Deformation, Fluid Flow, and Reservoir Appraisal in Foreland Fold and Thrust Belts

Several topics are covered including: *the use of hydrocarbon-bearing fluid inclusions and apatite fission tracks as paleothermometers for reconstructing P-T evolution of subthrust reservoirs *the use of hydrocarbon-bearing fluid inclusions and apatite fission tracks as paleothermometers for reconstructing P-T evolution of subthrust reservoirs *the coupling of kinematic and thermal modeling performed to trace the burial (P-T) evolution of potential source rocks and reservoirs in three cases studies in the southern Apennines, Colombia, and Pakistan *analytical results and integrated studies, which link deformation and fluid circulation in various fold and thrust belts, with the Sierra Madre in Mexico, the Central Brooks Range, the Arctic in Alaska, the Coastal belt in northern Spain, and the Ukraine featured. Links between deformation, fluid flow, diagenesis, and reservoir characteristics are discussed in depth and descriptions of petrographic techniques integrated with basin modeling are discussed in case studies for carbonate reservoirs in the Apennines, the Canadian Rockies, and the Polish Carpathians, and for sandstone reservoirs in Eastern Venezuela. Sixteen of the twenty-one chapters illustrate the influence of thrust-belt evolution on regional petroleum systems. The petroleum potential in the Tunisian Atlas and in Sicily, close to where the Hedberg Conference and post-conference field trip were held, is described. An older example is documented, for the Gaspé Appalachians, where multiphase Paleozoic deformation had a strong control on the burial history of potential source rocks, petroleum generation and migration, and oil charge of the traps. As the first in the brand-new Hedberg Series of publications, this volume is a comprehensive look at understanding petroleum systems in fold and thrust belts.
The Effect of Hydrothermal Fluid Flow on Early Diagenetic Dolomitization: An Example from the Devonian Slave Point Formation, Northwest Alberta, Canada
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Published:January 01, 2004
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CiteCitation
Ihsan S. Al-Aasm, Julie D. Clarke, 2004. "The Effect of Hydrothermal Fluid Flow on Early Diagenetic Dolomitization: An Example from the Devonian Slave Point Formation, Northwest Alberta, Canada", Deformation, Fluid Flow, and Reservoir Appraisal in Foreland Fold and Thrust Belts, Rudy Swennen, François Roure, James W. Granath
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Abstract
The Middle Devonian carbonates of the Slave Point Formation, Hamburg field, northwestern Alberta, are composed mainly of stromatoporoid and Amphipora floatstones and rudstones, with interbedded mudstone and grainstone facies characteristic of deposition in open to slightly restricted marine platform environments. These carbonates have undergone a complex diagenetic history, from shallow to deep burial, as represented by fracturing, calcite cementation, silicification, and dolomitization.
Petrographically, four different types of dolomite have been identified (from early to late): (1) fine-crystalline matrix dolomite; (2) pseudomorphic dolomite; (3) medium-crystalline pervasive dolomite; and (4) saddle dolomite. Fine-crystalline dolomite (5–50 (μm) replaces the mud matrix and...
- Alberta
- basins
- Beaverhill Lake Group
- biostratigraphy
- calcite
- Canada
- carbonate rocks
- carbonates
- carbonatization
- cementation
- chemical composition
- clastic rocks
- Devonian
- diagenesis
- dolomitization
- dolostone
- early diagenesis
- Elk Point Group
- floatstone
- grainstone
- Invertebrata
- Middle Devonian
- mudstone
- natural gas
- Paleozoic
- Peace River Arch
- petroleum
- petroleum exploration
- platforms
- Porifera
- reservoir properties
- reservoir rocks
- rudstone
- sedimentary basins
- sedimentary rocks
- Slave Point Formation
- Stromatoporoidea
- structural traps
- traps
- Western Canada
- northwestern Alberta
- Hamburg Field