MODELING GAS MIGRATION, DISTRIBUTION, AND SATURATION IN A STRUCTURALLY AND PETROLOGICALLY EVOLVING TIGHT GAS RESERVOIR
In the NW German Basin tight gas accumulations are found in conventional traps in sub-Zechstein Carboniferous Westphalian C & D reservoirs (porosity < 10%, permeability near 50 microdarcies). Top seal is provided by the Zechstein evaporites. Westphalian A and B coals are the primary source for methane-rich gas. The complex structural history includes contractional tectonics at the end of the Variscan Orogeny, extension-related subsidence, and Late Jurassic to Early Cretaceous, and Late Cretaceous contractional inversion. The reservoir received multiple charges as the various sources matured.
The basin model is initialized at the base of the Namurian. Changes in the three-dimensional structural configuration, porosity, and permeability are modeled in 5 million year increments to present. The basin model outputs are imported to the migration software, which is run in a dynamic mode. Dynamic mode allows investigation of the impact of trap structural reconfigurations and multiple charges on the final distribution and saturations of gas in the traps.
The outcome of the basin and migration modeling shows reasonable fidelity with known drilling results in the Carboniferous tight gas reservoir. Accumulations are predicted where they are known to exist, and there is a good match between predicted areas of moderate (40-60%) and high (>60%) gas saturations and the wells that penetrate those areas and have similar saturations. While the results are promising, more test cases with good calibration will be required before full confidence in the methodology is gained.