A 150 km length, 6-second deep, seismic line across the west central and north parts of the South Caspian Basin was used to construct quantitative dynamical, thermal and hydrocarbon evolution patterns. The depth of the west part of the 2-D section of the South Caspian Basin is almost 30 km. The computer program GEOPETII was used to provide quantitative evolution models. The procedure provided an opportunity to investigate the development dynamics of: excess fluid pressure, porosity retention, rock fracturing, compaction, heat transfer, maturity, generation pressure, kinetic hydrocarbon generation, migration and accumulation, together with solubility effects on hydrocarbon transport. The results suggest that: (i) Temperature is 350-400 degrees C in the deepest part of the section at a depth of 26-29 km; (ii) The highest values of excess pressure (nearly twice hydrostatic fluid pressure) are in Jurassic and Cretaceous formations in the west part of the section, which has now subsided to a depth of about 20-27 km; (iii) Major oil and gas generation began in the last 10-5 MYBP, the migration in free-phase and in water solution occurring dominantly in the last few million years; (iv) Trapping of hydrocarbons took place mainly, but not exclusively, in the 3-9 km depth interval in the sands of the Productive Series of the Pliocene, embedded in a shale sequence; (v) Oil and gas filling of the shallow reservoirs by oil and gas is on-going today, indicating an extremely high productivity for any reservoir found in the offshore area; (vi) There is overlap with depth of oil and gas reservoirs, and the total amount of hydrocarbons estimated to be trapped is considerable; (vii) The high overpressure expected makes for a drilling hazard, but one which it is worthwhile to overcome if the anticipated oil and gas accumulations are encountered. (C) 1998 Elsevier Science Ltd. All rights reserved.
