Baselode Defines the Significance of Massive Clay Alteration System Identified on Hook Uranium Project 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
Baselode Defines the Significance of Massive
Clay Alteration System Identified on Hook
Uranium Project
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
New defined target areas are within 6 km of near-surface ACKIO uranium prospect
Toronto, Ontario--(Newsfile Corp. - September 23, 2024) - Baselode Energy Corp. (TSXV: FIND)
(OTCQB: BSENF) ("
Baselode
" or the "
Company
") is pleased to provide results and findings from the
exploration and discovery portion of the drill program on Hook project ("
Hook
") in the Athabasca Basin
area of northern Saskatchewan.
"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.
Cannot view this video?
Visit:
https://www.youtube.com/watch?v=nKoT-b4CCUY
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.
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.
FIGURE 1 - Baselode projects location map. ACKIO uranium prospect identified with yellow
circle.
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FIGURE 2 - Drill holes (HK24-009 to HK24-023) location map
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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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