Skyharbour's Partner Company Basin Uranium Corp. Announces Intersection of Significant Mineralization from Phase 1 Drilling at Mann Lake

Skyharbour's Partner Company Basin Uranium Corp. Announces Intersection of Significant Mineralization from Phase 1 Drilling at Mann Lake

Skyharbour Resources Ltd. 's ( TSX-V: SYH ) ( OTCQB: SYHBF ) (Frankfurt: SC1P ) (the "Company") partner company, Basin Uranium Corp. ("Basin Uranium") is pleased to announce the intersection of significant uranium mineralization from the five-hole, phase one drill program at its Mann Lake project located 25 km southwest of the McArthur River Mine and 15 km to the northeast along strike of Cameco's Millennium uranium deposit.

"Our phase one drill program has confirmed the northeast trending conductor corridor (A3) as highly prospective for uranium mineralisation with the first significant intersection of uranium at Mann Lake. We are greatly encouraged as these new results substantially upgrade the potential of the underexplored southeastern half of the project." commented Mike Blady, CEO of Basin Uranium. "We are looking forward to commencing phase two drilling in September and building off our successful phase one results."

Mann Lake Uranium Project
https://www.skyharbourltd.com/_resources/maps/SKY_MannLake_20211129.jpg

Phase One Drilling Highlights   :

  • 323 ppm U 3 O 8 over 0.5 metres, intersected 30 metres below the unconformity within a broader 7.2-metre interval of anomalous uranium and graphite mineralization in hole MN22002. Additionally, 46 ppm U 3 O 8 over 0.5 metres intersected 8 metres below the unconformity and immediately beneath a strongly sericite bleached shear zone in hole MN22004.
  • Significant boron (B) mineralization, which serves as a pathfinder element for uranium deposits, with over 1,000 ppm B encountered at the unconformity in hole MN22005, 525 ppm B encountered at the unconformity in hole MN22001 and 319 ppm B in dravite (boron-rich clay) below the unconformity in hole MN22003.
  • Significant rare earth elements (REE's), including a highlight value of 5,028 ppm over 0.5 metres within a broader 50-metre interval of anomalous mineralization starting 20 metres below the unconformity in hole MN22003.
  • Statistical analysis demonstrates correlation between anomalous concentrations of pathfinder elements (B, Co, Cu, Ni, and Pb) associated with the anomalous uranium mineralization. Pathfinder elements are widely regarded as guides to the discovery of unconformity-style uranium deposits and provide further evidence of the presence of fluid movement potentially related to a uranium mineralizing system.

A phase two drill program at Mann Lake is planned to commence shortly to follow-up on the encouraging results from phase one. It will also incorporate targets generated from the recently completed geophysical surveys on the property which include gravity and airborne mobile magnetotellurics (mobile MT). The results of these surveys are currently being analyzed and incorporated into historic geophysical surveys with results anticipated to be released in the near-term.

Phase One Drill Program Summary   :

The Phase 1 program was comprised of 3,503 metres of diamond drilling over five holes. Four drill holes (MN22001 – MN22004) over a strike length of 1,500 metres targeted the interpreted basement conductor from the 2014 MT resistivity survey, and a magnetic low (interpreted metasediment basement) within a gravity low anomaly (interpreted as a basement fault structure). One hole (MN22005) was drilled to test the intersection of a NE-trending structure parallel to MN06-005 which returned over 1,000 ppm boron at the unconformity, and a cross cutting E-W trending structure on strike to hole MN06-002 where hematite paleo weathering occurred at the unconformity.

Hole MN22001

Was drilled to test an interpreted basement conductor corresponding with ground UTEM conductor (A3), a mag low interpreted to be a metasediment basement host and a gravity low interpreted as a basement fault structure. This hole was successful in crossing the unconformity and intersecting weakly anomalous radioactive values. It also intersected graphite mineralization along fracture planes and foliation, indicating the potential for nearby uranium mineralization.

Hole MN22002

Was designed to test the same conductor and geophysical setting as hole MN22001, collared 400 metres to the N-NE. It was successful, crossing the unconformity and entering basement metasediments (mostly psammite) as well as locating anomalous radioactive values with the handheld scintillometre and downhole probe. Monazite and allanite mineralization at the anomaly was also observed. Graphite mineralization was also noted in basement psammites along foliations and within some fractures. Notably, this hole returned 323 ppm U 3 O 8 from 660.05 to 660.55 metres approximately 30 metres below the unconformity within a larger 7.2-metre interval of anomalous uranium radioactivity which is host to graphite mineralization.

