Carbonate Reservoir Rocks
This core workshop is the product of an effort by the SEPM Carbonate Research Group to emphasize the value of careful core interpretation to hydrocarbon exploration and production programs. Initially conceived as a small conference the format was expanded in response to strong interest from the geologic community. The end result was a workshop including 14 core displays. The notes were intended as a guide but the thorough documentation of these cores will be of interest to many others.
Gas Reservoirs in Stuart City Trend Along Lower Cretaceous Shelf Margin in South Texas1
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Published:January 01, 1980
Abstract
A complex of reefs, banks, tidal bars, channel fills, and stabilized grainflats accumulated along the Lower Cretaceous shelf margin in South Texas. The wide range of energy levels along this shelf-margin complex resulted in deposition of numerous facies, some with initial porosities as great as 30 to 40 percent. Subsequent marine cementation, meteoric phreatic diagenesis, and deep subsurface cementation have generally filled pore spaces and blocked permeability within the limestone. Only four facies commonly have greater than 5 percent porosity and 5 milli-darcys permeability--the algae encrusted miliolid-coral-caprinid pack-stone, mollusk grainstone, rudist grainstone, and coral-stromatoporoid boundstone.
Intraparticle porosity is common in several wackestone facies but only locally reaches 20 percent; permeability, however, is generally low in these intervals. Interparticle and fracture porosity are also locally significant. Where interparticle porosity is greater than 5 percent, permeability reaches 10 millidarcys. Higher permeability always occurs where fractures are common.
Stuart City gas fields are facies-controlled stratigraphic traps. Gas is present within common intraparticle and moldic porosities, which are best preserved in the four depositional facies listed above. Fractures provide the effective gas collecting network in the Stuart City reservoirs. Relatively rapid decline in gas production from many wells, response to fracture enhancement, and decreased water production with time supports the importance of fractures to gas production.