June 17, 2019 - 8:00 AM EDT
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Azincourt Energy Initial Drilling Confirms East Preston Basement Prospectivity

VANCOUVER, British Columbia, June 17, 2019 (GLOBE NEWSWIRE) -- AZINCOURT ENERGY CORP. (“Azincourt” or the “Company”) (TSX.V: AAZ, OTC: AZURF), is pleased to announce positive results from the Company’s recent phase one drill program at the East Preston uranium project, located in the western Athabasca Basin, Saskatchewan, Canada.

The initial drill campaign has confirmed the prospectivity of the East Preston project, as basement lithologies and graphitic structures intersected at East Preston are very similar and appear to be analogous to the Patterson Lake South-Arrow-Hook Lake/Spitfire uranium deposit host rocks and setting.  A total of 552 meters of drilling was completed in three holes prior to the onset of spring break-up conditions that impacted the duration of the program.  The rapid onset of spring required shifting from entirely overland-supported drilling to helicopter-supported drilling. All drill holes targeted multiple closely spaced discreet graphitic conductors with coincident gravity low anomalies often indicative of alteration or thicker overburden due to enhanced glacial scouring over altered, or structurally disrupted basement.

“We are certainly very pleased with the results of the first few holes, it’s an excellent start to initial drill testing at East Preston,” said president & CEO, Alex Klenman. “We have confirmed the project contains the appropriate environment – both geologically and geochemically – that is consistent with uranium mineralization in the area.  That’s a significant confirmation, and to be able to determine this at the outset is very positive development.  These are the right graphitic-rich host rocks and given we have just started drilling, we’re obviously optimistic about what’s ahead. We have dozens of high priority targets yet to drill, and thanks to recent substantial institutional support we are well funded to execute a much larger phase two program.  Permitting is already underway, we have the cash, and we have the targets.  Our timing looks good with sector developments as well. We’re excited to get more drills in the ground and will announce details of the upcoming phase two drill campaign in the coming weeks,” continued Mr. Klenman.

“We are highly encouraged with our first drill program results at East Preston,” said Ted O’Connor, Director and Technical Advisor for East Preston. “We have confirmed that we have prospective graphitic basement rocks and the right basement unconformity setting on the project. There are numerous conductor corridor system targets to test as we vector towards areas of structural disruption; all critical ingredients as we continue development of East Preston,” continued Mr. O’Connor.

The East Preston project lies immediately south of the interpreted southern edge of the Athabasca Basin, so no Athabasca sandstone was expected.  Overburden thickness ranged from 15 to 33 m thick, and as expected, no Athabasca sandstone was intersected.  Numerous untested graphitic conductive trends remain on the project for drill testing, and additional targets have been generated from the recent VTEM survey that now covers the entire East Preston project lands.

The basement rocks intersected comprised amphibolite-grade (high-grade) metamorphic pelitic/mafic to pssamopelitic/felsic gneisses and schists with pegmatitic partial melt segregations. Numerous intervals of blue quartz ‘units’ interpreted as either amphibolite-grade orthoquartzite, or silica-flooded, altered gneissic precursors were also intersected. The gneissic rocks often become highly strained displaying mylonitic to proto-mylonitic textures.

All drill holes intersected at least two intervals of graphitic pelitic gneiss/schist, sufficiently explaining the HLEM and VTEM conductors targeted. In drill holes EP19001 and EP19002, the graphitic rocks intersected were primarily stratigraphic with little associated structural disruption. Drill hole EP19003 intersected moderate to strong structural upgrading within the upper graphitic-pyritic unit encountered. Anomalous radioactivity was observed immediately in the hanging wall upper contact of this graphitic fault interval associated with partial melt pegmatite.

A photo accompanying this announcement is available at https://www.globenewswire.com/NewsRoom/AttachmentNg/a8cd7bfb-e51b-4832-a9f8-4f965fcb421f

Downhole probe results showed anomalous radioactivity predominantly attributed to thorium related to observed partial melt pegmatitic granite intervals in drill core.  Drill core samples collected were submitted to SRC Geoanalytical Laboratories in Saskatoon for ICP-MS Total Digest, ICP-MS Partial digest, Boron by fusion and Gold fire assay chemical analysis. Trace element geochemistry shows anomalous results for basement-hosted unconformity uranium deposit pathfinders Ni, Co, Cu, Zn and As associated with graphitic schist intervals. Graphitic rocks hosting uranium mineralization are often associated with Ni-Co-As; Cu and Zn sulphides in anomalous, to substantial quantities. The presence of these pathfinder elements adds additional information and will enhance vectoring towards the most prospective areas of the conductor systems.

Drill Hole Analysis

EP19001 (Pad B, 094/-45°): PAD B on L2400 targets the confluence of north- and northeast-trending conductors (prospective structure) with a coincident gravity anomaly (potential alteration), and a positive airborne radiometric anomaly (a potential mineralization indicator).

