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Active thrust faulting offshore Boumerdes, Algeria, and its relations to the 2003 Mw 6.9 earthquake
Author(s) -
Déverchère J.,
Yelles K.,
Domzig A.,
Mercier de Lépinay B.,
Bouillin J.P.,
Gaullier V.,
Bracène R.,
Calais E.,
Savoye B.,
Kherroubi A.,
Le Roy P.,
Pauc H.,
Dan G.
Publication year - 2005
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2004gl021646
Subject(s) - geology , fault scarp , escarpment , seismology , active fault , submarine pipeline , bathymetry , fault (geology) , thrust fault , structural basin , crust , aftershock , geomorphology , geophysics , geotechnical engineering , oceanography
We investigate the active seismogenic fault system in the area of the 2003 Mw 6.9 Boumerdes earthquake, Algeria, from a high‐resolution swath bathymetry and seismic survey. A series of 5 main fault‐propagation folds ∼20–35 km long leave prominent cumulative escarpments on the steep slope and in the deep basin. Fault activity creates Plio‐Quaternary growth strata within uplifted areas such as a rollover basin on the slope and piggyback basins in the deep ocean. Most thrusts turn to fault‐propagation folds at the sub‐surface and depict ramp‐flat trajectories. We find that the two main slip patches of the 2003 Mw 6.9 Boumerdes earthquake are spatially correlated to two segmented cumulative scarps recognized on the slope and at the foot of the margin. The overall geometry indicates the predominance of back thrusts implying underthrusting of the Neogene oceanic crust.