Hole MN22003

Was a step-out of 350 metres to the N-NE of MN22002 and was designed to test the same conductor and geophysical setting. Blood-red hematite paleoweathering at the unconformity and silica mottling has overprinted the texture of the psammite directly below the unconformity. Dravite-clay alteration can be found within fractures throughout the paleoweathered section and decreases in prevalence with depth.

This hole was successful in crossing the unconformity and intersecting radioactively anomalous intervals with allanite mineralization. Intervals within the basement rocks were found to contain graphite and dravite mineralization. Significant rare earth elements (REE's) of 5,028 ppm (Sum REE's = La+Ce+Pr+Nd+Sm+Eu+Gd) over 0.5 metres from 681.22 metres downhole were intersected within a broader 50 metre zone of anomalous REE mineralization starting 20 metres below the unconformity.

Hole MN22004

Was a 150-metre step-out along the conductor and strike of MN06-003A which intersected 12 metres of hematized paleoweathering up hole of the unconformity. An interpreted basement conductor, mag low and gravity low were present. While the hole did not intersect any lithology resembling the target Wollaston Group metasediments. The intersection of minor monazite mineralization, 46 ppm U 3 O 8, over 0.33 metres starting from 615.22 metres downhole in close proximity to strong clay alteration, remains a potentially interesting indication of uranium mineralization nearby.

Hole MN22005

This hole was designed to test the intersection of a NE-trending structure parallel to MN06-005 which returned over 1,000 ppm boron and 720cps at the unconformity, and a cross cutting E-W trending structure on strike to MN06-002 where 750cps and hematite paleoweathering occurred at the unconformity.

The hole was successful in intersecting a strongly hematite altered basement fault structure up hole and in close proximity to the unconformity. There was also a small interval of granitized strongly foliated metapelite intersected just below the unconformity, followed by granitic gneiss with intercalated pegmatites to the end of hole. Within the granite basement, clay dravite mineralization occurred, coating the surfaces of several low angle fractures between 652m - 663m.

Phase 1   Mann Lake Drill Plan   :
https://skyharbourltd.com/_resources/maps/Phase-one-Drill-Plan.jpg

Table 1: Collar Locations

Hole Number



Azimuth (Deg)



Dip (Deg)



Easting



Northing



Total Depth (m)



Depth to Unconformity (m)



MN22001 0 -90 470812 6383121 731 650.65
MN22002 0 -90 471133 6383344 683 631.31
MN22003 0 -90 471379 6383635 713 630.95
MN22004 0 -90 471878 6384180 704.65 607.76
MN22005 0 -90 473245 6384561 671.67 623.79
Total Metreage (m) 3503.32

QA/QC   :

Samples were sent for geochemical analysis with SRC Geoanalytical Laboratories, Saskatoon for the following analyses: ICP-MS1 (Sandstone) and ICP-MS2 (Basement) which includes both partial and total digestion methods as well as an additional Boron analysis. Over limit analysis were completed using U3O8 total digestion when U >1000ppm.

On receipt of final certificates of analysis, the QA/QC sample results were reviewed to ensure the order of samples were reported correctly, that the blanks ran clean, and that the results for each standard had minimal variance from its certified value. QA/QC for the Mann Lake drilling included certified reference material ("CRM's") and blanks that were inserted into each sample batch in order to verify the analytical from the lab.

About Mann Lake:

Skyharbour has entered into an Option Agreement (the "Agreement") with Basin Uranium whereby Basin Uranium has an earn-in option to acquire a 75% interest in the Mann Lake Uranium Project. Under the Option Agreement, Basin Uranium Corp will contribute cash and exploration expenditure consideration totalling CAD $4,850,000 over a three-year period ("Project Consideration"). Of the Project Consideration, $850,000 will be in cash payments to Skyharbour and $4,000,000 will be in exploration expenditures on the project. Basin Uranium Corp will also issue to Skyharbour the equivalent value of CAD $1,750,000 in shares of Basin Uranium over the three-year earn-in period to complete the earn-in.

The Mann Lake Uranium Project is strategically located 25 km southwest of the McArthur River Mine, the largest high-grade uranium deposit in the world, and 15 km to the northeast of Cameco's Millennium uranium deposit. The Mann Lake project is also adjacent to the Mann Lake Joint Venture operated by Cameco (52.5%) with partners Denison Mines (30%) and Orano (17.5%). Denison Mines acquired International Enexco and its 30% interest in the project after a 2014 winter drill program discovered high-grade, basement-hosted uranium mineralization at this adjacent project.

