Using our extensive subsurface knowledge and GIS capabilities, CDL has established workflows to evaluate carbon sequestration targets and answer the key questions: Is there a storage opportunity? Is the storage capacity of the CCUS opportunity large enough to sequester the CO2 in the given time frame? Is the storage opportunity suitable?
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CDL's deep understanding of depositional environments and fluid interactions in the subsurface has been our core competency for nearly 35 years and we are using this foundation to strategically deliver CCUS site identification, Deep Geothermal and Critical Mineral assessments to clients world-wide.
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The objective of this study is to determine the hydrogeologic framework of the Granite Wash Formation (and equivalent Keg River sand, Chinchaga sand and Keg River Carbonates) in the Boyer area and its relationship to the northern fringe of the Peace River Arch. The Keg River and Chinchaga sands diachronous deposits occur at stratigraphically similar positions on the Precambrian basement surface surrounding the Peace River Arch. The Keg River Carbonates are the stratigraphic equivalent of the Keg River Sands,