الفهرس 
CHAPTER I INTRODUCTIONOnly 14 pages are availabe for public view
 |  | from | 124 |  |  |
| | | from | 124 | | |
Abstract
Salma Delta Filed area is located in West Qantara concession in the eastern
onshore Nile Delta and south of Manzala Lake between Latitudes 31º 3’ 00’’ N, 31º
7’ N and Longitudes 31º 55’ E, 32º 2’ E.
The present study has been done to integrate the geologic studies, well log
evaluation and the petrophysical laboratory measurements on core in order to better
development and understanding the hydrocarbon potentialities of the Abu Madi
Formation in Salma Delta field. For the present work four wells were selected (SD-
1, SD-3, SD-4, and SD-5) to evaluate the Abu Madi Formation.
The available data of studied area are well-logging data including composite log,
gamma ray, density, neutron, resistivity, sonic logs, that provided by El Wastani
Petroleum Company in LAS and ASCII formats, in addition to core analysis results
for Salma Delta-4 well, to achieve the work, and make integration between core and
log data, we used linear and non-linear regressions to build relevant relationships
between log and core data.
This study includes five main chapters as follow:
The first chapter focused on a brief account was given about the location of the
study area, aim of the study and the methods of treatment have been used in the
present study, available data for study. Also the previous work on the study area has
been mentioned. This was carried out by reviewing the previous works that have
been conducted in this concern.
The second chapter, of this study deals with the geological setting including the
stratigraphic succession, tectonic and structural setting of the Nile Delta with
emphasizing on the Salma Delta Field area, regional stratigraphical overview, and
lithological characteristics especially, in Abu Madi reservoir which is the main
reservoir in this study, The sediments of Abu Madi Formation are composed of
large thick layers of rarely conglomeratic sandstone and interbedded with clay
layers which became thicker and more frequent in the upper part of the formation.
The sand is quarzitic variable in grain size and almost loose. The conglomeratic
levels in a sandy matrix in the lower part of the Formation exhibited lower
unconformity. The Abu Madi reservoir had been consistently proved to be the best
reservoir in the Nile Delta as it has a high porosity with an average of 21%