Zusammenfassung
We present results from the cross-correlations of seismic noise recordings
among pairs of stations in the Parkfield network, California. When
performed on many station pairs at short ranges, the noise correlation
function (NCF) is the passive analog to a shot gather made with active
sources. We demonstrate the presence of both a P-wave and a Rayleigh
wave in the NCF. A time-frequency analysis allows us to separate
the two wave packets that are further identified through their polarization.
Arrival times were estimated from the NCF and they compared favorably
with predictions using ray tracing in a regional velocity model and
with the velocity gradient across the San Andreas Fault.
Nutzer