The Upper Devonian Duvernay Formation represents one of the most important sources of conventional oil within the Western Canada Sedimentary Basin. It is an organic-rich, basinal shale and limestone sequence within the Upper Devonian Woodbend Group. Several lithofacies from the Duvernay Formation have been identified in this study. This study concentrated on the shales and mudstones of the Duvernay Formation. The terrestrial material is probably derived from the area to the north or northwest. The major diagenetic processes that affected shales and mudstones lithofacies are cementation, dolomitization and pyritization. Minor processes include physical compaction, dissolution, anhydritization and fracturing. Framboidal pyrite, non-ferroan ca...
The Fairholme carbonate complex is part of the extensively dolomitized Upper Devonian carbonate reef...
The reservoir properties of the Duvernay Formation mudrock gas and oil (“shale gas”) reservoir in Al...
Dolostone gas reservoirs in the Devonian west-central Alberta deep basin exist at three stratigraphi...
The Middle Devonian carbonates of the Sulphur Point Formation, Rainbow South Field, northwestern Alb...
The Middle Devonian carbonates of the Slave Point Formation, Hamburg Field, northwestern Alberta, ar...
The Upper Devonian (Famennian)-Lower Carboniferous (Tournaisian) Exshaw Formation is a thin, lateral...
This paper characterizes organic matter in the mixed hydrocarbon (oil-dry gas, oil-condensate) produ...
The Late Devonian Duvernay Formation is characterized by organic-rich mudrocks, argillaceous carbona...
The natural gas reservoir of the Pine Creek Field lies exclusively within the Normandville Member of...
Integrated petrographic, geochemical and fluid inclusion study of fracture mineralization in Mississ...
The Upper Devonian Big Valley Formation in southern Alberta is a 10-m thick carbonate succession, un...
Upper Devonian (Frasnian) stromatoporoid and coral buildups in the Alberta Basin are among the most ...
The Nisku Formation in the Alberta subsurface consists of bank facies, reefal facies, and basinal/sl...
Dolomitization of Leduc Formation (Upper Devonian) along the southern part of the Rimbey-Meadowbrook...
The Fairholme carbonate complex is part of the extensively dolomitized Upper Devonian carbonate reef...
The Fairholme carbonate complex is part of the extensively dolomitized Upper Devonian carbonate reef...
The reservoir properties of the Duvernay Formation mudrock gas and oil (“shale gas”) reservoir in Al...
Dolostone gas reservoirs in the Devonian west-central Alberta deep basin exist at three stratigraphi...
The Middle Devonian carbonates of the Sulphur Point Formation, Rainbow South Field, northwestern Alb...
The Middle Devonian carbonates of the Slave Point Formation, Hamburg Field, northwestern Alberta, ar...
The Upper Devonian (Famennian)-Lower Carboniferous (Tournaisian) Exshaw Formation is a thin, lateral...
This paper characterizes organic matter in the mixed hydrocarbon (oil-dry gas, oil-condensate) produ...
The Late Devonian Duvernay Formation is characterized by organic-rich mudrocks, argillaceous carbona...
The natural gas reservoir of the Pine Creek Field lies exclusively within the Normandville Member of...
Integrated petrographic, geochemical and fluid inclusion study of fracture mineralization in Mississ...
The Upper Devonian Big Valley Formation in southern Alberta is a 10-m thick carbonate succession, un...
Upper Devonian (Frasnian) stromatoporoid and coral buildups in the Alberta Basin are among the most ...
The Nisku Formation in the Alberta subsurface consists of bank facies, reefal facies, and basinal/sl...
Dolomitization of Leduc Formation (Upper Devonian) along the southern part of the Rimbey-Meadowbrook...
The Fairholme carbonate complex is part of the extensively dolomitized Upper Devonian carbonate reef...
The Fairholme carbonate complex is part of the extensively dolomitized Upper Devonian carbonate reef...
The reservoir properties of the Duvernay Formation mudrock gas and oil (“shale gas”) reservoir in Al...
Dolostone gas reservoirs in the Devonian west-central Alberta deep basin exist at three stratigraphi...