1997
DOI: 10.1016/s0899-5362(97)00114-0
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Crustal thickness of Egypt determined by gravity data

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Cited by 13 publications
(11 citation statements)
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“…Their estimated crustal depths along the Red Sea and Gulf of Aqaba coastal regions are consistent and well correlated with the previous Moho depth that was inferred from the gravity data analysis (e.g. Dorre et al, 1997 andSaleh et al, 2006); see the correlations in Figs. 10a, b, c. Near the Red Sea, the crust is continental, consisting of a sedimentary layer of 3 km with velocity of 3.5 km/s, overlying a 30 km thickness of crust with moderate velocity changes from 6.0 to 6.35 km/s (Meshref, 1990).…”
Section: Crustal Structures Heat Flow and Seismicitysupporting
confidence: 85%
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“…Their estimated crustal depths along the Red Sea and Gulf of Aqaba coastal regions are consistent and well correlated with the previous Moho depth that was inferred from the gravity data analysis (e.g. Dorre et al, 1997 andSaleh et al, 2006); see the correlations in Figs. 10a, b, c. Near the Red Sea, the crust is continental, consisting of a sedimentary layer of 3 km with velocity of 3.5 km/s, overlying a 30 km thickness of crust with moderate velocity changes from 6.0 to 6.35 km/s (Meshref, 1990).…”
Section: Crustal Structures Heat Flow and Seismicitysupporting
confidence: 85%
“…10a, 10b and 10c), which clearly reveals northward and eastward trends of the crustal thinning toward the Mediterranean Sea and Red Sea, respectively. This was also observed by Makris et al (1988), Marzouk (1988, Dorre et al (1997), andSeber et al (2000) who describe the Egyptian territory as a continental crust with a thickness of 30-34 km, bounded by thin new oceanic crust (< 20 km) that is formed by the Red Sea rifting.…”
Section: Crustal Structures Heat Flow and Seismicitysupporting
confidence: 70%
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