dc.contributor.author |
Kollias, Stefanos |
en |
dc.contributor.author |
Foudopoulos, Panayotis |
en |
dc.contributor.author |
Halkias, Christos |
en |
dc.date.accessioned |
2014-03-01T02:47:36Z |
|
dc.date.available |
2014-03-01T02:47:36Z |
|
dc.date.issued |
1984 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/33265 |
|
dc.relation.uri |
http://www.scopus.com/inward/record.url?eid=2-s2.0-0021563382&partnerID=40&md5=f63ee35f42665e59e6bb203a24999a5f |
en |
dc.subject.other |
COMPUTER PROGRAMMING - Algorithms |
en |
dc.subject.other |
SEISMOLOGY |
en |
dc.subject.other |
AUTOREGRESSIVE MOVING-AVERAGE MODELS |
en |
dc.subject.other |
MINIMUM VARIANCE DECONVOLUTION |
en |
dc.subject.other |
MULTIPLE-REFLECTION SUPPRESSION |
en |
dc.subject.other |
SEQUENTIAL SEISMIC DECONVOLUTION |
en |
dc.subject.other |
TIME-VARYING SEISMIC SIGNALS |
en |
dc.subject.other |
SIGNAL PROCESSING |
en |
dc.title |
SEQUENTIAL DECONVOLUTION OF TIME VARYING SEISMIC SIGNAL MODELS. |
en |
heal.type |
conferenceItem |
en |
heal.publicationDate |
1984 |
en |
heal.abstract |
The problem of sequential seismic deconvolution and suppression of multiple reflections is examined in this paper. An ARMA model is used to represent the unknown and probably time varying seismic wavelet, while the reflectivity sequence of the earth is modelled as a white sparse spike train. The method uses a fixed-lag version of minimum variance deconvolution, while an instrumental variable algorithm updates the model parameters. The above model is appropriately combined with a time domain state space earth model, which constructs and removes the part of the signal containing all significant multiple effects. An example is given, which illustrates the above results. |
en |
heal.publisher |
North-Holland, Amsterdam, Neth |
en |
heal.journalName |
[No source information available] |
en |
dc.identifier.spage |
652 |
en |
dc.identifier.epage |
655 |
en |