Title of article
Seismicity of Morocco for the Period 1987–1994
Author/Authors
S. O. El Alami، نويسنده , , B. Tadili، نويسنده , , L. Ait Brahim، نويسنده , , I. Mouayn ، نويسنده ,
Issue Information
ماهنامه با شماره پیاپی سال 2004
Pages
14
From page
969
To page
982
Abstract
A seismic data file of 3,740 earthquakes from January 1987 to December 1994 has been
elaborated for Morocco and the border regions, with 10 main events registering magnitudes from 5 to 5.6.
Such seismicity is particularly important for Morocco as the released seismic energy constitutes a
considerable part of the total energy radiated during the 20th century. Relative seismicity maps confirm the
persistence of the major features of the seismicity of Morocco. An important seismic activity is observed in
the Alboran region continental crust, which absorbs the maximum deformation resulting from the
convergence of the African and Iberian plates. However, in the longitude window 3.5 – 6 W at depths of
25 to 50 km, a seismic gap zone seems to take place. An explanation of this phenomenon may be provided
by the slab breakoff model. Even if the seismicity of Morocco remains moderate, heavy damage is observed
when the magnitude of earthquakes exceeds 4.5, especially in the case of traditional buildings.
Keywords
seismicity , Gap , aftershocks , 87–94 , MOROCCO. , hazard
Journal title
Pure and Applied Geophysics
Serial Year
2004
Journal title
Pure and Applied Geophysics
Record number
429691
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