Receiver-function methods utilize three-component teleseismic P coda to determine structure beneath seismographs. Most methods treat coda complexity as mode conversions and reflections off subhorizontal interfaces beneath ...
Seismic waves that travel along the surface of subducted slabs provide a means to infer petrology to considerable depth. At high frequencies (0.5-10 Hz) they are particularly sensitive to the presence and state of subducted ...
Seismic attenuation (1/Q) changes abruptly between the stable Eurasian craton and adjacent mountain belts associated with the Alpine-Himalayan collision. New attenuation measurements on local body and coda waves provide ...