This hole successfully intersected graphite-rich intermediate-mafic (semipelitic?) gneiss and schist units between 105-145m (5-10% graphite), and 157.2-181.9m (2-5% graphite). Both intervals are sandwiched between granitic to granodioritic orthogneiss. Lithology variations and graphite content are significant enough to explain the geophysical conductor targets at this location.  Overall alteration intensity is considered low to moderate. Radiometric anomalies are limited to biotite-rich fractures +-blue quartz or pods within pegmatitic granite subunits. The targeted hole successfully intersected graphite-laden structures/lithologies that are similar in character to host lithologies along the Patterson Lake trend.

EP19002 (Pad E, 105/-45°): PAD E on L1200 targets a flexure in the HLEM conductor trend and two down hole northwest dipping Maxwell Planes. This site is located 1.5km southwest and on-strike of hole EP19002.

Near identical sequence of lithologies as in hole EP19001 with intercepts averaging 40m higher in the hole.  Radiometric anomalies are limited to biotite-rich fractures +-blue quartz or pods within pegmatitic granite subunits. Overall more carbonate and less garnet than EP19001. Two graphite rich bands correlate well with projected geophysical conductor traces.

Hole EP19003 (Pad KB, 120/-45°): PAD KB on M600 targets a flexure in a strong VTEM conductor trend. This site is located 1.0 km north of hole EP19001, along a second parallel conductor feature.

This hole intersected graphitic conductive lithologies significantly earlier than the predicted Maxwell-plate predicted depth of 155m, but in league with VTEM predicted conductor traces. Overall lithologic sequence is similar to holes 1 and 2, but overall graphitic content is higher in this hole. Garnet metamorphic overprint is high with low carbonate alteration. Pyrite content is also significantly elevated in the 54-61.5m interval. The highest count of 368 cps occurs at 50.5m depth in a pegmatitic granite immediately adjacent to the first graphitic fault gouge.

A photo accompanying this announcement is available at https://www.globenewswire.com/NewsRoom/AttachmentNg/2de2f8be-1f42-4254-8050-dbcdd26404d1

About East Preston

Azincourt is currently earning towards 70% interest in the 25,000+ hectare East Preston project as part of a joint venture agreement with Skyharbour Resources (TSX.V: SYH), and Clean Commodities Corp (TSX.V: CLE).   Extensive regional exploration work at East Preston was completed in 2013-14, including airborne electromagnetic (VTEM), magnetic and radiometric surveys. 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 Company completed a winter geophysical exploration program in January-February 2018 that generated a significant amount of new drill targets within the previously untested corridors while refining additional targets near previous drilling along the Swoosh corridor.

Ground-truthing work confirmed the airborne conductive trends and more accurately located the conductor axes for future drill testing. The gravity survey identified areas along the conductors with a gravity low signature, which is often associated with alteration, fault/structural disruption and potentially, uranium mineralization. The combination/stacking of positive features has assisted in prioritizing targets.

The Main Grid shows 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 prospectivity targets because of the structural complexity.

The targets are basement-hosted unconformity related uranium deposits similar to NexGen’s Arrow 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).

Quality Assurance, Quality Control and Data Verification

Drill core samples were interval grab samples of interesting lithologies from 0.7m to 2 m in length, split in half longitudinally, with one-half of the core retained, and the other half placed in sealed bags and shipped to SRC Geoanalytical Laboratories (SRC) in Saskatoon, SK for sample preparation, processing and ICP-MS multi-element analysis using Total and Partial digestion, gold by fire assay and boron by fusion. SRC is an ISO/IEC 17025/2005 and Standards Council of Canada certified analytical laboratory. The Company’s Qualified Person for the drill program, Mr. Ted O’Connor, has verified the data disclosed, including drilling, sampling and analytical data. The program is designed to include analytical quality assurance and control routines comprising the systematic use of standards, blanks and duplicate samples.

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 Ted O’Connor, P.Geo. a director of the Company, as well as a qualified person.

About Azincourt Energy Corp. 

Azincourt Energy 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 in the Athabasca Basin, Saskatchewan, Canada, and the Escalera Group uranium-lithium project located on the Picotani Plateau in southeastern Peru.

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
[email protected]

Azincourt Energy Corp.
1430 – 800 West Pender Street
Vancouver, BC V6C 2V6
www.azincourtenergy.com

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Figure 1: East Preston uranium project, initial drill pad locations

Figure 1: East Preston uranium project, initial drill pad locations
Figure 2: Project Location – Western Athabasca Basin, Saskatchewan, Canada

Figure 2: Project Location – Western Athabasca Basin, Saskatchewan, Canada

Source: GlobeNewswire (June 17, 2019 - 8:00 AM EDT)

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