Abstract
This research study attempt to evaluate the hydrocarbon potentials, thermal and burial history and the timing of hydrocarbon generation in Herwa-1 well within the Nigerian Sector of the Chad basin. Organic geochemical study of some ditch cuttings samples from Herwa-1 well and a One-dimensional basin modeling study was carried out. The result of the geochemical analysis revealed a moderate to good TOC greater than 0.5wt% in Fika and Gongila formation, the Hydrogen Index (HI) ranges from 150-300 (mgHC/g) and the Tmax values falls within the range of greater than or equal to 430°C. The hydrocarbon potentials in Herwa-1 well was further supported with the values of S1+S2 which is greater than or equal to 2 mg/g of rock in almost all the samples, suggesting a good hydrocarbon potentials. The 1-D basin model was constructed for Herwa-1 well in order to assess the burial history and thermal maturity of the potential source rocks in the Nigerian sector of the Chad basin. The modeling results indicate that maximum burial occurred in the late Miocene and suggesting erosion might have been the cause of the thinning of the Tertiary sediments in the present time. The calibration of Vitrinite reflectance against Temperature revealed the present day heat flow to be at 60 mW/m<sup>2</sup> and Paleo heat flow falls within the range of 68 mW/m<sup>2</sup>. However, it is also revealed that Oil Window begins at (0.60-1.30% VRr) at the depth of (2000-3000 m) in the middle Cretaceous and the Gas Window start during the late Cretaceous to Tertiary with a value of (1.3-2.5% VRr) at a depth greater than (3500 m).
Highlights
Nigerian Sector of the Chad Basin is part of the Western Central African rift system, which was formed during the separation of African and South American plates in the cretaceous
The Nigerian Sector of the Chad basin is among the Nigerian inland basins occupying the north eastern part of Nigeria as seen in Fig. 1, it covers at least one tenth of the total area extent of the Chad basin
Significant discoveries of commercial hydrocarbon accumulation have been made on either side of the of the Nigerian sector of the Chad basin, such as Doba basin in the Chad republic and the Termit agadem basin in the republic of Niger, the source rocks contributing to the hydrocarbon generation in this basins were correlatable and similar to it counterpart Bima sandstone in the Nigerian sector of the Chad basin (Obaje et al, 1999, 2004)
Summary
Nigerian Sector of the Chad Basin is part of the Western Central African rift system, which was formed during the separation of African and South American plates in the cretaceous. Little or none has been presented on the burial history and thermal maturity of the potential source.
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