QUEBEC CITY, QUEBEC -
Newsfile Corp.
- 4 September 2024 - Quebec Innovative Materials Corp. (CSE: QIMC)
(FSE: 7FJ) ("QI Materials", "QIMC" or the "Company"), is proud to
announce a landmark discovery made in collaboration with our Quebec
partner, the Institut National de la Recherche Scientifique (INRS). The
findings from the recently completed 9.7km north-south line 7 have
uncovered hydrogen soil samples with concentrations exceeding 1000 parts
per million (ppm). Significantly, we observed 8 readings exceeding 600
ppm, with 2 of those surpassing 1000 ppm. Additionally, the average
measured 531.9 ppm over a 450 ms interval between the readings above
1000 ppm (Fig. 1). Professor Marc Richer-Laflèche, Scientific Head of
Applied Geoscience Laboratory comments, "These highly anomalous values
can be considered first-class given the absolute values that, locally,
exceed the instrumental detection limit of 1000 ppm. The results from
Line 7 validate the geological hydrogen model interpretations we
outlined in previous announcements."
The data distribution is illustrated in Figure 2, which maps the anomalies against a backdrop of satellite imagery.
Figure 1. Section showing the variability of H2 concentrations measured
in the soils of line 7 at St-Bruno-de-Guigues. Data are given as a
function of distance in meters
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Figure 2: Map of the distribution of hydrogen anomalies in the soils of
the St-Bruno-de-Guigues area. Data projected onto satellite image
background.
To view an enhanced version of this graphic, please visit:
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Exceptional natural hydrogen levels
"We are thrilled to announce this transformative discovery outlining a highly charged 70km
2 hydrogen area within our 250km
2
Ville Marie property," said John Karagiannidis, CEO of QIMC. "The
hydrogen concentrations identified by INRS mark a significant
advancement in our pursuit of clean, renewable energy solutions. This
breakthrough highlights our leadership in the hydrogen sector and
strengthens our commitment to advancing sustainable technologies that
support Quebec's clean emission goals. We eagerly anticipate the next
steps in developing and commercializing this remarkable hydrogen
resource."
Strategic Impact
To delineate the area of high hydrogen values observed along line 1 of
the July 2024 soil gas survey, the INRS field crew extended line 1
westward during the first week of August 2024. This extension begins at
the boundary between forest and agricultural land and ends near the
chemin des secondes et troisième rangs of St-Bruno-de-Guigues (line 7).
"As initially predicted in our hydrogen model, the intensity of the soil
hydrogen anomalies gradually decreased towards the west (Figure 3)",
notes Professor Marc Richer-Lafleche. "This decrease in concentration
emphasizes a westward closure of the hydrogen anomaly domain. This
spatial variability may reflect, among other things, the presence of
contrasting geological units (arkosic sandstones, Cobalt Group
conglomerates, Ordovician dolomitic limestones) and also the probable
presence of the Rivière-Blanche fault, which may be present in the
St-Bruno-de-Guigues area beneath the thick glacial-lacustrine
sediments", states Professor Marc Richer-Lafleche.
Fig. 3: Location map of the soil gas survey for Line 7 (North-South) and East-West Lines 1, 2, 3, 4 and 5.
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"We believe that this fault is partly responsible for the emplacement of
hydrogen in the St-Bruno-de-Guigues area," said John Karagiannidis, CEO
of QIMC. The location of this fault is a priority for QIMC and INRS and
will be the subject of a high spatial resolution audiomagnetotelluric
survey to be carried out in the fall of 2024.
"In the area of the sampling stations containing the hydrogen anomalies,
there is no evidence in the field (or in the MRNF databases) of the
presence of wells (former mining or oil wells), which could explain,
among other things, the presence of H2 anomalies from anthropogenic
sources. What's more, unlike the false H2 anomalies regularly reported
in the scientific literature, the H2 anomalous zones at
St-Bruno-de-Guigues extend for more than one kilometer (along
north-south or east-west axes), which cannot be explained by
anthropogenic sources.
It is also unlikely that the gas anomalies are the result of subsurface
biogenic processes, as the glaciolacustrine sediments hosting the H2
anomalies and also the H2-depleted zones (background) are very similar
from one sampling site to another. These Quaternary sediments are
essentially dominated by a mineral matrix with little potential to
generate significant amounts of hydrogen through fermentation reactions
with organic matter. In contrast to the study by Etiope et al. (2024),
which was carried out on soils from the Pusteria Valley region (northern
Italy), the H2 concentrations observed in soils from the Lake
Témiscamingue graben are not associated with very high CH4 and CO2
concentrations. Therefore, it is likely that the source of hydrogen in
St-Bruno-de-Guigues soils is geological rather than biogenic," details
Professor Marc Richer-Lafleche.
Next Steps:
Soil sampling is scheduled in the fall of 2024 to further analyze the
granulometric and elemental characteristics of glaciolacustrine
sediments in the St-Bruno-de-Guigues area.
Gravimetry and audiomagnetotellurism (AMT) geophysics are also planned
for the fall of 2024 to assess variations in the thickness of local
sedimentary rock deposits (gravity troughs) over the Archean basement.
These data will allow us to locate the areas most likely to contain
reservoir rocks. AMT data will allow us to locate graben-related faults
in the St-Bruno-de-Guigue area that are covered by Quaternary sediments.
"The high levels of hydrogen discovered by INRS underscore our
commitment to leading the transition to sustainable, clean energy
solutions," said John Karagiannidis. "We are excited about the upcoming
phases of commercial development and the opportunity to advance our
renewable energy initiatives."
REF:
Etiope, G., Ciotoli, G., , Bena, E., Mazzoli, C., Rockmann, T.,
Sivan, M., Squartini, A., Laemmel, A., Szidat, S., Haghipour, N. and
Sassi, R., 2024. Surprising concentrations of hydrogen and
non-geological methane and carbon dioxide in the soil . Science of the
Total Environment, 948.
About the INRS and Pr. Marc Richer-LaFlèche, P.Geo.
The Institut National de la Recherche Scientifique ("INRS") is a
high-level research and training institute. Pr. Richer-LaFlèche's team
has exceptional geological, geochemical and geophysical experience
specifically in the regions of QIMC's newly acquired claims. They have
carried out over six years of geophysical and geochemical work and
collected thousands of C1-C4 Soil-Gas analyses.
M. Richer-LaFlèche also holds an FRQNT grant, in partnership with Quebec
MRN and the mining industry, to develop and optimize a Soil-Gas method
for the direct detection of mineralized bodies and faults under
Quaternary cover. In addition to sulphide gases, hydrogen was
systematically analyzed in the numerous surveys carried out in 2023 in
Abitibi, Témiscamingue and also in the Quebec Appachian. M.
Richer-LaFlèche is the Qualified Person responsible for the technical
information contained in this news release and has read the information
contained herein.
In addition, the INRS team has several portable gas spectrometers and
the sampling equipment and logistics necessary for taking gas samples
and geophysical measurements on the ground or in the aquatic
environment. He is a professional geologist registered with the Ordre
des géologues du Québec and is the Qualified Person responsible for the
technical information contained in this news release and has read the
information contained herein and approves the press release.
For more information about Quebec Innovative Materials Corp. and its products, please visit
www.qimaterials.com.
QUÉBEC INNOVATIVE MATERIALS CORP.
John Karagiannidis
Chief Executive Officer
Tel: +1 438-401-8271
For further information, please contact:
Email:
info@qimaterials.com
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