the reflection response. Despite manystudies on the imaging of local structures through retrieval and forward modeling of stackedautocorrelograms, there is limited work on the inversion of these data. In this study, we demonstrate thatthe probabilistic inversion of autocorrelograms is efficientand can be used as an alternative imaging toolwhen other approaches are not applicable. Here, we calculate autocorrelograms of teleseismicPwave codarecorded on more than 1,200 permanent and temporary seismic stations across Australia and utilize aBayesian framework to invert these data for crustal imaging. Th...
By comparing records of the radial component of motion of teleseismic P waves to records of the vert...
We retrieve the local P wave empirical Green's functions between the elements of five different regi...
Teleseismic traveltime anomalies for events recorded on portable seismograph arrays across the north...
Due to a sharp contrast in elastic properties across the basement rocks of sedimentary basins (SBs),...
International audienceDue to a sharp contrast in elastic properties across the basement rocks of sed...
Traveltimes of P and mode-converted S-waves and their reverberations place a tight constraint on the...
Seismic body waves from distant earthquakes, which propagate near vertically beneath recording stati...
In many regions of the world characterized by a relatively low rate of seismicity, the determination...
The prevailing drive of modern seismology is to improve our knowledge of the Earth's structure, comp...
Current estimates of Moho depth in southeastern Australia are based on sparse sampling. The results ...
This project harnesses the high density of seismic stations in AlpArray and the AlpArray complementa...
The discovery of long-range spatial correlation in earthquake coda and ambient noise records has had...
Global phases are seismic waves that travel through the earth's core before emerging at the surface....
International audienceReceiver functions are a powerful tool to isolate and interpret receiver-side ...
Adjoint tomography has been recently applied to ambient seismic noise and teleseismic P waves separa...
By comparing records of the radial component of motion of teleseismic P waves to records of the vert...
We retrieve the local P wave empirical Green's functions between the elements of five different regi...
Teleseismic traveltime anomalies for events recorded on portable seismograph arrays across the north...
Due to a sharp contrast in elastic properties across the basement rocks of sedimentary basins (SBs),...
International audienceDue to a sharp contrast in elastic properties across the basement rocks of sed...
Traveltimes of P and mode-converted S-waves and their reverberations place a tight constraint on the...
Seismic body waves from distant earthquakes, which propagate near vertically beneath recording stati...
In many regions of the world characterized by a relatively low rate of seismicity, the determination...
The prevailing drive of modern seismology is to improve our knowledge of the Earth's structure, comp...
Current estimates of Moho depth in southeastern Australia are based on sparse sampling. The results ...
This project harnesses the high density of seismic stations in AlpArray and the AlpArray complementa...
The discovery of long-range spatial correlation in earthquake coda and ambient noise records has had...
Global phases are seismic waves that travel through the earth's core before emerging at the surface....
International audienceReceiver functions are a powerful tool to isolate and interpret receiver-side ...
Adjoint tomography has been recently applied to ambient seismic noise and teleseismic P waves separa...
By comparing records of the radial component of motion of teleseismic P waves to records of the vert...
We retrieve the local P wave empirical Green's functions between the elements of five different regi...
Teleseismic traveltime anomalies for events recorded on portable seismograph arrays across the north...