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AGU: Geophysical Research Letters

 

Index Terms

  • Geodesy and Gravity: Seismic deformations
  • Seismology: Earthquake dynamics and mechanics
  • Seismology: Earthquake parameters

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L18607, 4 PP., 2004
doi:10.1029/2004GL020687

Slip distribution of the 2003 Boumerdes-Zemmouri earthquake, Algeria, from teleseismic, GPS, and coastal uplift data

B. Delouis

UMR 6526, CNRS, Géosciences Azur, Nice, France

M. Vallée

Osservatorio Vesuviano, Istituto Nazionale di Geofisica e Vulcanologia, Naples, Italy

M. Meghraoui

UMR 7516, CNRS, Institut de Physique du Globe, Strasbourg, France

E. Calais

Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, Indiana, USA

S. Maouche

Centre de Recherche en Astronomie, Astrophysique et Geophysique (CRAAG), Algiers, Algeria

K. Lammali

Centre de Recherche en Astronomie, Astrophysique et Geophysique (CRAAG), Algiers, Algeria

A. Mahsas

Centre de Recherche en Astronomie, Astrophysique et Geophysique (CRAAG), Algiers, Algeria

P. Briole

UMR 7580, CNRS, Institut de Physique du Globe, Paris, France

F. Benhamouda

Institut National de Cartographie et de Télédétection (INCT), Algiers, Algeria

K. Yelles

Centre de Recherche en Astronomie, Astrophysique et Geophysique (CRAAG), Algiers, Algeria

Using a joint inversion of seismological waveforms and ground displacement observations, we estimate several parameters of the fault geometry and rupture process of the Mw = 6.9 May 21, 2003 Boumerdes-Zemmouri earthquake. The relocated epicenter is considered as a known parameter. Total rupture length, rupture duration, and maximum slip are 55 km (from 3.4°E to 4.0°E), 12 s, and 3 m. The modeled south dipping reverse fault, oriented ENE-WSW outcrops a few km offshore which is consistent with the absence of observed surface rupture inland. Two shallow and relatively localized slip zones are found, on both sides of the hypocenter. To the SW, between Boumerdes and Zemmouri, slip is concentrated between 11 and 2 km depth. To the NE, between Zemmouri and Dellys, slip is concentrated between 6 km depth and the sea floor. Various resolution tests indicate that our model is well constrained by the available data, and help understanding which data constrains each parameter of the model.

Received 5 June 2004; accepted 18 August 2004; published 23 September 2004.

Citation: Delouis, B., M. Vallée, M. Meghraoui, E. Calais, S. Maouche, K. Lammali, A. Mahsas, P. Briole, F. Benhamouda, and K. Yelles (2004), Slip distribution of the 2003 Boumerdes-Zemmouri earthquake, Algeria, from teleseismic, GPS, and coastal uplift data, Geophys. Res. Lett., 31, L18607, doi:10.1029/2004GL020687.

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