POST-STACK SEISMIC INVERSION FOR LAND SEISMIC DATA NORTHERN WESTERN DESERT, EGYPT
El-Werr, A., Shokry, M., Shebl, A., Elmidany, A. (2017). POST-STACK SEISMIC INVERSION FOR LAND SEISMIC DATA NORTHERN WESTERN DESERT, EGYPT. EKB Journal Management System, 15(1), 89-95. doi: 10.21608/jegs.2017.385698
A. El-Werr; M.M.F. Shokry; A. Shebl; A. Elmidany. "POST-STACK SEISMIC INVERSION FOR LAND SEISMIC DATA NORTHERN WESTERN DESERT, EGYPT". EKB Journal Management System, 15, 1, 2017, 89-95. doi: 10.21608/jegs.2017.385698
El-Werr, A., Shokry, M., Shebl, A., Elmidany, A. (2017). 'POST-STACK SEISMIC INVERSION FOR LAND SEISMIC DATA NORTHERN WESTERN DESERT, EGYPT', EKB Journal Management System, 15(1), pp. 89-95. doi: 10.21608/jegs.2017.385698
El-Werr, A., Shokry, M., Shebl, A., Elmidany, A. POST-STACK SEISMIC INVERSION FOR LAND SEISMIC DATA NORTHERN WESTERN DESERT, EGYPT. EKB Journal Management System, 2017; 15(1): 89-95. doi: 10.21608/jegs.2017.385698

POST-STACK SEISMIC INVERSION FOR LAND SEISMIC DATA NORTHERN WESTERN DESERT, EGYPT

Journal of Egyptian Geophysical Society
Volume 15, Issue 1, 2017, Page 89-95  XML PDF (3.6 MB)
Document Type: Original Article
DOI: 10.21608/jegs.2017.385698
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Authors
A. El-Werr1; M.M.F. Shokry1; A. Shebl1; A. Elmidany2
11- Geophysics Department, Faculty of Science, Ain Shams University
22- Senior Field Geophysicist at Arabian Gas Seismic Company, KSA
Abstract
Post stack seismic inversion is the procedure for extracting underlying model of the physical
characteristics of rocks and fluids. It is used to estimate the physical properties of the rocks by combining seismic and
well logs data. Post stack seismic inversion has proven to be very useful theory in the detection of the hydrocarbon
occurrences and lithological definition in the area of study. Lower acoustic impedance anomaly was very clear
confirming the hydrocarbon occurrences at the zone of interest in our study area which is Alam El Bueib 3G reservoir
member. Also, this approach was very helpful in the detection of higher acoustic impedance anomaly at the level of
Alamein Formation due to the presence of dolomite and shale as seal rocks.
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