FN Archimer Export Format PT J TI Comment on "Zemmouri earthquake rupture zone (M-w 6.8, Algeria): Aftershocks sequence relocation and 3D velocity model" by A. Ayadi et al. BT AF DEVERCHERE, Jacques DE LEPINAY, Bernard Mercier CATTANEO, Antonio STRZERZYNSKI, Pierre CALAIS, Eric DOMZIG, Anne BRACENE, Rabah AS 1:1,2;2:3;3:4;4:1,2;5:5;6:6;7:7; FF 1:;2:;3:;4:;5:;6:;7:; C1 Univ Europeenne Bretagne, Brest, France. Univ Brest, Inst Univ Europeen Mer, UMR Domaines Ocean 6538, CNRS, F-29280 Plouzane, France. Univ Nice Sophia Antipolis, CNRS, UMR GeoAzur 6526, F-06560 Valbonne, France. IFREMER, Ctr Brest, Lab Environm Sedimentaires, F-29280 Plouzane, France. Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA. Midland Valley Explorat, Glasgow G2 2HG, Lanark, Scotland. SONATRACH Explorat, Ctr Res & Dev, Boumerdes 35000, Algeria. C2 UEB, FRANCE UBO, FRANCE UNIV NICE, FRANCE IFREMER, FRANCE UNIV PURDUE, USA MIDLAND VALLEY EXPLORAT, UK SONATRACH EXPLORAT, ALGERIA SI BREST IN WOS Ifremer jusqu'en 2018 copubli-france copubli-europe copubli-univ-france copubli-int-hors-europe copubli-sud IF 3.303 TC 13 TU Centre national de la recherche scientifique Institut de recherche pour le développement Observatoire de la côte d'azur Université Nice - Sophia-Antipolis Université Pierre et Marie Curie UR https://archimer.ifremer.fr/doc/00003/11440/7994.pdf LA English DT Article CR MARADJA MARADJA/2 PRISME BO Le Suroît L'Atalante DE ;Boumerdès-Zemmouri earthquake;deformation;kinematics;margin AB Although often difficult to characterize, the relationship between a seismic rupture, its aftershock sequence, and cumulative subsurface or surface faulting or folding is an important challenge to modern seismology and seismotectonics. Among other benefits, it helps document fault length, slip, and magnitude relationships, reconstruct the evolution of the rupture process through historical and prehistorical times and identify the complexity of the deformation in its path toward the surface. This approach is a prerequisite to any seismic hazard assessment but is particularly difficult for faults whose surface trace projects offshore. A specific effort to identify and quantify the source parameters of large earthquakes in coastal areas is therefore needed, not only in subduction zones but also in areas of slow rate and/or diffuse deformation. PY 2010 PD APR SO Journal Of Geophysical Research-solid Earth SN 0148-0227 PU Amer Geophysical Union VL 115 IS B04320 UT 000277265300001 BP 1 EP 6 DI 10.1029/2008JB006190 ID 11440 ER EF