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Three-dimensional Outcrop Reservoir Analog Model: A Case Study of the Upper Khuff Formation Oolitic Carbonates, Central Saudi Arabia

Start Date: August 23, 2017 - 04:15 PM
End Date: August 23, 2017 - 05:15 PM

​By Hassan Eltom ​
University of Kansas, Lawrence, USA
Host: Prof. Volker Vahrenkamp​
Venue: Lecture Hall 1 (2322), Engineering and Science Hall (Building 9)

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​Abstract:
 Oolitic grainstones can contain significant hydrocarbon reserves. Due to variations in sedimentary processes and diagenetic alteration, the porosity and permeability values of these deposits are highly variable. We identified potential reservoir units in the Upper Khuff Formation in central Saudi Arabia using an outcrop analog model by incorporating outcrop porosity and permeability information into oolitic grainstone facies in a three dimensional (3D) framework. Our results predict reservoir potential in subsurface Khuff equivalent and elsewhere. 
Six major surfaces representing fourth-order sequence boundaries were identified in outcrop, and these separate a five zones in the 3D outcrop model. In terms of depositional environments, these are defined as Zones 1 and 2 (subtidal and sand sheets deposits in a shoal complex), Zones 3 and 4 (sand sheets and lenses deposits in a back shoal), and Zone 5 (tidal flat). The population of lithofacies with in each zone in the 3D outcrop model was performed separately using a different geostatistical algorithm. The resulting 3D facies model adequately illustrates the continuity of beds and fairly represents the stratigraphic architecture observed in outcrop. The 3D volume of the outcrop model was subdivided into three broad stratigraphic intervals. The lower interval (Zones 1 and 2) was deposited during a rapid sea-level rise at the Permian–Triassic transition and consists dominantly of oolitic units with oomoldic and interparticle porosity. The middle interval (Zones 3 and 4) was deposited during an interval of rapid sea-level fluctuation and is characterized by the appearance of marine fauna after a long-term extinction in the lower Triassic interval. The dominant porosity types within this interval are moldic, interparticle, and intraskeletal. The upper interval (Zone 5) was deposited during a major sea-level regression. This interval contains a significant amount of early diagenetic dolomite and is dominated by interparticle and intercrystalline porosity. The results demonstrate that including porosity values from outcrop measurements in a 3D outcrop facies model can provide more accurate visualizations of reservoir units. This methodology could be used to predict reservoir potential in analogous carbonate reservoirs.


 Bio:
Hassan Eltom graduated from Khartoum University (Sudan) in 2001 with BSc degrees in Geology and Chemistry. He earned MSc and PhD degrees in Geology from King Fahd University of Petroleum and Minerals (KFUPM) in Dhahran, Saudi Arabia. His PhD is about an outcrop analog of the Arab-D reservoir in Saudi Arabia. Hassan has a total of 12 years of experience integrating field, lab, and modeling techniques to better understand past paleoenvironments and paleoceanography through study of ancient carbonate strata. Hassan experience includes four years with Schlumberger overseas as a Borehole Geologist and four years with KFUPM as a researcher. Currently, Hassan is working with Kansas Carbonate Interdisciplinary Carbonate Consortium (KICC) as a researcher, a post he holds since 2014.  Hassan has been involved in and led research activities including the investigations of Paleozoic and Cenozoic carbonates of Saudi Arabia, Sudan, and Kansas. His research interests include carbonate sedimentology, stratigraphy and geochemistry and the characterization and modeling of reservoirs based on outcrop analog and 3-D geostatistical modeling.