In addition to these faults, there are also faults with variable directions between east-west and northeast-southwest, that divide the basin into different tectonic-sedimentary areas, that could have influenced sediment deposition during Mesozoic.
Furthermore, in addition to these defects, there are irregularities in the direction of faults that run both east-west and northeast-southwest, dividing the basin into separate areas characterized by different geological formations, which may have impacted sedimentation patterns during the Mesozoic period.