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Natural hydrocarbon accumulation related to formation overpressured interval; study case is the Saharan platform (Southern Tunisia)

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Abstract

Organic geochemistry analysis and formation fluid overpressure study have been performed on several oil well data located to the northern part of the Ghadames Basin (southern Tunisia Saharan platform). The main results of this work highlight the important role of overpressured interval in hydrocarbon accumulation. In fact, the analysis of the Paleozoic–Mesozoic petroleum systems in Southern Tunisia shows that the hydrocarbons generated by Ordovician and Silurian source rocks migrate upward following fault systems or through the major Hercynian unconformity to finally accumulates in structural or stratigraphic traps. These migration pathways provide favorable conditions to fill up the Silurian, Devonian, or Triassic reservoirs. The overpressured zone located above Triassic reservoir constitutes a continuous and efficient seal to hydrocarbon trap structures. So the overpressure plays the role of hydraulic seal advantaging oil and gas accumulation in the Ghadames Basin associated with the impermeable (evaporites) and then stopping any upward migration of natural hydrocarbon.

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Acknowledgements

This work was supported by Research Unit: GEOGLOB (code: 03/UR/10-02), Science Faculty of Sfax and Hydroscience Appliqués (06/UR/10-03), Higher Institutes of Water Sciences and Techniques of Gabes and Laboratory Water, Energy and Environment (LR3E). Special thanks go to the National Company of Petroleum in Tunisia (ETAP) for the effective contribution in this work by geochemical analysis and data. We also thank the two anonymous reviewers for their valuable recommendations, whose implementation greatly improved the initial manuscript.

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Correspondence to Dhaou Akrout.

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Akrout, D., Ahmadi, R., Mercier, E. et al. Natural hydrocarbon accumulation related to formation overpressured interval; study case is the Saharan platform (Southern Tunisia). Arab J Geosci 5, 849–857 (2012). https://doi.org/10.1007/s12517-011-0287-6

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