COMMODITIES IT DISCRIMINATES (9)
What this layer helps you find
Conventional, tight & heavy multilateral oilNatural gas & condensate (Montney, Duvernay, Deep Basin)Crude bitumen (oil sands)Lithium (oilfield brines)HeliumGeothermal heat & powerCO2 pore space (carbon storage)Sulphur (by-product)Coalbed methane
Prospectivity envelopes citing this dataset (9)
- Leduc reef trend (Rimbey–Meadowbrook–Clearwater)Lithium (oilfield brines) · Lithium-enriched Devonian carbonate formation brine (DLE target)Profile ↗
- Peace River Arch / Worsley helium fairwayHelium · Basement-sourced helium trapped in Devonian / Cambrian reservoirs on a basement highProfile ↗
- Deep basin thermal maximum (Hinton–Fox Creek–Grande Prairie)Geothermal heat & power · Hot sedimentary aquifer (Leduc, Swan Hills, Granite Wash) and closed-loop targetsProfile ↗
- Industrial Heartland Basal Cambrian SandstoneCO2 pore space (carbon storage) · Deep saline aquifer storage (Basal Cambrian Sandstone, Leduc, Nisku)Profile ↗
- Montney (Alberta side)Natural gas & condensate (Montney, Duvernay, Deep Basin) · Tight siltstone liquids-rich gas, multi-stage fractured horizontalsProfile ↗
- Duvernay (Kaybob and East Shale Basin)Conventional, tight & heavy multilateral oil · Devonian organic-rich shale — condensate / light oil resource playProfile ↗
- Clearwater heavy-oil play (Marten Hills–Nipisi)Conventional, tight & heavy multilateral oil · Shallow Cretaceous heavy oil produced with multilateral unstimulated horizontalsProfile ↗
- Foothills sour-gas belt (Caroline–Waterton)Sulphur (by-product) · By-product elemental sulphur from deep Devonian–Mississippian sour gasProfile ↗
- Horseshoe Canyon dry CBM fairwayCoalbed methane · Dry (no water) coalbed methane in Upper Cretaceous coal zonesProfile ↗