Abstract
This study present a microfacies approach to reservoir-related outcrop analog studies of the exposed discontinuous fringing rhodolith and coral reef complex of Wadi Waqb Member (Miocene Carbonate) of Jabal Kibrit formation in Midyan region, Saudi Arabia. Four facies were recognized as follows: MF-1) Proximal clastic facies comprises of calcallochemic sandstone MF-2) Upper reef front facies characterize by quartz-peloid packstone, and red algal bioclastic boundstone, and MF-3), Lower reef front facies compose of bioturbated rhodophyte-bioclastic grainstone, and MF-4) Fore reef facies comprise of intraclastic wackestone to mudstone. MF-1 represents a mixed carbonate-siliciclastic deposits with very good intergranular porosity preservation in outcrops. However, this porosity does not have any bearing on the Wadi Waqab main reservoir. The preserved primary intergranular and vuggy porosities in MF-2 and MF-3 are considered to be the main components of the Wadi Waqb reservoir. MF-4 possesses no visible porosity in thin section and therefore, does not have any bearing to the main reservoir.
Original language | English |
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Title of host publication | 79th Society of Exploration Geophysicists International Exposition and Annual Meeting 2009, SEG 2009 |
Publisher | Society of Exploration Geophysicists |
Pages | 4227-4232 |
Number of pages | 6 |
ISBN (Print) | 9781615675661 |
DOIs | |
State | Published - 2009 |
Publication series
Name | 79th Society of Exploration Geophysicists International Exposition and Annual Meeting 2009, SEG 2009 |
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Bibliographical note
Publisher Copyright:© 1996-2018 Society of Exploration Geophysicists All Rights Reserved.
ASJC Scopus subject areas
- Geophysics