PUMA
Istituto di Scienze Marine     
Geissler W., Matias L., Stich D., Carrilho F., Jokat W., Monna S., Ibenbrahim A., Mancilla F., Gutscher M., Sallares V., Zitellini N. Focal mechanisms for sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment. In: Geophysical Research Letters, vol. 37 article n. L18309. AMER GEOPHYSICAL UNION, 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA, 2010.
 
 
Abstract
(English)
An eleven-month deployment of 25 ocean bottom seismometers provides an unprecedented opportunity to study low-magnitude local earthquakes in the complex transpressive plate boundary setting of the Gulf of Cadiz, known for the 1755 Lisbon earthquake and tsunami. 36 relocated earthquakes (ML 2.2 to 4.8) concentrate at 40-60 km depth, near the base of the seismogenic layer in similar to 140 Ma old oceanic mantle lithosphere, and roughly align along two perpendicular, NNE-SSW and WNW-ESE striking structures. First motion focal mechanisms indicate compressive stress for the cluster close to the northern Horseshoe fault termination which trends perpendicular to plate convergence. Focal mechanisms for the second cluster near the southern termination of the Horseshoe fault indicate a strike-slip regime, providing evidence for present-day activity of a dextral shear zone proposed to represent the Eurasia-Africa plate contact. We hypothesize that regional tectonics is characterized by slip partitioning. Citation: Geissler, W. H., et al. (2010), Focal mechanisms for sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment, Geophys. Res. Lett., 37, L18309, doi: 10.1029/2010GL044289.
DOI: 10.1029/2010GL044289
Subject GIBRALTAR PLATE BOUNDARY
TECTONIC IMPLICATIONS
MARGIN;
IBERIA
ATLANTIC


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