New insights on source rock maturation in the southern Gulf of Gabes (Tunisia) via 1-D modeling: effect of combined corrected borehole temperature and thermal conductivity on heat flow distribution

Organic geochemical study of Permian series from the Jeffara and Dahar areas (Southern Tunisia): Identification and characterization of a Tunisian Permian source rock

“…This was confirmed through the variation of geothermal flux, identified in the region compared to the average geothermal gradient. In fact, the distribution of the geothermal flux in terms of "heat-flow density" (HFD) at the level of the Mediterranean basin and, in particular, at the southern segment of the Geotraverse (EGT-S) campaign, shows a heat flux anomaly superior than 100 MW/m 2 in the Jeffara region (Bouaziz et al, 2015;Gabtni., 2006;Mraidi et al;Fig. 12 (C)).…”