Azincourt Energy Recieves Results of 2023 Drilling Program at the East Preston Uranium Project
AZINCOURT ENERGY RECIEVES RESULTS OF 2023 DRILLING
PROGRAM AT THE EAST PRESTON URANIUM PROJECT
• Elevated uranium, dravite clay alteration identified in K and H-Zones
Vancouver B.C., August 17, 2023 - AZINCOURT ENERGY CORP. (“Azincourt” or the
“Company”) (TSX.V: AAZ, OTCQB: AZURF), is pleased to announce that the sample analysis has
finally been received from the 2023 exploration program at the East Preston uranium project in the
Athabasca Basin, Saskatchewan, Canada.
Drilling for the 2023 program at the East Preston Project consisted of a total of 3,066 meters
completed in 13 drill holes between February and March 2023. Drilling was focused on the G, K, H,
and Q zones (Figure 3) with results reported in a news release dated March 28th, 2023.
Winter 2023 Diamond Drilling Program Highlights
A total of 687 samples were collected throughout the program and sent to the Geoanalytical
Laboratory at the Saskatchewan Research Council in Saskatoon, Saskatchewan for analysis. As was
reported in a news release dated July 11, 2023, there was a delay with the analytical results. After a
review of the initial data received from the lab, ther e were significant quality control issues noted
within the results. As part of the quality control process, standards with a known concentration of
uranium are inserted in the sample batches. These samples are analyzed to confirm that the results for
that batch of samples are within an acceptable range based on the results of the standards. The issues
noticed manifested as anomalous results occurring in the samples analyzed immediately following
several of the standards. As a result, these samples were reanalyzed. Once the issue was identified ,
confirmed, and resolved, the company requested that all samples of the affected batches be run
through the process to ensure a complete consistent data set.
Analysis of the results shows uranium enrichment within the previously identified clay alteration
zones along the K, and H- target zones. Uranium enrichment is identified as uranium (U) values and
a uranium/thorium ratio (U/Th) above what would normally be expected in the given rock type or
area.
Drilling on the northeast trending G-Zone (Figure 2) identified extensive hydrothermal alteration and
evidence of east-west cross-cutting structures along the southern portion of the zone. The primary
rock types in the alteration zone are granodiorite and diorite gneiss with average expected values of
2-3 ppm U and U/Th ratios of 0.25-0.3. Elevated radioactivity was intersected in EP0045 and EP0047
and EP0047 returned elevated U and U/Th values. While this is a good sign, the alteration zone does
not display the upgraded clay alteration halo seen at Zones K and H.
Illite and kaolinite are both indicators of hydrothermal alteration typically found within alteration
halos of unconformity uranium deposits. Dravite is a boron-rich clay which is typically found within
a larger clay package in close proximity to uranium mineralization in the system. Both illite and
dravite have been identified as being significant vectors for the recent Patterson Lake North discovery
by F3 Uranium approximately 60 km to the northwest of the East Preston project.
On the north end of the K-Zone (Figure 2), drilling intersected extensive structure and hydrothermal
clay alteration within the structural zone . Samples of clay alteration were analyzed by Short
Wavelength Infrared Reflectance (SWIR, sometimes referred to as “PIMA”) to confirm the clay
species. All three holes contained i llite and kaolinite clay species , with EP0049 also having dravite
identified within the structural zone. EP0049 also returned elevated Thorium.
The H-Zone covers a change in orientation of the structural and conductive trend from north south to
southwest trending (Figure 2). Drilling intersected an intense graphitic fault zone with hydrothermal
alteration. The Illite clay alteration halo identified in the K -Zone extends south into the H Zone as
far south as EP0053. Hole EP0053 intersected elevated radioactivity and both kaolinite and dravite
are also present within the illite alteration package. Dravite was also identified in hole EP0052. Rocks
in this zone are expected to return values of 0.5-1.5 ppm U and U/Th ratios of 0.25-0.5. Holes EP0052
and EP0056 returned the best analytical results of the program with U/Th ratios of 1.0 and 1.8
respectively, and uranium in the 5-6 ppm range.
The company considers the drilling results to date to be significant, as major uranium discoveries in
the Athabasca Basin such as McArthur River, Key Lake, and Millennium were primarily the result of
drill testing of strong alteration zones related to conductor features. Identifying and upgrading the
strong alteration zones is a significant step forward in identifying the key areas along the conductor
trends where more attention is required.
“The alteration we are seeing in the K and H Zones is very encouraging” said VP, Exploration, Trevor
Perkins. “The associated elevated uranium present is also very promising and shows that we are
vectoring towards something in this area . The identification of dravite and illite clays with the
elevated uranium emphasizes that we are on the right track and getting close. This target area will be
a top priority moving forward and based on results we may see the north-northwest trending structures
taking on more significance for targeting on this trend and others on the pr operty,” continued Mr.
Perkins.
