Abstract
We present a way of characterizing the structure beneath a seismic station, by exploiting stacked correlograms of three-component records from teleseismic events. This seismic daylight imaging approach exploits the extraction of reflection and conversion information from teleseismic coda via tensor autocorrelation. The approach is illustrated for a number of Australian stations in a variety of tectonic environments using hundreds of teleseismic events, to extract P and S reflectivity and converted Ps and Sp information. The results show a very good agreement with prior knowledge across Australia. Compared with the classical receiver function, the broader-frequency band of 0.5–4.0 Hz provides additional information on finer-scale structure.
| Original language | English |
|---|---|
| Pages (from-to) | 6234-6242 |
| Number of pages | 9 |
| Journal | Geophysical Research Letters |
| Volume | 43 |
| Issue number | 12 |
| DOIs | |
| Publication status | Published - 2016 |
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