The Abu-Dabbab area, located in the central part of the Egyptian Eastern Desert, is an active seismic region where micro-earthquakes (≈ML 1.73) tectonic activity signals all over the study area. Firstly, our results indicate low to medium tectonic activity and general anomaly patterns detected along the major tectonic zones of the study area. Secondly, based on most of the low to medium tectonic activity distributed in the study area and the detected anomalies, we discuss two potential drivers of the seismicity in the Abu-Dabbab area, which are fault-controlled and deep-rooted activities
Abstract Paleo and recent earthquakes have been recorded in Wadi Hagul area and its environs, which ...
AbstractThe study of earthquake activity and seismic hazard assessment of Egypt is very important du...
AbstractThe earthquake activity and the state of stress in and around Egypt will provide an opportun...
AbstractA local geodetic network consisting of eleven benchmarks has been established to study the r...
A local geodetic network consisting of eleven benchmarks has been established to study the recent cr...
Abu-Dabbab area is characterized by high seismicity and complex tectonic setting, for these facts, a...
Quiescent faults may be capable of creating catastrophic earthquakes in locations with moderate and/...
AbstractAbu Dabbab area is considered as one of the most active earthquake sources in Egypt. It is d...
Quiescent faults may be capable of creating catastrophic earthquakes in locations with moderate and/...
AbstractA local geodetic network consisting of eleven benchmarks has been established to study the r...
The Sieyal fault is in the western desert of Egypt about 100 kilometers southwest of Aswan. The remo...
AbstractIn the Southern Eastern Desert of Egypt, A NW–SE oriented structural graben extends from the...
Abstract The basement rocks, Neogene sediments and Quaternary alluvial deposits in the Abu Dabbab a...
AbstractAbu Dabbab area is considered as one of the most active earthquake sources in Egypt. It is d...
ABSTRACT: The Central Eastern Desert of Egypt is composed mainly of Precambrian metamorphic and magm...
Abstract Paleo and recent earthquakes have been recorded in Wadi Hagul area and its environs, which ...
AbstractThe study of earthquake activity and seismic hazard assessment of Egypt is very important du...
AbstractThe earthquake activity and the state of stress in and around Egypt will provide an opportun...
AbstractA local geodetic network consisting of eleven benchmarks has been established to study the r...
A local geodetic network consisting of eleven benchmarks has been established to study the recent cr...
Abu-Dabbab area is characterized by high seismicity and complex tectonic setting, for these facts, a...
Quiescent faults may be capable of creating catastrophic earthquakes in locations with moderate and/...
AbstractAbu Dabbab area is considered as one of the most active earthquake sources in Egypt. It is d...
Quiescent faults may be capable of creating catastrophic earthquakes in locations with moderate and/...
AbstractA local geodetic network consisting of eleven benchmarks has been established to study the r...
The Sieyal fault is in the western desert of Egypt about 100 kilometers southwest of Aswan. The remo...
AbstractIn the Southern Eastern Desert of Egypt, A NW–SE oriented structural graben extends from the...
Abstract The basement rocks, Neogene sediments and Quaternary alluvial deposits in the Abu Dabbab a...
AbstractAbu Dabbab area is considered as one of the most active earthquake sources in Egypt. It is d...
ABSTRACT: The Central Eastern Desert of Egypt is composed mainly of Precambrian metamorphic and magm...
Abstract Paleo and recent earthquakes have been recorded in Wadi Hagul area and its environs, which ...
AbstractThe study of earthquake activity and seismic hazard assessment of Egypt is very important du...
AbstractThe earthquake activity and the state of stress in and around Egypt will provide an opportun...