Publication | Open Access
The Gulf of Aqaba earthquake swarm of 1983 January-April
64
Citations
29
References
1984
Year
EngineeringFault GeologyPeriod 1983Earthquake HazardsEarth ScienceGeophysicsEarthquake SourceLocal EarthquakesGeodesyMarine GeologyAqaba Earthquake SwarmInduced SeismicityGeographyEarthquake RuptureTectonicsFault GeometrySeismologyEarthquake ActivitySeismic Hazard
In the period 1983 January 21 -April 20, more than 500 local earthquakes (ML≥ 4.85) occurred in the Gulf of Aqaba area between latitudes 29°00′and 29°25′and longitudes 34°30′and 34°45′. Most of the activity including the largest shocks was restricted to the area between latitudes 29°07′and 29° 15′and longitudes 34°33′and 34°42′where the NW Atiya regional dyke crosses the area and is horizontally displaced by NE strike-slip faults. The first-motion directions of four large shocks, including the largest, at both UNJ and HLW stations are in agreement with a strike-slip mechanism at a NE-trending fault in this area. The b value showed a temporal increase with time from 0.43 to 0.69. This, together with other geological and geophysical observations may indicate that subsurface magmatic activity has affected the stressed crustal rocks, thus triggering earthquake activity.
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