Constraining crustal and uppermost mantle structure beneath station TBZ (Trabzon, Turkey) by receiver function and dispersion analyses
We jointly invert teleseismic radial-component receiver functions and regional Rayleigh and
Love surface-wave group velocities for 1-D shear-wave velocity structure beneath station …
Love surface-wave group velocities for 1-D shear-wave velocity structure beneath station …
On the P and S Receiver Functions Used for Inverting the One-Dimensional Upper Mantle Shear-Wave Velocities
The teleseismic P receiver functions are customarily inverted to attain the seismic velocities
beneath a seismic station. Surface wave dispersion data are often added to reduce the effect …
beneath a seismic station. Surface wave dispersion data are often added to reduce the effect …
A New Method for Selecting the Phase and Group Velocity Dispersion Curves of Rayleigh and Love Surface Waves: Real Data Case of Central Anatolia, Turkey …
We propose a new method to select the dispersion curve of Rayleigh and Love surface
waves obtained from local and regional earthquakes. This method is efficient for the crustal …
waves obtained from local and regional earthquakes. This method is efficient for the crustal …
Teleseismic inversion of crustal S-wave velocities beneath the Isparta Station
M Erduran - Journal of Geodynamics, 2009 - Elsevier
Waveforms of 50 teleseismic receiver functions and dispersion curves have been used to
invert jointly for the 1D average crust and uppermost mantle seismic structure beneath …
invert jointly for the 1D average crust and uppermost mantle seismic structure beneath …
[PDF][PDF] Crust structure beneath station TBZ (Trabzon, Turkey) from joint inversion of surface waves and receiver functions
Teleseismic receiver functions model velocity contrasts and relative travel times associated
with layered medium, but frequently encounter non-uniqueness problem when inverted …
with layered medium, but frequently encounter non-uniqueness problem when inverted …