The November 2026 field program by Québec Innovative Materials Corp. (QIMC) focused on the New Salem zone within the western Cumberland Basin, Nova Scotia. A single contiguous traversal of roughly 1.5 kilometres was sampled, producing a tightly spaced dataset of 28 soil-gas stations at ~50-metre intervals. The work targeted the faulted contact between the Rapid Brook (Horton Group) and Ragged Reef (Cumberland Group) Formations and collected material using GeoFrontiers-supplied equipment to minimize contamination and ensure reproducible results.
The survey revealed a coherent hydrocarbon footprint and a persistent helium elevation across the corridor. A 450 m continuous anomaly containing methane (C1) together with significant ethane, propane and butane (C2–C4) components was mapped across eight stations inside exploration license EL56912. Independent laboratory analyses were completed by GeoFrontiers Corporation (Texas), which used high-sensitivity gas chromatography to quantify the volatile constituents and helium, providing an external quality check on the field program.
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Key analytical highlights and anomaly geometry
The soil-gas array produced distinct concentration peaks and spatially coherent signatures. A peak methane value of 87.68 ppmv was recorded at station QIMC-ARE-1050. Overall, 12 of 28 stations reported methane above 5.0 ppmv, and a run of seven consecutive stations displayed methane between 5.7 ppmv and 87.7 ppmv, consistent with a connected subsurface source rather than isolated near-surface generation. The survey-wide mean methane concentration was 8.99 ppmv.
Heavier hydrocarbons and thermogenic indications
Along the methane corridor, the presence of heavier hydrocarbons was notable: peak ethane (C2) reached 1.61 ppmv, propane (C3) peaked at 0.503 ppmv, and combined butanes (C4) peaked at 0.211 ppmv, with a maximum combined C2–C4 fraction of 2.31 ppmv. The relative proportions and low methane-to-(ethane+propane) ratios observed across the anomaly are more consistent with a thermogenic contribution than with shallow biogenic methane produced by soil organic decay, supporting the interpretation of a deeper hydrocarbon source.
Helium response and independent verification
Every collected sample showed helium above the quoted atmospheric baseline of 5.240 ppmv. Values ranged from 5.306 ppmv to 5.722 ppmv, with a survey mean of 5.456 ppmv — roughly a 4.0% average anomaly over background and a maximum exceeding 10.8%. Because helium is commonly used as a tracer of deep crustal or mantle-linked fluid pathways, a consistent above-background helium footprint across all stations suggests widespread diffusive migration to the near surface rather than isolated shallow sources.
Laboratory quality control
All 28 samples were shipped to GeoFrontiers Corporation in Texas for independent analysis via gas chromatography. GeoFrontiers performed quantification of C1–C4 hydrocarbons and helium with calibrated multi-detector systems and provided verification of sampling integrity. QIMC emphasizes that this external verification is central to the technical confidence in the dataset and supports the interpretation of the mapped anomalies.
Context, interpretation and next steps
QIMC’s management views the results as the successful completion of Stage 1 of its proprietary R2G2 exploration workflow, a staged method that integrates near-surface geochemistry, geophysics, structural geology and subsurface modeling to define drill-ready targets. CEO John Karagiannidis noted that the scale and consistency of the multi-analyte corridor justify targeted follow-up work, including additional geochemical transects, focused geophysics and drill-target definition inside EL56912.
Scientific commentary from Professor Marc Richer Lafleche (INRS) places these findings in a broader regional frame. As part of QIMC’s 2026 hydrogen exploration program, the area around New Salem was expanded for soil-gas work and revealed enriched volatile organics. Professor Lafleche emphasized that while surface gas surveys cannot quantify subsurface volumes, they are powerful for narrowing the footprint and de-risking follow-up seismic and drilling efforts. Regional geology — including organic-rich lacustrine and coal-bearing strata with mixed Type II–III kerogen and maturity consistent with thermogenic gas generation — provides a plausible source for the observed signals.
Given the data, QIMC plans to advance the New Salem corridor toward Stage 2 activities: targeted geochemical grids, higher-resolution geophysics and eventual drill testing of defined anomalies. The company will continue to report progress as work moves forward and aims to refine the dual-commodity thesis that couples potential hydrocarbon/condensate systems with helium optionality in the western Cumberland Basin.
