Bulletin of the Seismological Society of America; February 2006; v. 96; no. 1;
p. 59-68; DOI: 10.1785/0120050108
© Seismological Society of America
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Figure 4. Coseismic Interferograms of the 24 February 2004 Al Hoceima earthquake. Each
fringe shows 2.83 cm of surface displacement along the radar line of sight.
Dashed lines are digitized fringes used in modeling the interferograms. Blue
line is the best model fault. Barbed lines are inactive thrust faults shown to
facilitate comparison of the interferograms. Black arrows indicate radar look
direction.
