Forge Resources Drilling Points to Multiple Porphyry Centres Across 4 KM at Alotta
Forge Resources Drilling Points to Multiple
Porphyry Centres Across 4 KM at Alotta
Vancouver, British Columbia--(Newsfile Corp. - September 15, 2026) -
Forge Resources Corp.
(CSE:
FRG) (OTCQB: FRGGF) (FSE: 5YZ) ("
FRG
" or the "
Company
") is pleased to report visual results and
initial observations from drilling at the Alotta Project, including the deepest hole (ALT-26-021) drilled to
date. The Alotta Project, located within Yukon's Dawson Range Gold Belt, is one of several Late
Cretaceous, gold-enriched porphyries that include the Casino and Revenue-Nucleus deposits.
The 2026 drill program focused on targeting interpreted porphyry centres, which are prospective for
porphyry-style mineralization and are thought to be responsible for the gold-enrichment confirmed at the
Payoff and Severance zones (Figure 1). Several holes were designed to test geophysical anomalies
identified during pre-season data compilation. Holes ALT-26-017, -018 and -021 all successfully
intercepted significant porphyry veining and alteration over extensive core lengths.
Highlights
:
2,792 metres drilled in six holes
at the Commission, Payoff and Severance zones, completing
the 2026 program at Alotta.
Mineralization and alteration have been intersected in every hole drilled at Alotta to date
-
across a footprint more than 4 km long, consistent with several porphyry centres rather than a
single centre.
ALT-26-021 is the deepest hole on the Property at 651 m.
It was mineralized and altered
through the entire length of the hole, including biotite, magnetite and chlorite alteration and
pyrite±pyrrhotite-molybdenite-chalcopyrite mineralization.
Vein density and magnetite content increase with depth in ALT-26-018 and -021
, a pattern
typically developed nearing porphyry centres.
Visible gold was intersected at the Payoff Zone
(ALT-26-020, 217 m), adding to the previously
reported occurrences of visible gold in the zone.
ALT-26-019 tested the Severance Zone
and intersected propylitic altered porphyry with
abundant pyrite ± pyrrhotite and minor molybdenite and chalcopyrite.
Assays are pending
and will be released once received, compiled and interpreted.
PJ Murphy, CEO of Forge Resources
, states
: ""Alotta continues to get bigger, not smaller. Each
season we've added ground to the story rather than narrowing it, and the picture that's emerging is of a
large system with several distinct centres rather than a single target, which is exactly the kind of setting
that has produced the major deposits in this part of the Yukon"
Figure 1
. Alotta Project overview
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ALT-26-017, 018 and 021 - Commission Zone
Holes
ALT-26-017, -018 and -021
were drilled to test a geophysical anomaly defined during 3D
magnetic inversion modelling undertaken prior to the 2026 drill program. This anomaly is thought to be
one of possibly several centres responsible for the large geochemical and geophysical footprint of the
mineralization discovered to date. All three holes intersected significant amounts of porphyry type
veining and alteration throughout much of their lengths. A high density of veining is observed in all three
holes, with vein density increasing at depth in holes 018 and 021 (Photos 1 to 3). An increase in
magnetite, both as disseminations in altered porphyry and within quartz-pyrite veins, is evident in all
three holes.
Photo 1
. High density of quartz and quartz-sulphide veins at 430 m depth from hole ALT-26-018.
Sulphides include pyrite, pyrrhotite ± chalcopyrite ± molybdenite.
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Photo 2.
Significant density of quartz, sulphide and quartz-sulphide veins developed within strongly
altered porphyry from 193.5 m in hole ALT-26-021.
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Photo 3
. Quartz vein with K-feldspar alteration halo hosting molybdenite, pyrite and pyrrhotite. 630 m
depth from hole ALT-26-021.
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ALT-26-016 and ALT-26-020 - Payoff Zone
Hole ALT-26-016 was designed to test a 3D magnetic anomaly to the west of previous drilling at the
Payoff Zone.
The hole intersected porphyritic rocks at the top of the hole before transitioning into
granodiorite. Mineralization was observed throughout the hole. Semi-massive arsenopyrite and blebby
sphalerite occur within quartz veins showing localized epithermal textures, and as disseminations, in the
top 80 metres. Common mineralized stringers and veins of pyrite-pyrrhotite ± molybdenite occur along
the length of the hole (Photos 4 and 5).
Photo 4.
ALT-26-016, 45 m. Banded quartz-carbonate veins hosting pyrite, sphalerite and
arsenopyrite within altered porphyry.
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Photo 5.
ALT-26-016, 78 m. Chlorite altered porphyry hosting patchy semi-massive arsenopyrite and
pyrite.
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ALT-26-020 was drilled to the east of previous drilling at the Payoff Zone to test for gold-enriched
mineralization. As previously reported (News Release dated August 25, 2026), visible gold was
intercepted in the hole at a depth of 217 m, adding to the numerous occurrences of visible gold at the
Payoff Zone (Photo 6). Strong mineralization was observed throughout the hole, including an increase in
pyrite, pyrrhotite and local chalcopyrite deeper in the hole (Photo 7).
