Study of Conrad and Shaban deep brines, Red Sea, using bathymetric, parasound and seismic surveys
Kabeel, K. (2017). Study of Conrad and Shaban deep brines, Red Sea, using bathymetric, parasound and seismic surveys. EKB Journal Management System, 6(1), 90-96. doi: 10.1016/j.nrjag.2017.04.003
Khamis Kabeel. "Study of Conrad and Shaban deep brines, Red Sea, using bathymetric, parasound and seismic surveys". EKB Journal Management System, 6, 1, 2017, 90-96. doi: 10.1016/j.nrjag.2017.04.003
Kabeel, K. (2017). 'Study of Conrad and Shaban deep brines, Red Sea, using bathymetric, parasound and seismic surveys', EKB Journal Management System, 6(1), pp. 90-96. doi: 10.1016/j.nrjag.2017.04.003
Kabeel, K. Study of Conrad and Shaban deep brines, Red Sea, using bathymetric, parasound and seismic surveys. EKB Journal Management System, 2017; 6(1): 90-96. doi: 10.1016/j.nrjag.2017.04.003

Study of Conrad and Shaban deep brines, Red Sea, using bathymetric, parasound and seismic surveys

NRIAG Journal of Astronomy and Geophysics
Volume 6, Issue 1, June 2017, Pages 90-96    PDF (3.45 M)
DOI: 10.1016/j.nrjag.2017.04.003
Author
Khamis Kabeel
Abstract
Red Sea was formed where African and Arabian plates are moving apart. Each year the plates drift about 2.5 cm farther apart, so that the Red Sea is slowly but steadily growing hence known as the next coming ocean simply an embryonic ocean. It is characterized by the presence of many deep fractures, located almost exactly along the middle of the Sea from northwest to southeast. Theses fractures have steep sides, rough bottom and brines coming up form on the bottom. Brine deposits are the result of subsurface magmatic activity. They are formed in graben structure as shown by the bathymetric, parasound and seismic studies in the investigated area.
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