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Structural synthesis of eastern part of Beni Suef Basin northeast Nile valley, Egypt / Eman Hassan Salem ; Supervised Adel A. Sehim , Adel R. Moustafa

By: Contributor(s): Material type: TextTextLanguage: English Publication details: Cairo : Eman Hassan Salem , 2015Description: 148 P. : facsimiles , maps ; 25cmOther title:
  • المزيج البنائى لمنطقة شرق حوض بنى سويف: شمال شرق وادى النيل: مصر [Added title page title]
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  • Issued also as CD
Dissertation note: Thesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology Summary: The structural architecture of East Beni Suef Basin (EBSB) was studied using 3D seismic data and seven wells. The sedimentary fill of the basin is made up of Lower Cretaceous Kharita Formation, Upper Cretaceous Bahariya, Abu Roash, and Khoman Formations, Paleocene-Middle Eocene Apollonia Formation, Upper Eocene Maadi Formation and Post- Eocene sediments. Normal faults are the dominant structures in the basin. Three sets of faults were mapped; ENE-WSW fault set, NW-SE fault set, and NNW-SSE fault set. The EBSB was subjected to three main tectonic phases; The oldest (Early Cretaceous) tectonic phase was associated with the main extension and subsidence along the EBSB. The second phase was contemporaneous with the Late Cretaceous Syrian Arc deformation. The third tectonic phase took place during the Early Tertiary and was extensional
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Thesis Thesis قاعة الرسائل الجامعية - الدور الاول المكتبة المركزبة الجديدة - جامعة القاهرة Cai01.12.15.M.Sc.2015.Em.S (Browse shelf(Opens below)) Not for loan 01010110067257000
CD - Rom CD - Rom مخـــزن الرســائل الجـــامعية - البدروم المكتبة المركزبة الجديدة - جامعة القاهرة Cai01.12.15.M.Sc.2015.Em.S (Browse shelf(Opens below)) 67257.CD Not for loan 01020110067257000

Thesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology

The structural architecture of East Beni Suef Basin (EBSB) was studied using 3D seismic data and seven wells. The sedimentary fill of the basin is made up of Lower Cretaceous Kharita Formation, Upper Cretaceous Bahariya, Abu Roash, and Khoman Formations, Paleocene-Middle Eocene Apollonia Formation, Upper Eocene Maadi Formation and Post- Eocene sediments. Normal faults are the dominant structures in the basin. Three sets of faults were mapped; ENE-WSW fault set, NW-SE fault set, and NNW-SSE fault set. The EBSB was subjected to three main tectonic phases; The oldest (Early Cretaceous) tectonic phase was associated with the main extension and subsidence along the EBSB. The second phase was contemporaneous with the Late Cretaceous Syrian Arc deformation. The third tectonic phase took place during the Early Tertiary and was extensional

Issued also as CD

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