The Leduc Formation consists of fossil reefs that are highly porous, which makes them excellent reservoirs for oil and gas. They were deposited as limestone and mudstone in shallow water reef environments. Stromatoporoids were the primary reef-building organisms, and rock-types range from skeletal mudstones and floatstones to finer grained muddy packstones and wackestones. Many, but not all, of the reefs were later subjected to dolomitization during diagenesis, which increased their porosity, and they now consist of dolomite rather than limestone. The dolomitization that took place in the region has increased the porosity primarily in the more deeply buried lagoonal back reef facies. The pre-existing porosity has also been preserved well due to the dolomitization. Porosity in the region is dominated by vuggy, moldic, intercrystalline, as well as fracture types of porosity. Generally, the mean porosity of the Leduc Formation is 5.2%, with the permeability of the rocks in the region being an even spread. Anhydrite is also common in the Leduc Formation, along with the replacement dolomitization.
The Leduc Formation is a major source of oil and natural gas in central Alberta. The Leduc No. 1 well drilled in 1947 produced 50 thousand cubic metres of oil, marking the beginning of the post-war Albertan oil boom, and contributed to a large population boom in the cities of Calgary and Edmonton. The discovery and subsequent production from the wells also led to an economic boom in Alberta, which now puts Calgary among the forefront of producers of oil in North America. The Strachan and Ricinus West gas fields, discovered in 1967 and 1969, are also in Late Devonian Leduc-age reefs. The reefs were found using seismic common-depth point techniques, which were being developed and used in the Western CanadaSedimentary Basin. The well that was crucial to the discovery of these two formations was drilled in 1955, and yielded gas as well as some salt water. Reef buildup of the Strachan and Ricinus gas field reefs are and respectively.
Distribution and thickness
The Leduc Formation occurs as discrete, discontinuous reef "buildups" in a line following the Woodbend shelf margin from Drumheller in central Alberta to the Peace River Arch area in northern Alberta. The formation is absent in inter-reef areas, and buildups can reach from to in thickness.
Relationship to other units
In central Alberta the Leduc Formation conformably overlies the platform limestones and dolomites of the Cooking Lake and Beaverhill Lake Formations. In northern Alberta near the Peace River Arch it rests on older red beds or on the Granite Wash. The Leduc reefs are surrounded by shales of the Duvernay and Ireton Formations and the Woodbend Group that were deposited in non-reefal, open marine environments. The Leduc reefs are the same ages as, but not contiguous with, the reefs of the Cairn Formation farther west. Because the Leduc reefs are not exposed at the surface, the extensive outcrops of the Cairn reefs in the Canadian Rockies have been studied to increase the understanding of the Leduc reefs. Near the Leduc Formation there is also the Swan Hills Formation. These two formations hold some similarities, such as the types of rocks and certain diagenetic processes. Rock types in both regions are dominated by limestones and dolomites. Dolomitization has taken place in both formations however it is more dominant in the Leduc Formation. Evaporites such as Anhydrites are also more present in the Leduc Formation, however they are also present in the Swan Hills Formation. The Swan Hills formation also holds some differences to the Leduc Formation. The porosity types in both formations differ, and the types of fossilized biota also differ. Vuggy, moldic, intercrystalline, and fracture porosities are present in the Leduc Formation whereas the primary porosities in the Swan Hills Formation are interparticle and interfossil. One of the primary fossilized biota in the Leduc Formation are stromatoporoids, whereas the primary fossil type in the Swan Hills Formation are Amphipora.