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 and approved by David Billard, P.Geo., a Consulting Geologist for Skyharbour as well as a Qualified Person.

About Skyharbour Resources Ltd.:

Skyharbour holds an extensive portfolio of uranium exploration projects in Canada's Athabasca Basin and is well positioned to benefit from improving uranium market fundamentals with fifteen projects, ten of which are drill-ready, covering over 450,000 hectares of land. Skyharbour has acquired from Denison Mines, a large strategic shareholder of the Company, a 100% interest in the Moore Uranium Project which is located 15 kilometres east of Denison's Wheeler River project and 39 kilometres south of Cameco's McArthur River uranium mine. Moore is an advanced-stage uranium exploration property with high-grade uranium mineralization at the Maverick Zone that returned drill results of up to 6.0% U 3 O 8 over 5.9 metres including 20.8% U 3 O 8 over 1.5 metres at a vertical depth of 265 metres. Adjacent to the Moore Uranium Project is Skyharbour's recently optioned Russell Lake Uranium Project from Rio Tinto, which hosts historical high-grade drill intercepts over a large property area with robust exploration upside potential. The Company is actively advancing these projects through exploration and drill programs.

Skyharbour has a joint-venture with industry-leader Orano Canada Inc. at the Preston Project whereby Orano has earned a 51% interest in the project through exploration expenditures and cash payments. Skyharbour now owns a 24.5% interest in the Project. Skyharbour also has a joint venture with Azincourt Energy at the East Preston Project whereby Azincourt has earned a 70% interest in the project through exploration expenditures, cash payments and share issuance. Skyharbour now owns a 15% interest in the Project. Preston and East Preston are large, geologically prospective properties proximal to Fission Uranium's Triple R deposit as well as NexGen Energy's Arrow deposit. Furthermore, the Company owns a 100% interest in the South Falcon Point Uranium Project on the eastern perimeter of the Basin, which contains a NI 43-101 inferred resource totaling 7.0 million pounds of U 3 O 8 at 0.03% and 5.3 million pounds of ThO 2 at 0.023%.

Skyharbour has several active option partners including: ASX-listed Valor Resources on the Hook Lake Uranium Project whereby Valor can earn-in 80% of the project through CAD $3,500,000 in exploration expenditures, $475,000 in cash payments over three years and an initial share issuance; CSE-listed Basin Uranium Corp. on the Mann Lake Uranium Project whereby Basin Uranium can earn-in 75% of the project through $4,000,000 in exploration expenditures, $850,000 in cash payments as well as share issuances over three years; and CSE-listed Medaro Mining Corp. on the Yurchison Project whereby Medaro can earn-in an initial 70% of the project through $5,000,000 in exploration expenditures, $800,000 in cash payments as well as share issuances over three years followed by the option to acquire the remaining 30% of the project through a payment of $7,500,000 in cash and $7,500,000 worth of shares.

Skyharbour's goal is to maximize shareholder value through new mineral discoveries, committed long-term partnerships, and the advancement of exploration projects in geopolitically favourable jurisdictions.

Skyharbour's Uranium Project Map in the Athabasca Basin:
https://www.skyharbourltd.com/_resources/image   s/SKY-SaskProject-Locator-20220324.jpg

To find out more about Skyharbour Resources Ltd. (TSX-V: SYH) visit the Company's website at www.skyharbourltd.com .

Skyharbour Resources Ltd.

"Jordan Trimble"

Jordan Trimble
President and CEO

For further information contact myself or:
Nicholas Coltura
Corporate Development and Communications
Skyharbour Resources Ltd.
Telephone: 604-558-5847
Toll Free: 800-567-8181
Facsimile: 604-687-3119
Email: info@skyharbourltd.com

NEITHER THE TSX VENTURE EXCHANGE NOR ITS REGULATION SERVICES PROVIDER ACCEPTS RESPONSIBILITY FOR THE ADEQUACY OR ACCURACY OF THE CONTENT OF THIS NEWS RELEASE.

The securities offered have not been, and will not be, registered under the United States Securities Act of 1933, as amended (the "U.S. Securities Act") or any U.S. state securities laws, and may not be offered or sold in the United States or to, or for the account or benefit of, United States persons absent registration or an applicable exemption from the registration requirements of the U.S. Securities Act and applicable U.S. state securities laws. This press release does not constitute an offer to sell or the solicitation of an offer to buy securities in the United States, nor in any other jurisdiction.

