Information - SM5 Seismic Imaging with Coda andNoise
Event Information
Seismic coda and ambient seismic noise are complicated wave fields, which are often treated as unwanted and disturbing signals in seismic recordings. The seismic coda is caused by multiple scattering at randomly distributed heterogeneities. Ambient seismic noise, on the other hand, is generated by randomly distributed seismic sources. Recent studies have revealed that using a statistical treatment one may extract important information from these random wave fields. Examples are the extraction of Green's functions, detections of temporal variations in the Earth, estimation of scattering and dissipation strengths, and others. This session invites contributions on new developments in the use of random wave fields. We welcome contributions on theoretical developments, laboratory experiments, and seismological field data interpretations.
Preliminary List of Solicited Speakers
Co-Sponsorship
General Statement
The information contained hereafter has been compiled and
uploaded by the Session Organizers via the "Organizer Session Form".
The Session Organizers have therefore the sole responsibility
that this information is true and accurate at the date of publication,
and the conference organizer cannot accept any legal responsibility
for any errors or omissions that may be made, and he makes no warranty,
expressed or implied, with regard to the material published.
Back