Quebec Innovative Materials Corp. (QIMC) Confirms Third Major Natural Hydrogen Discovery In Nova Scotia With Soil-Gas Results Up To 4,125 Ppm

2025-09-22 07:13:12

(MENAFN- Newsfile Corp) Montreal, Quebec--(Newsfile Corp. - September 22, 2025) - Quebec Innovative Materials Corp. (CSE: QIMC) (OTCQB: QIMCF) (FSE: 7FJ) ("QIMC" or the "Company") is pleased to announce the discovery of a third major clean hydrogen zone in Nova Scotia. Soil-gas surveys conducted in the Southampton and East-Southampton areas returned 23 samples above 500 parts per million (ppm) hydrogen , of which 8 exceeded 1,000 ppm , including a peak value of 4,125 ppm - one of the highest concentrations recorded by the Company in the province to date.

"The confirmation of a third hydrogen zone in Nova Scotia, with 23 samples above 500 ppm including 8 over 1,000 ppm and a peak of 4,125 ppm, represents a transformative step for QIMC. Each new anomalous zone further validates our thesis that the Cumberland Basin is one of the most promising natural hydrogen districts in North America. Importantly, geology shows deformation and folding of rocks between the features that present strong similarities with the Carboniferous Basin of Lorraine in Europe, in both cases, we are in a carboniferous basin containing continental sedimentary rocks, including coal rocks, among others. With the integration of seismic data into our exploration model, QIMC is positioned - alongside Nova Scotia - at the forefront of clean hydrogen development," said John Karagiannidis, President & CEO of QIMC .

This latest discovery zone builds on QIMC's previously announced results at West Advocate and Eastern Advocate, further confirming Nova Scotia's Cumberland Basin as one of North America's most promising emerging natural hydrogen hubs. With three major zones now confirmed, the QIMC and INRS teams are expanding our Phase 2 and Phase 3 programs in these areas.

"Following recent meetings with our partners, we are also evaluating the next phase of development, which includes the integration of ammonia production into our model, leveraging Nova Scotia's existing infrastructure and port facilities," adds John Karagiannidis.

Geological Context of Southampton

The geomorphological and geological contexts of the Southampton area are markedly different from those of the tectonized zone of the Cobequid Highlands in the Advocate and West-Advocate areas. As a result, the discovery of a new hydrogen anomalous domain in the Southampton area is noteworthy and must be interpreted in terms of geological characteristics specific to the Cumberland Carboniferous Basin .

Prof. Marc Richer-Laflèche (INRS) commented: "The Southampton anomalies highlight a structural and geological setting distinct from Advocate. Here we are working within a Carboniferous basin environment, which provides a unique context for hydrogen migration and accumulation."

Structural Controls and Basin Setting

As shown on the elevation data map (Fig. 1a), hydrogen soil-gas anomalies are located on a lower elevation plateau north of the Cobequid Highlands. This topography is influenced by a regional fault system separating the Carboniferous domains of the Cumberland Basin to the north (Pennsylvanian sedimentary rocks) from the older granitic and Neoproterozoic volcanic-sedimentary terrains of the Jeffers Group to the south (Fig. 1c).

This geological contrast is clearly expressed by a magnetic high on Nova Scotia's regional aeromagnetic map (Fig. 2). On a local scale, magnetic and gravimetric surveys show low potential field values , which encompass most of the highest hydrogen anomalies observed. Such zones typically indicate a thickening of sedimentary sequences in basins.

Seismic Data Integration

Seismic reflection data, reprocessed by the Geological Survey of Canada (Durling, 2023), underline the importance of the Athol syncline , which reaches a depth of ~5 km beneath the anomalous Southampton sector. This section also shows the presence of at least four south-dipping faults .

In QIMC's exploration model, these faults act as migration conduits, promoting the upward movement of hydrogen to surface soils (Fig. 3).

Prof. Richer-Laflèche added: "The seismic integration is critical. It shows the geometry of the basin, the depth of the Athol syncline, and the role of fault systems that facilitate hydrogen migration. This structural picture strengthens our confidence in the Southampton anomalies."

Lithological Associations

The highest hydrogen concentrations were observed over the Carboniferous Ragged Reef Formation , composed of alternating fluvial sandstones, conglomerates, mudstones, lacustrine limestones, and rare coal horizons. In contrast, soils overlying the Malagash Formation did not display hydrogen anomalies.

Structurally, the strongest anomalies coincide with zones affected by secondary south-dipping faults trending EW to WNW-ESE. These features appear to intersect a subvertical strike-slip fault along the southern margin of the Cumberland Basin, at the foot of the Cobequid Uplands.

Conceptually, this geological and structural framework suggests hydrogen formation result from groundwater infiltration into south-dipping faults and reactions at depth with igneous rocks of the Cobequid Highlands. The well-documented high geothermal gradient of the Cumberland Basin acts as a catalyst for such hydrogen-producing processes.

Figure 1. A) NASA elevation map (in m), B) total magnetic field map, C) simplified geological map D) residual Bouguer anomaly (gravimetry). Maps from the site. The red box shows the perimeter of the Soil-Gas survey conducted in the Southampton and East-Southampton areas.