dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Intrinsic and scattering attenuation image of Teide volcanic complex from an active seismic experiment
VerfasserIn Janire Prudencio, Edoardo Del Pezzo, Araceli Garcia-Yeguas, Jesús Ibáñez
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250057168
 
Zusammenfassung
Data from an active seismic experiment to study the internal structure of Teide volcano in Tenerife island, Spain, were collected during winter 2007 in a multi-national project envolving numerous research Institutions. 6850 air gun shots fired from The Spanish oceanographic R/V Hespérides were recorded on a dense local seismic network consisting of 150 independent seismic stations on land with a sampling frequency of 200 hertz. Data quality is generally good, and P wave arrivals are identified up to an offset of 30–40 kilometers, and in some cases up to 60 kilometers. This data set has been utilized in the present work to study the seismic attenuation and scattering properties of the Teide volcanic complex. We first studied the spectral properties of the seismogram envelopes, observing that heterogeneity is sufficiently high in the whole earth volume investigated to approximate the propagation by a diffusion process. Then, the coda envelope for any source-receiver couple has been inverted in terms of scattering parameters for a diffusion model. The retrieved parameters have been associated with a gaussian space probability function, maximum in the midlle of the segment connecting source epicenter and station and tending to zero at the borders of the scattering ellipse. Being the shots fired at surface, the 2-D assumption is realistic. The space distribution of the scattering parameters weighted by the probability already discussed furnishes the 2-D image. Results show strong space variation of the attenuation and scattering coefficients, associated with the main structural features of the Teide volcanic complex.