This release includes certain statements that may be deemed to be "forward-looking statements". All statements in this release, other than statements of historical facts, that address events or developments that management of the Company expects, are forward-looking statements, including the Private Placement. Although management believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance, and actual results or developments may differ materially from those in the forward-looking statements. The Company undertakes no obligation to update these forward-looking statements if management's beliefs, estimates or opinions, or other factors, should change. Factors that could cause actual results to differ materially from those in forward-looking statements, include market prices, exploration and development successes, regulatory approvals, continued availability of capital and financing, and general economic, market or business conditions. Please see the public filings of the Company at www.sedar.com for further information.


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  • Five drill holes outlined an open massive hydrothermal clay alteration system measuring at least 200 m x 100 m, resembling alteration found in Athabasca high-grade uranium deposits
  • Radioactivity within the clay alteration system increases with depth and remains open
  • Drill hole HK24-010 intersected 13.4 metres of continuous radioactivity within a 200 m wide alteration system
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"These results represent an important discovery on our Hook project. While we've already made a discovery at Hook with ACKIO, this is only a small part of the broader Hook land package. The potential on the property is substantial as Hook is an extensive project, and our discovery at ACKIO, combined with our neighbour Atha Energy's discovery in their Gemini Mineralized Zone, highlights that the region has all the geological features needed to host significant uranium deposits. More importantly, we can clearly demonstrate that this area is fertile with uranium mineralization. Large-scale alteration systems are key indicators when it comes to uranium, which tends to occur in smaller deposits relative to other minerals. We're pleased to have uncovered such a large system, exhibiting all the hallmark features needed for a new high-grade Athabasca uranium discovery," commented James Sykes, CEO, President, and Director of Baselode.

Watch this video for a detailed analysis of the two follow-up target areas and a comparison of Hook alteration systems to seven Athabasca high-grade uranium deposits that have combined over 700 million pounds of uranium.

The first alteration system the Company highlights is in the HK24-016 area, measuring more than 250 metres wide by 400 metres deep, with a core of massive clay and bleached alteration styles that measure 100 metres wide by at least 200 metres deep. These core alteration styles are important as they are the same style associated with at least three basement-hosted Athabasca high-grade uranium deposits.

The second alteration system identified in the HK24-010 area is significant due to its similarly large scale, intersecting 13 meters of continuous anomalous radioactivity within pegmatite along the margin of the fluid pathway. While assays are pending, the Company is well-funded and eager to proceed with follow-up drill plans for these high-priority exploration targets.

Hook Exploration Drill Hole Highlights

HK24-016 area

Drill holes HK24-016, HK24-017, and HK24-021 to HK24-023 were collared 5.5 kilometres southwest of ACKIO (Figure 2, Figure 3). HK24-016 intersected 140 metres of massive hydrothermal clay and bleaching alteration (the "clay alteration") within a broader 370 m thick alteration corridor (Figure 4). The drill hole intersected anomalous radioactivity associated with fracture-controlled remobilized hematite alteration within the clay alteration (Figure 5).

Both HK24-017 and HK24-021 targeted the clay alteration up-dip and down-dip, with each intersecting 30 and 145 metres of clay alteration, respectively. HK24-022 was collared 100 metres southeast of HK24-016 and intersected 60 metres of clay alteration, and HK24-023 was collared 50 metres northeast and intersected 110 metres of clay alteration. Initial observations suggests follow-up drilling is required beneath HK24-021 and to the north of HK24-023.

The clay alteration encountered within these Hook drill holes (Figure 6) share numerous similarities to massive hydrothermal clay alteration systems observed in Athabasca basement-hosted, high-grade uranium systems, such as Cameco's Millennium and Eagle Point deposits, Uranium Energy Corp's Roughrider deposits, and Denison Mines' Gryphon deposit.

The upper outer halo of the clay alteration is further identified with unique limonite liesegang banding and fracture-controlled alteration, including a distinct quartz stockwork. These are also similar outer halo alteration styles that have been observed within large-scale Athabasca uranium deposits.

HK24-010 area

Drill holes HK24-009 and HK24-010 were collared 6 kilometres northeast of ACKIO (see Figure 2, Figure 7). Details of these drill holes were initially released on July 17, 2024. HK24-010 has returned the best radioactive intersection outside of Baselode's near-surface ACKIO uranium prospect with 13.2 metres of continuous anomalous radioactivity starting at 186 metres beneath the surface hosted within a pegmatite along the western margin of a 200 m-wide, structurally-controlled, hematite and bleached alteration system. The area remains open in all directions.

