Greenridge Exploration Completes Advanced 3D Inversion and Lithology Modelling Program at the Carpenter Lake Uranium Project
Advanced 3‑D modelling unlocks new drill targets across 15 km of strike at Carpenter Lake
Greenridge announced completion of an integrated 3‑D multi‑physics inversion and machine‑learning lithology modelling program for its Carpenter Lake uranium project. The effort combined historic VTEM, Falcon airborne gravity, high‑resolution magnetic data and 2025 drilling results to produce a unified geological framework. The model identified several high‑priority drill targets along more than 15 km of the Cable Bay Shear Zone (CBSZ) where conductive plates, density lows and favorable lithology intersect. Future work will use this model to guide the next drilling phase and includes a planned higher‑resolution ground gravity survey.
- New information: The modelling program delivers previously unavailable 3‑D target definition across a large strike length, directly informing drill‑site selection.
- Deviation from expectations: Prior updates (Jan 2026) only hinted at upcoming geophysical work; the concrete delivery of a detailed model and explicit high‑priority targets is an upgrade over earlier guidance.
- Potential upside: If the identified targets convert to drill intercepts, the project’s resource potential could increase substantially, improving Greenridge’s valuation.
- Risk considerations: The program does not yet contain assay results; success hinges on subsequent drilling performance and financing to execute the next phase.
Overall, the news is a material positive development—new, actionable data that can materially affect future cash flows but is not yet a game‑changing catalyst.
Greenridge Exploration Inc. is a Canadian explorer focused on uranium (Athabasca Basin) and critical base‑metal projects (nickel, copper, cobalt, PGEs). Its flagship uranium asset is the Carpenter Lake Project in the South Central Athabasca Basin, centered on the Cable Bay Shear Zone—a 15 km strike length of conductive, graphitic pelite horizons that are classic hosts for unconformity‑type uranium deposits.