N. El-Azabi, “Sedimentary Facies, Palaeoenvironments and Facies Development of the Miocene–Pliocene Se- quence in the Sadat–Wadi Hagul Stretch, Northwest Gulf of Suez and Their Time Correlatives in the Adjacent Basins, Egypt,” 5th International Conference on the Geology of the Arab World, Cairo University, Cairo, 2000, pp. 1135-1174.

has been cited by the following article:

• TITLE: Seismicity and Geologic Structures Indubitable in Wadi Hagul, North Eastern Desert, Egypt

  AUTHORS: Tarek A. Seleem, Hamdy A. Aboulela

  KEYWORDS: Eastern Desert, Wadi Hagul, Remote Sensing, GIS, Seismic Activity

  JOURNAL NAME: International Journal of Geosciences, Vol.2 No.1, February 24, 2011

  ABSTRACT: Paleo and recent earthquakes have been recorded in Wadi Hagul area and its environs, which have left behind geologic structures of deformation preserved in exposed sedimentary rocks. To evaluate such deformation and surface break, different techniques and data types are used compromising image processing techniques, Geographic Information Systems (GIS), seismicity data, as well as, field investigation. The field investigation clarified that the study area is enriched with soft-sediment deformation structures encompassing two types of geologic structures; brittle and viscoplastic structures. The analysis of the various types of data elucidate that, the earthquakes of Wadi Hagul are frequently distributed at an average depth ranging from (1 to 35 km) within the top of the Earth’s crust which are mainly controlled by existing Hagul fault zone. The study gives new insight for a better understanding of the seismic activity in the study area which helps in the seismic hazard assessment