الفهرس 
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Abstract
Nile Delta Basin is characterized by its high Hydrocarbon potentialities. This basin
is attracted the attention of geologists and geophysicists for Hydrocarbon
investigation and exploration. This is due to the huge subsurface sedimentary
section exists in the basin which include considerable source rocks within Kafr El
Sheikh Formation in Pliocene Age and Sidi Salim Formation and Qantara Formation
in Miocene Age and Tineh Formation in Oligocene Age, and considerable reservoir
rocks within El Wastani Formation and Kafr El Sheikh Formation in Pliocene Age and
Abu Madi Formation and Qawasim Formation and Qantara Formation in Miocene
Age and also Tineh Formation in Oligocene Age.
The study area lies approximately 6 km South of El Mansoura city. It is located
between Lat. 30 ° 54’ 00”, 31° 00’ 00”N and Long. 31° 20’ 00”, 31°25` 00”E
approximately.
The materials used in this study include available previous geological and
geophysical studies as well as internal reports of companies is helpful to study the
general stratigraphic column of the Nile Delta basin with special emphasis on the
study area. Also, subsurface data are read in the form of lithostratigraphic
information , and was used complete log sets from five wells to evaluate Abu Madi
Formation and complete log sets from seven wells to evaluate Qawasim Formation
in the study area, including the Gamma Ray (GR), Spontaneous Potential (SP),
Caliper, Deep , intermediate and Shallow resistivities (HRLA, AIT), Micro-Spherically
Focused log (MSFL), Photoelectric factor (PEF), and porosity tools (Density, Neutron,
and Sonic), In the form of (LAS Format),and pressure readings and samples for six
wells and also twenty seismic lines in the study area.
The data entry and corrected and interpreted by Special Soft wares as Petrel
(Schlumberger, 2013), Seisvision for seismic interpreta@on (Geographics Halliburton
landmark 2012), (Interac@ve Petrophysics (IP)) (Version 3.5, Schlumberger, 2008),
Geoatlas (