* Late Cretaceous and [[Cenozoic]] siliciclastic sedimentation formed thick, [[Well_log_sequence_analysis#Parasequence_stacking_patterns|prograding]] prisms over the transitional crust and differentially loaded the Late Jurassic salt. The [[Deformation|deformed]] salt created anticlinal highs bordering sediment-filled [[Syncline|synclinal]] lows, which continued to subside and provide sediment transport pathways downslope. The deformation of the salt and associated sediments formed both structural and [[stratigraphic trap]]s within the siliciclastic section. Sedimentary burial and salt-thickness/mobility patterns affect [[Petroleum generation|hydrocarbon generation]] due to variations in the thermal conductivity of salt. Intersecting fault trends, one paralleling northwest–southeast-trending [[basement]] faults and a second associated with depositional strike-oriented [[growth fault]]s, provide vertical avenues for [[migration]] of hydrocarbons from deeply buried mature Mesozoic [[source rock]]s upward into reservoir rocks of Jurassic, Cretaceous, and Cenozoic age. | * Late Cretaceous and [[Cenozoic]] siliciclastic sedimentation formed thick, [[Well_log_sequence_analysis#Parasequence_stacking_patterns|prograding]] prisms over the transitional crust and differentially loaded the Late Jurassic salt. The [[Deformation|deformed]] salt created anticlinal highs bordering sediment-filled [[Syncline|synclinal]] lows, which continued to subside and provide sediment transport pathways downslope. The deformation of the salt and associated sediments formed both structural and [[stratigraphic trap]]s within the siliciclastic section. Sedimentary burial and salt-thickness/mobility patterns affect [[Petroleum generation|hydrocarbon generation]] due to variations in the thermal conductivity of salt. Intersecting fault trends, one paralleling northwest–southeast-trending [[basement]] faults and a second associated with depositional strike-oriented [[growth fault]]s, provide vertical avenues for [[migration]] of hydrocarbons from deeply buried mature Mesozoic [[source rock]]s upward into reservoir rocks of Jurassic, Cretaceous, and Cenozoic age. |