TY  - BOOK
AU  - Ali Abdelhady Abdelbaset Abdelraheim
AU  - Ahmed Mokhtar AbuKhadra , 
AU  - Selim Saber Selim , 
TI  - Geologic modeling of t he lower messinian sequences in Elbasant field, onshore East Nile Delta-Egypt / 
PY  - 2018///
CY  - Cairo : 
PB  - Ali Abdelhady Abdelbaset Abdelraheim , 
KW  - Qawasim formation
KW  - Seismic geomorphology
KW  - Tidal-dominated estuary
N1  - Thesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology; Issued also as CD
N2  - The development of a tidal-dominated estuary above the basal messinian incision in  the lower messinian qawasim formation in the onshore East Nile Delta province is interpreted from 3D seismic, core, borehole images, and wireline logs data from four  selected wells. Sedimentologically in terms of five facies associations of the qawasim Formation are; tidally influenced fluvial channels, overbank muds, estuarine tidal channel, estuarine tidal bars and estuarine muds. These facies associations are building blocks for  the depositional model that bounded by two incisions during the early messinian time. The  lower cycle is called qawasim level I which contains fluvial channel encased in overbank muds of fluvial plain. The upper cycle, qawasim level II is characterized by estuarine tidal  channel, estuarine tidal bars, and estuarine muds. The geomorphological characteristics of qQawasim Formation (lower and upper levels) can be detected using detailed seismic interpretations. The sedimentological and seismic characteristics of the Qawasim Formation  in El Basant field may indicates the depositions in a tidal regime within estuary domain
UR  - http://172.23.153.220/th.pdf
ER  -