Figure9. B-B’ section: Early Jurassic half graben systems controlling deposition of Toarcian strata on the Tunisian shelf in the Gulf of Tunis. Note the Triassic structural style. Position of early Toarcian strata only approximated. For location, see Figure 4. Interpretation is based mainly on the existing well data and on the NW-SE regional seismic section

From

A Review of Jurassic Oceanic Anoxic Events as Recorded in the Northern Margin of Africa, Tunisia

Mohamed Soua

Journal of Geosciences and Geomatics. 2014, 2(3), 94-106 doi:10.12691/jgg-2-3-4