Diagenesis, compaction, and fluid chemistry modeling of a sandstone near a pressure seal: Lower Tuscaloosa Formation, Gulf Coast
- Pennsylvania State Univ., University Park, PA (United States)
Petrographic, isotopic, and fluid-inclusion evidence from normally and overpressured sandstones of the lower Tuscaloosa Formation (Upper Cretaceous) in the Gulf Coast documents quartz-overgrowth precipitation at 90{degrees}C or less, calcite cement precipitation at approximately 100{degrees} and 135{degrees}C, and prismatic quartz cement precipitation at about 125{degrees}C. Textural evidence suggests that carbonate cement dissolution occurred before the second phases of calcite and quartz precipitation, and was followed by precipitation of grain-rimming chlorite and pore-filling kaolinite. Geochemical calculations demonstrate that present-day lower Tuscaloosa Formation water from 5500 m depth could either dissolve or precipitate calcite cements in model simulations of upward water flow. Calcite dissolution or precipitation depends on P{sub CO{sub 2}} variability with depth (i.e., whether there is one or two-phase flow) or on the rate of generation of CO{sub 2} with depth. Calculations suggest that 10{sup 5}-10{sup 6} rock volumes of water are required to flow through the section to precipitate 1-10% calcite cement. Compaction analysis suggests that late-stage compaction occurred in normally pressured sandstones after dissolution of carbonate cements, but was hindered in overpressured sandstones despite the presence of high porosity. These results document the inhibition of compaction by overpressured fluids and constrain the timing of pressure seal formation. Modeling results demonstrate that the proposed paragenesis used to constrain timing of pressure seal formation is feasible, and that most of the cement diagenesis occurred before the pressure seal became effective as a permeability barrier.
- OSTI ID:
- 263030
- Journal Information:
- AAPG Bulletin, Journal Name: AAPG Bulletin Journal Issue: 7 Vol. 80; ISSN 0149-1423; ISSN AABUD2
- Country of Publication:
- United States
- Language:
- English
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Diagenesis as related to burial history, pressure regimes, and low-permeability zones in the upper Cretaceous lower Tuscaloosa Formation, Mississippi and Louisiana
Diagenesis as related to burial history, pressure regimes, and low-permeability zones in the upper Cretaceous lower Tuscaloosa Formation, Mississippi and Louisiana