Open AccessMoment tensor solutions for small and moderate earthquakes in the Ibero‐Maghreb region
Author(s) -
Stich Daniel,
Ammon Charles J.,
Morales Jose
Publication year - 2003
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2002jb002057
Subject(s) - geology , seismology , seismogram , moment tensor , principal axis theorem , focal mechanism , seismotectonics , geodesy , peninsula , inversion (geology) , clockwise , neogene , tectonics , fault (geology) , rotation (mathematics) , geometry , paleontology , geography , deformation (meteorology) , mathematics , oceanography , archaeology , structural basin
We applied time domain moment tensor inversion of local and regional waveforms to small and moderate ( M w = 3.5–5.7) shallow earthquakes from the Iberian Peninsula, northern Morocco, and northern Algeria. For the 6+ years period from November 1995 to March 2002 and the previous Network of Autonomously Recording Seismograms (NARS) experiment, moment tensor solutions were obtained for 58 events, considerably increasing the total number of available solutions in the study area. For each event we performed a moment tensor inversion and a double‐couple grid search. For simple faulting events the grid search is valuable as a quality test for its ability to reveal potential ambiguities of the solutions and to assess confidence limits of fault plane parameters or principal axes orientation. The computed mechanisms show regional consistency: A large part of the Iberian Peninsula is characterized by normal faulting mechanisms with SW‐NE oriented T axes. Thrusting and SE‐NW compression is dominant in Algeria. In the Alboran Sea, the westernmost part of the Mediterranean, and the transition between both regimes, strike‐slip mechanisms dominate with approximately N‐S oriented P axes. This pattern suggests a regional anomaly characterized by clockwise rotation of the principal horizontal stress orientations.