Fig. 5From: Geothermal exploration in a sedimentary basin: new continuous temperature data and physical rock properties from northern OmanT-logs and T-gradient plotted versus depth for six of the analyzed boreholes, additionally the litho-stratigraphic logs are given and for three wells gamma ray logs (provided by MRMWR). The mean T-gradient for each well is given below the curves. The NB-19 and the RGS2-L well show conductive conditions were changes in the T-gradient correlate with changes in the litho-stratigraphic log. Six intervals (black bar) were chosen to calculate the surface heat flow (Table 3). For location of the boreholes see Figs. 1, 2Back to article page