Drill hole samples have been sent to Saskatchewan Research Council for uranium and multi-element analysis. Results will be released after being received and reviewed by the Company.

NOTES:

  1. cps* = "counts-per-second", as measured with a handheld RS-125 Gamma-Ray Spectrometer/Scintillometer ("RS-125"). The reader is cautioned that Baselode uses scintillometer readings as a preliminary indication for the presence of radioactive materials (uranium, thorium and/or potassium), and that scintillometer results may not be used directly to quantify or qualify uranium concentrations of the rock samples measured.
  2. The Company defines groupings of RS-125 as i) background radioactivity (50 to 200 cps), ii) above-background radioactivity (200 to 300 cps), and iii) anomalous radioactivity (300 to 1,000 cps).
  3. "Radioactivity (>300 cps)" in Table 1 is defined as drill core length with no greater than 2.0 m of consecutive drill hole length measuring less than 300 cps.
  4. All reported drill hole depths and lengths do not represent true thicknesses.

About Baselode Energy Corp.

Baselode controls 100% of approximately 238,930 hectares for exploration in the Athabasca Basin area of northern Saskatchewan, Canada. The land package is free of any option agreements or underlying royalties.

The Company discovered the ACKIO near-surface, uranium prospect in September 2021. ACKIO measures greater than 375 m along strike, greater than 150 m wide, comprised of at least 9 separate uranium Pods, with mineralization starting as shallow as 28 m and 32 m beneath the surface in Pods 1 and 7, respectively, and down to approximately 300 m depth beneath the surface with the bulk of mineralization occurring in the upper 120 m. ACKIO remains open at depth, and to the north, south and east.

Baselode's Athabasca 2.0 exploration thesis focuses on discovering near-surface, basement-hosted, high-grade uranium orebodies outside the Athabasca Basin. The exploration thesis is further complemented by the Company's preferred use of innovative and well-understood geophysical methods to map deep structural controls to identify shallow targets for diamond drilling.

QP Statement

The technical information contained in this news release has been reviewed and approved by Cameron MacKay, P.Geo., Vice-President, Exploration & Development for Baselode Energy Corp., who is considered to be a Qualified Person as defined in "National Instrument 43-101, Standards of Disclosure for Mineral Projects."

For further information, please contact:

James Sykes, CEO, President and Director
Baselode Energy Corp.
jsykes@oregroup.ca
306-221-8717
www.baselode.com

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the TSX Venture Exchange policies) accepts responsibility for the adequacy or accuracy of this release.

Certain information in this press release may contain forward-looking statements. This information is based on current expectations that are subject to significant risks and uncertainties that are difficult to predict. Actual results might differ materially from results suggested in any forward-looking statements. Baselode Energy Corp. assumes no obligation to update the forward-looking statements, or to update the reasons why actual results could differ from those reflected in the forward looking-statements unless and until required by securities laws applicable to Baselode Energy Corp. Additional information identifying risks and uncertainties is contained in the Company's filings with Canadian securities regulators, which filings are available under Baselode Energy Corp. profile at www.sedarplus.ca.

This news release does not constitute an offer to sell or a solicitation of an offer to buy any of the securities in the United States. The securities have not been and will not be registered under the United States Securities Act of 1933, as amended (the "U.S. Securities Act") or any state securities laws and may not be offered or sold within the United States or to, or for the account or benefit of, U.S. Persons unless registered under the U.S. Securities Act and applicable state securities laws, unless an exemption from such registration is available.

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FIGURE 1 - Baselode projects location map. ACKIO uranium prospect identified with yellow circle.

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_001full.jpg

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FIGURE 2 - Drill holes (HK24-009 to HK24-023) location map

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https://images.newsfilecorp.com/files/6412/224182_480ec88df46cda96_002full.jpg

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FIGURE 3 - HK24-016 target area drill holes (HK24-016, HK24-017, and HK24-021 to HK24-023) location map

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FIGURE 4 - Cross-section interpretation of large hydrothermal fluid system with core massive clay and bleaching alteration (blue)

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FIGURE 5 - Fracture-controlled, hydrothermal remobilized anomalous radioactivity, HK24-016

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FIGURE 6 - Massive clay and bleaching alteration system, HK24-021. NOTE: clay has been gouged with carbon scribe to demonstrate drill core softness

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FIGURE 7 - HK24-010 target area drill holes (HK24-009 and HK24-010) location map

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MOVIE 1 - Clay alteration and bleaching identified within drill hole HK24-021

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