Photo 6
. ALT-26-020, 217 m. Grains of visible gold hosted in a 1 cm wide quartz vein within strongly
biotite and silica altered porphyry.
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Photo 7
. ALT-26-020, 301 m. Chalcopyrite with pyrrhotite in strongly altered porphyry.
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ALT-26-019 - Severance Zone
Hole ALT-26-019 tested the Severance Zone, where a multi-element soil geochemical anomaly and the
highest-grade rock sample collected on the Property (0.35% copper and 1.2 g/t gold) define the surface
expression of the zone. The hole intersected altered and mineralized porphyritic rocks along the majority
of its length, with abundant epidote and chlorite alteration and intervals of sericite. The hole also
intersected several large fault zones that cut across the porphyry veining and associated alteration. The
significance of the fault zones is yet to be determined, but they appear to juxtapose lower-temperature
parts of the system against higher-temperature parts, and may have increased the depth of oxidation.
Significant carbonate and quartz-carbonate veining was observed throughout the hole, which appears to
be associated with the faults (Photos 8 and 9).
Some of these veins exhibit epithermal textures.
Photo 8
. Quartz-carbonate-pyrite veins within sericite altered porphyry from hole ALT-26-019. 37 m
depth.
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Photo 9
. Carbonate alteration and veining cutting quartz-pyrite veins from hole ALT-26-019. 300 m
depth.
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Interpretation - A Multi-Centre System
Drilling to date at the Alotta Property has shown that multiple porphyry centres are likely present.
Overprinting alteration assemblages are common in drill core and likely reflect the multi-centre nature of
the system. These multiple centres likely contribute to the gold enrichment observed in the Payoff Zone
(Figure 2).
Figure 2.
Conceptual model of the porphyry system at the Alotta Property. Overprinting alteration
zones are common in core and may have direct implications for observed gold enrichment in the
Payoff Zone. Approximate location of holes ALT-26-019, 020 and 021. Modified from Sillitoe (2010).
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Quality Assurance/Quality Control
Analytical work is being completed by ALS Canada Ltd., with sample delivery and preparation in
Whitehorse, Yukon, and geochemical analysis in North Vancouver, British Columbia.
Rigorous procedures are in place regarding sample collection and data entry. Certified assay
standards, coarse reject duplicates, field duplicates and blanks are routinely inserted into the sample
stream to ensure integrity of the assay process. Core is being sampled using a diamond core saw, with
half of each interval sent to the lab for analysis and the other half retained.
Half-core samples received at ALS are fine-crushed and a 250 g split was pulverized to better than 85%
passing 75 microns. Gold was determined for core samples using a 50 g charge by fire assay followed
by an atomic absorption spectroscopy finish (Au-AA24). The fine fraction was analyzed for 48 elements
using a four acid digestion followed by inductively coupled plasma combined with mass spectroscopy
and atomic emission spectroscopy finish (ME-MS61).
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 (Standards of Disclosure for Mineral
Projects) and was reviewed and approved by Kelson Willms, P.Geo., of Archer, Cathro & Associates
(1981) Limited. Mr. Willms is a Qualified Person for the purposes of National Instrument 43-101.
About Forge Resources Corp.
Forge Resources Corp. is a Canadian-listed junior exploration company focused on exploring and
advancing the Alotta Project, a prospective porphyry copper-gold-molybdenum project consisting of 230
mineral claims that cover 4,723 hectares, located 50 km southeast of the Casino porphyry deposit in the
unglaciated portion of the Dawson Range porphyry/epithermal belt in the Yukon Territory of Canada.
In addition, the Company holds an 80% interest in Aion Mining Corp., a company that is developing the
fully permitted La Estrella coal project in Santander, Colombia. The project contains eight known seams
of metallurgical and thermal coal.
On behalf of the Board of Directors
"PJ Murphy", CEO Forge Resources Corp.
Forward-Looking Statements
Certain of the statements made and information contained herein may contain forward-looking
information within the meaning of applicable Canadian securities laws. Forward-looking information
includes, but is not limited to, information concerning the Company's intentions with respect to the
development of its mineral properties. Forward-looking information is based on the views, opinions,
intentions and estimates of management at the date the information is made, and is based on a
number of assumptions and subject to a variety of risks and uncertainties and other factors that could
cause actual events or results to differ materially from those anticipated or projected in the forward-
looking information (including the actions of other parties who have agreed to do certain things and
the approval of certain regulatory bodies). Many of these assumptions are based on factors and
events that are not within the control of the Company and there is no assurance they will prove to be
correct. There can be no assurance that forward-looking information will prove to be accurate, as
actual results and future events could differ materially from those anticipated in such information. The
Company undertakes no obligation to update forward-looking information if circumstances or
management's estimates or opinions should change except as required by applicable securities laws,