Focal mechanisms for sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment (Articolo in rivista)

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  • Focal mechanisms for sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment (Articolo in rivista) (literal)
Anno
  • 2010-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1029/2010GL044289 (literal)
Alternative label
  • Geissler W., Matias L., Stich D., Carrilho F., Jokat W., Monna S., Ibenbrahim A., Mancilla F., Gutscher M., Sallares V., Zitellini N. (2010)
    Focal mechanisms for sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment
    in Geophysical research letters; AGU, American geophysical union, Washington, DC (Stati Uniti d'America)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Geissler W., Matias L., Stich D., Carrilho F., Jokat W., Monna S., Ibenbrahim A., Mancilla F., Gutscher M., Sallares V., Zitellini N. (literal)
Pagina inizio
  • L1830 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 37 (literal)
Rivista
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  • 6 (literal)
Note
  • ISI Web of Science (WOS) (literal)
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  • Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany; Univ Lisbon, Ctr Geofis, IDL, P-1749016 Lisbon, Portugal; Univ Granada, Inst Andaluz Geofis, E-18071 Granada, Spain; Inst Meteorol, P-1250102 Lisbon, Portugal; Alfred Wegener Inst Polar & Marine Res, D-2850 Bremerhaven, Germany; INGV, Natl Inst Geophys & Vulcanol, I-00143 Rome, Italy; Ctr Natl Rech Sci & Tech, Rabat 10102, Morocco; Univ Granada, Inst Andaluz Geofis, E-18071 Granada, Spain; Univ Brest, CNRS, UMR 6538, Inst Univ Europeen Mer, F-29280 Plouzane, France; CSIC, ICM, Inst Marine Sci, Barcelona 08002, Spain; CNR-ISMAR, Geologia Marina - Bologna; (literal)
Titolo
  • Focal mechanisms for sub-crustal earthquakes in the Gulf of Cadiz from a dense OBS deployment (literal)
Abstract
  • 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. (literal)
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