Figure 5. Results of seismic facies analysis for the Upper Jurassic interval. Four types of seismic facies Figure 5. Results of seismic facies analysis for the Upper Jurassic interval. Four types of seismic facies were described and linked with the main sedimentary environments: (1) A—bedded seismic facies were described and linked with the main sedimentary environments: (1) A—bedded seismic facies related to bedded facies of the inter- and intra-buildup sub-basins (2) B—mound-shaped refers to related to bedded facies of the inter- and intra-buildup sub-basins (2) B—mound-shaped refers to carbonate buildups, (3) C—contorted-chaotic observed at the cores of carbonate buildups, (4) D— carbonate buildups, (3) C—contorted-chaotic observed at the cores of carbonate buildups, (4) D—chaotic chaotic seismic facies associated with talus or with deposits of the gravity mass-flows. seismic facies associated with talus or with deposits of the gravity Seismic facies type A is very common within the entire study area, and was termed the bedded seismic facies (Figure 5). This type is most pronounced within the upper parts of the Upper Jurassic