Browsing Faculty of Natural Science by Author "Carey, Paul F."
Now showing items 1-5 of 5
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Comparative study of the chemostratigraphic and petrophysical characteristics of wells A-A1, A-L1, A-U1 and A-I1 in the Orange Basin, South Atlantic Margin, Offshore South Africa
Bailey, Carlynne (University of the Western Cape, 2009)Many hydrocarbon reservoirs are situated in barren sequences that display poor stratigraphic control. Correlation between the wells can become extremely difficult and traditional correlation techniques can prove to be ... -
The petrophysical analysis and evaluation of hydrocarbon potential of sandstone units in the Bredasdorp Central Basin
Olajide, Oluseyi (University of the Western Cape, 2005)This research was aimed at employing the broad use of petrophysical analysis and reservoir modelling techniques to explore the petroleum resources in the sandstone units of deep marine play in the Bredasdorp Basin. -
Porosity and permeability distribution in the deep marine play of the central Bredasdorp Basin, Block 9, offshore South Africa
Ojongokpoko, Hanson Mbi (University of the Western Cape, 2006)This study described porosity and permeability distribution in the deep marine play of the central Bredasdorp Basin, Block 9, offshore South Africa using methods that include thin section petrography, X-ray diffraction, ... -
Porosity and Permeability Distribution in the Deep Marine Play of the Central Bredasdorp Basin, Block 9, Offshore South Africa
OJongokpoko, Hanson Mbi (University of the Western Cape, 2006)This study describes porosity and permeability distribution in the deep marine play of the central Bredasdorp Basin, Block 9, offshore South Africa using methods that include thin section petrography, X-ray diffraction, ... -
Sequence stratigraphic characterisation of petroleum reservoirs in Block 11b/12b of the Southern Outeniqua Basin
Nfor, Nformi Emmanuel (University of the Western Cape, 2011)The main purpose of this study was to identify and characterize the various sand prone depositional facies in the deepwater Southern Outeniqua Basin which generally tend to form during lowstand (marine regression) conditions ...