Sego Resources Intercepts Porphyry-Related Phyllic Alteration at Cuba Zone, 1200 m Northeast of the Billy Zone Porphyry Copper Discovery Made in December 2025
Sego Resources Intercepts Porphyry-Related
Phyllic Alteration at Cuba Zone, 1200 m
Northeast of the Billy Zone Porphyry Copper
Discovery Made in December 2025
Vancouver, British Columbia--(Newsfile Corp. - February 2, 2026) - Sego Resources Inc. (TSXV: SGZ)
("Sego" or "the Company") is pleased to announce that a classic, porphyry-related phyllic alteration zone
was intercepted in drill hole DDH25-71, that was drilled at company's Cuba Zone (Figure 1), which is
located 1200 meters northeast of the South Gold Zone, now part of a larger Billy Zone.
Figure 1. Geologic map of Cuba Zone (red), with traces of DDH25-71, DDH-MM-18-37 and DDH-MM-
34 drill holes.
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Drill hole DDH25-71 was based on earlier copper intercepts from drill holes DDH-MM-18-37 and DDH-
MM-18-34. The purpose of this drill hole was to explore potentially deeper, structurally controlled
porphyry copper mineralization.
Figure 2. Longitudinal section looking northeast, showing the drill hole DDH25-71 and drill holes MM-18-
37 and MM-18-34 with projected drill results.
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Pyrite is present within the phyllic altered zone, being mostly fine and disseminated, with occasional
stringers and veinlets.
Quartz stockwork was also observed locally (Figure 3).
Based on geological observations from this hole, the next Cuba zone drill hole can be drilled from the
northeast, which could intercept the mineralized zone earlier.
A
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B
Figure 3. Examples of quartz stockwork in DDH25-71 drill core. 35 cm long HQ core.
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Phyllic alteration is very important in the exploration for copper porphyry deposits, as it often defines a
halo or a shell surrounding the central, potassic (K-feldspar/biotite) alteration zone.
Patchy potassic (K-feldspar) alteration was also intercepted, in the lowermost part of drill hole DDH25-
71, starting at 542.93 m, and extending until the end of the drill hole at 586.64 m, gradually increasing in
its size and intensity with increasing depth.
Below 577.68 m, and especially between 580.84 m and 586.64 m (end of drill hole, Figure 4), the core
looks similar in its appearance (patchy potassic, K-feldspar alteration and brecciated nature) to the best
mineralized intervals of
MM-18-37 drill hole, which were also at the very end of drill hole MM-18-37, from
225 m to 233 m (final depth).
Magnetic susceptibility readings in drill hole DDH25-71 made a very sharp, big increase at 560 m,
compared to earlier readings. All magnetic susceptibility readings from 560 m to 588 m (measured at
every meter) were high to very high.
Figure 4. Patchy potassic (K-feldspar alteration) at 582.50 m-583.70 m in drill hole DDH25-71.
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Core logging has been completed, with ongoing core cutting and samples being prepared for shipping
to the lab in Calgary.
Qualified Person
The technical information in this news release has been reviewed and approved by Goran Markovic,
MSc., P.Geo., who is a Qualified Person under the definitions established by NI 43-101, and is an
Independent Consulting Geologist commissioned by Sego Resources Inc.
J Paul Stevenson, CEO, Director
For further information please contact:
J. Paul Stevenson, CEO
(604) 682-2933
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. No regulatory authority has approved or disapproved the information contained in this news
release.
This release includes certain statements that may be deemed "forward-looking statements". All
statements in this release, other than statement of historical facts that address future production,
reserve potential, exploration drilling, exploitation activities and events or developments that the
Company expects re forward-looking statements. Although the Company believes the expectations
expressed in such forward-looking statements are based on reasonable assumptions, statements are
not guarantees of future performance and actual results or developments may differ materially from
the forward-looking statements. Factors that could cause actual results to differ materially from those
in forward-looking statements include market prices, exploitation and exploration successes,
continued availability of capital and financing, general economic, market or business conditions.
Investors are cautioned that any such statements are not guarantees of future performance and those
actual results or developments may differ materially from those projected in the forward-looking
statements.
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