Dissertation (Metadaten)
Titel:Origin and nature of the regional detachment fault in the area of the deep Galicia margin
 
Autor:Thomas Leythaeuser
 
URN:NBN:urn:nbn:de:gbv:8-diss-11382
 
Fakultät:Mathematisch-Naturwissenschaftliche Fakultät
DDC Sachgebiet:550 Geowissenschaften
 
Datum der mdl. Prüfung:02.07.2004
 
Referent(in):Prof. Dr. T. Reston
Korreferent(en) Korreferentin:Prof. Dr. E. R. Flüh
 
Beschreibung (original):In the area of the Deep Galicia Margin two multi-channel seismic lines (ISE-1 and ISE-2) have been processed and interpreted in the present study. The main objective was to attempt clarification of the precise nature and origin of the so-called S-reflector. For this purpose a full waveform inversion was carried out for a selected CMP gather besides prestack depth migration and poststack time migration. The results of the full waveform inversion lead to the conclusion that the S-reflector represents an approx. 50m thick low-velocity zone wedged in a stepwise velocity increase between continental crust and mantle. For this zone a compressional wave velocity of 5.2 km/s was determined as compared to 5.45 km/s for the overlying continental crust and 7.0 km/s for the mantle interval below. These p-wave velocities in the uppermost mantle are interpreted to result from a particular serpentinisation history involving two separate stages of seawater influx leading to the development of a detachment fault seismically imaged as the S-reflector.
 
(übersetzt):keine dt.-spr. Zusammenfassung vh.
 
Schlagworte:Spanien ; Kontinentalrand ; Geophysik ; Iberische Halbinsel ; Rifting ; Common-mid-point-Refraktionsseismik ; S-reflector, passive continental margin, rifting, detachment fault, peridotite ridge, full waveform inversion, serpentinisation
 
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