“We’re encouraged by the appropriate clay content in the alteration zones. If you’re hunting for a
uranium deposit, this is what you need to see,” said CEO, Alex Klenman. “The elevated uranium
values from the last two drill programs, combined with the confirmed presence of relevant clays and
strong U/Th ratios, within these systems , are substantial developments in the progression of the
project and should not be underestimated. Although we’d certainly welcome encountering significant
mineralization we continue to be well within a practical discovery timeline. We are eager to continue
moving the project forward and will begin formulating the next phase of drilling at East Preston. In
the meantime, we’re active at the Big Hill lithium project in Newfoundland and are awaiting results
of the current work program. A follow up program is in the planning stage and will be announced
shortly,” continued Mr. Klenman.
East Preston Targets
The primary target area on the East Preston Project is the conductive corridors from the A -Zone
through to the G -Zone (A-G Trend) and the K -Zone through to the H and Q -Zones (K-H-Q Trend)
(Figure 2). The selection of these trends is based on a compilation of results from the 2018 through
2020 ground-based EM and gravity surveys, property wide VTEM and magnetic surveys, and the
2019 through 2022 drill programs, the 2020 HLEM survey indicates multiple prospective conductors
and structural complexity along these corridors.
Drilling has confirmed that identified geophysical conductors comprise structurally disrupted zones
that are host to accumulations of graphite, sulphides, and carbonates. Hydrothermal altera tion,
anomalous radioactivity, and elevated uranium have been demonstrated to exist within these
structurally disrupted conductor zones.
Permitting and Community Engagement
The permitting process is underway for the 2024-2026 drill programs. Azincourt Energy continues
to be engaged in regular meetings with the Clearwater River Dene Nation and other rights holders to
ensure that concerns of the local communities are addressed with regards to the East Preston project.
A more in-depth engagement process will also be commencing within the next couple of months with
the La Loche Metis Local #39. Azincourt looks forward to a continued close working relationship
with CRDN and other rights holders to ensure that any potential impacts and concerns are addressed
and that the communities can benefit from activities in the area through support of local business,
employment opportunities, and sponsorship of select community programs and initiatives. Local
businesses are engaged to provide services and supplies and m embers of the Clearwater River Dene
Nation and surrounding communities have been directly employed on site or to provide support and
services to keep the camp and programs running.
Figure 1: East Preston Project Location – Western Athabasca Basin, Saskatchewan, Canada
Figure 2: 2023 Target areas and Drill Hole Locations at the East Preston Uranium Project with the
area of dravite and kaolinite clay alteration highlighted in red.
About East Preston
Azincourt controls a majority 78.4% interest in the 25,000+ hectare East Preston project as part of a
joint venture agreement with Skyharbour Resources (TSX.V: SYH), and Dixie Gold. Three
prospective conductive, low magnetic signature corridors have been discovered on the property. The
three distinct corridors have a total strike length of over 25 km, each with multiple EM conductor
trends identified. Ground prospecting and sampling work completed to date has identified outcrop,
soil, biogeochemical and radon anomalies, which are key pathfinder elements for unconformity
uranium deposit discovery.
The East Preston Project has multiple long linear conductors with flexural changes in orientation and
offset breaks in the vicinity of interpreted fault lineaments – classic targets for basement -hosted
unconformity uranium deposits. These are not just simple basement conductors; they are clearly
upgraded/enhanced prospectively targets because of the structural complexity.
The targets are basement-hosted unconformity related uranium deposits similar to NexGen’s Arro w
deposit and Cameco’s Eagle Point mine. East Preston is near the southern edge of the western
Athabasca Basin, where targets are in a near surface environment without Athabasca sandstone cover
– therefore they are relatively shallow targets but can have great depth extent when discovered. The
project ground is located along a parallel conductive trend between the PLS -Arrow trend and
Cameco’s Centennial deposit (Virgin River-Dufferin Lake trend).
Qualified Person
The technical information in this news release has been prepared in accordance with the Canadian
regulatory requirements set out in National Instrument 43-101 and reviewed on behalf of the company
by C. Trevor Perkins, P.Geo., Vice President, Exploration of Azincourt Energy, and a Qualified
Person as defined by National Instrument 43-101.
About Azincourt Energy Corp.
Azincourt is a Canadian -based resource company specializing in the strategic acquisition,
exploration, and development of alternative energy/fuel projects, including uranium, lithium, and
other critical clean energy elements. The Company is currently active at its joint venture East Preston
uranium project located in the Athabasca Basin, Saskatchewan, and the Big Hill lithium project,
located in southwestern Newfoundland.
ON BEHALF OF THE BOARD OF AZINCOURT ENERGY CORP.
“Alex Klenman”
Alex Klenman, President & CEO
Neither the TSX Venture Exchange nor its regulation services provider (as that term is defined in the
policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this
release.
This press release includes “forward-looking statements”, including forecasts, estimates, expectations
and objectives for future operations that are subject to a number of assumptions, risks and
uncertainties, many of which are beyond the control of Azincourt. Investors are cautioned that any
such statements are not guarantees of future performance and that actual results or developments may
differ materially from those projected in the forward -looking statements. Such forward -looking
information represents management’s best judgment based on information currently available. No
forward-looking statement can be guaranteed, and actual future results may vary materially.
For further information please contact:
Alex Klenman, President & CEO
Tel: 604-638-8063
Azincourt Energy Corp.
1430 – 800 West Pender Street
Vancouver, BC V6C 2V6
www.azincourtenergy.com