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Publications:<br />
1- "Tar occurrences and their effect on the reservoir characteristics of Lower Rudeis<br />
Formation at the central part of the Gulf of Suez,Egypt".<br />
J.Faculty of Oil and Mining (Accepted in 22/7/2003)<br />
By: <strong>Ghorab</strong> .M.A and Shazly.T.F.<br />
2- "Types of shale and their relation with the hydrocarbon fluids of Matulla<br />
Formation in the central part of the Gulf of Suez,Egypt".<br />
J.Faculty of oil and mining (Accepted in 22/7/2003)<br />
By: <strong>Ghorab</strong> .M.A and Shazly.T.F .<br />
3- "Determining the different types of porosities and the related water saturations at<br />
Rudeis-Sidri area,Gulf of Suez,Egypt".<br />
J. of Applied Geophysics 2 ,305 (2003).<br />
By:<strong>Mahmoud</strong> Abdel Halim <strong>Ghorab</strong> .<br />
4- "The relation between the variables exponent and the lithology of some Miocene<br />
rocks in the central part of the Guluf of Suez,Egypt.<br />
J. of Geologic Survy,2006.<br />
By:<strong>Mahmoud</strong> Abdel Halim <strong>Ghorab</strong> .<br />
5- DETERMINED THE PALOECOLOGY OF NUKHUL AND MATULLA<br />
FORMATIONS BY USING WELL LOG DATA, AT THE CENTRAL PART OF<br />
THE GULF OF SUEZ,EGYPT.<br />
EGYPT.J.PETROL.17 No.1,pp.7583(2007)<br />
BY:MAHMOUD GHORAB.<br />
6- DETERMINED THE DIP DIRECTIONS OF THE BEDS BY DETECTING<br />
THEIR MINEROLOGICAL COMPOSITION FORM WELL LOG DATA IN<br />
THE FEIRAN OIL FIELD, GULF OF SUEZ, EGYPT.<br />
JOUR. OF APPLIED SCIEN. RESEA.:CC-CC,(2008)<br />
BY:MAHMOUD GHORAB<br />
7- THE RELATION BETWEEN THE SHALE ORIGIN (SOURCE OR NON<br />
SOURCE) AND ITS TYPE FOR ABU ROASH FORMATION AT WADI<br />
EL NATRUN AREA, SOUTH OF WESTERN DESERT, EGYPT.
AUSTRALIIAN J. OF BASIC AND APPL.SCIENCE (2008)<br />
BY :M.GHORAB,M.RAMADAN,A.Z.NOOH.<br />
8- A COMPARATIVE STUDY BETWEEN PICKETT'S PLOT AND X-Y<br />
CROSS PLOT METHODS ON ABU ROACH FORMATION AT THE<br />
SOUTH WESTERN OF WADI EL NATRUN AREA, WESTERN<br />
DESERT, EGYPT.<br />
JOUR. OF APPLIED SCIEN. RESEA.:CC-CC,(2008)<br />
BY:M.GHORAB AND T.SHAZLY.