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South Africa - Inkaba.org

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Comparing 1960’s Karoo basin seismic data with recent data<br />

(<strong>Inkaba</strong> ye<strong>Africa</strong> Line), to identify and correlate Karoo seismic<br />

stratigraphy on a more regional basis<br />

1 Lynise Esterhuizen, 2 Ge<strong>org</strong>e Smith<br />

1 Department of Geological Sciences, University of Cape Town, Rondebosch 7701, <strong>South</strong> <strong>Africa</strong><br />

lynise04@hotmail.co.za,<br />

2 Department of Geological Sciences, University of Cape Town, Rondebosch 7701, <strong>South</strong> <strong>Africa</strong><br />

ge<strong>org</strong>e.smith@uct.ac.za<br />

ABSTRACT<br />

The project entails comparing 1960’s Karoo basin seismic data with recent data (<strong>Inkaba</strong> ye<strong>Africa</strong> Line), to identify<br />

and correlate Karoo seismic stratigraphy on a more regional basis.<br />

Due to the recent interest in shale gas exploration in the Karoo basin of <strong>South</strong> <strong>Africa</strong>, there is an interest in reinterpreting<br />

old 1960's seismic lines of SOEKOR (now archived by PASA). This project entails comparing these<br />

lines with a recent <strong>Inkaba</strong> ye<strong>Africa</strong> near vertical reflection line across the southern Karoo Basin (Lindeque, 2008),<br />

and tying the reflections to the known litho-stratigraphy, based on outcrop mapping and borehole data. It forms<br />

part of a shale gas project to identify the location and depths of the Whitehill and Prince Albert Formations. The<br />

differences in appearance and quality between the old and new data are outlined.<br />

The old Karoo seismic images are of poor quality, but were enhanced by two-dimensional convolutional filtering.<br />

Thereafter, the sections were re-interpreted using the recent seismic data and existing well-data as a guide.<br />

The <strong>Inkaba</strong> ye<strong>Africa</strong> seismic line shows much deeper penetration, with depths of up to 50km through the crust and<br />

across the Moho. The older data only shows the upper most crustal layers down to approximately 10km.<br />

The comparison of the two sets of data shows the differences in processing and how seismic acquisition quality has<br />

improved since the early 1960's. The data also indicate where the old data can still be of good use after significant<br />

but time-consuming enhancement using modern filtering techniques.<br />

Reference:<br />

Lindeque, A.S, 2008, Deep Crustal profile across the southern Karoo Basin, <strong>South</strong> <strong>Africa</strong>, Unpublished Masters Thesis in the<br />

Department of Geological Sciences, University of Cape Town<br />

KEYWORDS: Karoo basin, seismic data, image enhancement<br />

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