Decade Samples High Gold-Copper on the Bonaparte Property in Kamloops Mining Division Highlights of the grab sampling program include: 1662 g/t Au and 0.88% Cu. 175.37 g/t Au and 2.267 % Cu. 82.3 g/t Au and 1.548 % Cu. 15.02 g/t Au and 5.902 % Cu
Decade Samples High Gold-Copper on the
Bonaparte Property in Kamloops Mining
Division
Highlights of the grab sampling program include:
1662 g/t Au and 0.88% Cu.
175.37 g/t Au and 2.267 % Cu.
82.3 g/t Au and 1.548 % Cu.
15.02 g/t Au and 5.902 % Cu
Stewart, British Columbia--(Newsfile Corp. - October 30, 2025) -
Decade Resources Ltd.
(TSXV:
DEC) ("Decade" or the "Company") announces that it has received assay results from sampling on the
Bonaparte copper-gold property, located approximately 50km north of Kamloops, B.C., within the
Kamloops Mining Division. The Bonaparte mineral claims are located on NTS map sheet 92I/16W and
92P/1W, the centre of the property is located at 50°59'38.61" North longitude and 120°26'11.29" West
latitude. There are two reported Minfile Occurrences located on the property consisting of (Bonaparte
092 050) and (JS Molybdenite 092INE178).
The property has different target areas including:
1
.
Cu/Au/Mo porphyry potential
2
.
Bulk-tonnage RIRGS target with high grade gold results in historic drilling, trenching, underground
exploration**
3
.
High grade gold-copper veins.
The main area of historic exploration for gold to date was called the "Discovery area". This area is
mineral occurrence (MINFILE No. 092P 050) designated by MINFILE as a developed prospect.
Mineralization primarily occurs in a series of north-south trending quartz veins hosted mainly by a quartz
diorite intrusion. Locally, the quartz veins contain up to several per cent sulphides consisting of pyrite with
lesser chalcopyrite, pyrrhotite and molybdenite. Native gold is also evident but generally is associated
with silver-grey tellurides.
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Quartz-sulphide from the Crow vein in the 1994 bulk sample area showing chalcopyrite with minor pyrite
and fine visible gold. The white quartz is prior to the later grey sulphide bearing quartz along fractures in
the earlier material.
The sampling was conducted on exposed quartz-sulphide vein material in an open cut, the host quartz
diorite intrusive as well as altered and hornfelsed argillite in the contact areas. In addition, samples were
taken from 2018 unmarked and non-sampled drill core with quartz stringers piled near the portal, the
decline muck material and quartz veining 1 km east of the "Discovery area".
A total of 34 samples were collected as follows: 5 quartz-sulphide samples and 5 samples of quartz
diorite wall rocks were collected in the area of the 1994 bulk sample pit. Nine samples of quartz diorite 3
km east of the "Discovery area", 7 samples of hornfelsed argillite, 13 samples of NQ core and 4
samples from quartz stringers located 1 km east of the :Discovery area". Low copper and gold values
were obtained except for the quartz with chalcopyrite in the 1994 pit area. It was noted that all samples of
quartz diorite contained small amounts of chalcopyrite with analysis showing 0.01 to 0.02 % copper.
Highlights of the sampling is shown below:
Sample Number
Sample Type
Au g/t
Ag g/t
Cu %
Bi ppm
Te ppm
25-BP-1
Grab
175.7
78.63
2.267
139.63
218.83
25-BP-3
Grab
82.3
35.98
1.548
115.8
161.24
25-BP-4
Grab
15.02
58.3
5.902
6.27
22.86
25-BP-5
Grab
1662.2
519
0.88
675.48
>500
25-BP-7
Grab
2.45
0.58
0.006
0.66
2.1
The high bismuth and tellurium values indicate a potential for a RIRGS environment **.
The location of the high grade samples from the "Discovery area" are shown in the map and picture
below. The
"Discovery Zone" covers an area measuring 300m east-west by 350m north-south. At least 9
gold bearing quartz veins have been located to date within this area through historic trenching and
drilling. The Company QP has examined all the reported veins prior to reclamation by the previous claim
holder and confirms the veins in the following map shown below.
In 1994 a 3,700 metric ton bulk sample of mineralized vein material from surface trenching to a vertical
depth of 12.2m from an open cut on the Nutcracker, Owl, Grey Jay and Crow vein systems, with an
average grade of 25.4 g/t Au produced 3,160 ounces of gold. In 2010 a small bulk sample from the Crow
Vein was shipped to the Kinross Mill in Republic, Washington. The 364-ton sample assayed 16.3 g/t Au
(0.475 oz/t Au), yielding 161.95 troy ounces of gold. The above results are both from the BC Minfile and
a 43-101 report by R. Kemp. The Company thinks that these results can be relied on.
A historic drill hole, 15-05 located roughly 500m east of the mined area tested a coincident resistivity
and Cu-Au soil geochemical anomaly encountering quartz veins in granodiorite similar to those
encountered in the "Discovery Zone." Assay results from DDH 15-05 returned 7.88g/t gold, 38.4g/t silver
and 0.33% copper over a 1.0m core width. The 1988 soil geochemical surveys along Cooler Creek
identified many anomalous Au-Cu soil geochemical anomalies with soil results reporting up to 3,270ppb
Au and a rock grab sample of quartz vein material reporting 73.03g/t Au (2.13opt Au). The Company QP
has not verified the above results and they should not be relied on. They are included as reference data
for exploration potential.
Map is extracted from a 43-101 on the property prepared in 2019 for the previous operators by R.
Kemp, P.Geo.
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The above photo shows sampling on the Central Crow vein.
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Claim Acquisition
The Company also has staked an additional 1180 ha to cover an area that had historic silt sampling that
yielded 1230 ppb gold draining an area east of the 'Discovery area". Exploration by the Company has
indicated the presence of quartz diorite in the drainage area that may be responsible for the anomalous
results.
Management Commentary
Ed Kruchkowski, President of Decade Resources, stated:
"The Bonaparte Gold project is an exciting addition to the Company portfolio of properties with
geological merit. The presence of at least nine (9) gold bearing quartz veins in an area measuring 300m
X 350m in size open to extension along strike and to depth where multi ounce gold assays have been
intersected in historic drilling presents a large exploration target. The presence of historical copper and
gold soil geochemical results extending to the southeast from the "Discovery Zone" approximately 1 km
away, where gold in soil results are reported with up to 3,270ppb Au as well as prospecting uncovering a
quartz vein float sample which assayed 73.03g/t Au extends the exploration area even farther. Drilling in
2015 as reported in the 43-101 report confirms that additional gold bearing quartz veins can be located
outside of the "Discovery Zone" 500m east in the Cooler Creek area."
All samples were prepared at MSA Labs' preparation laboratory in Terrace, B.C., and assayed at MSA
Labs' geochemical laboratory in Langley, B.C. Gold was assayed using a fire assay with atomic
absorption (AA) spectrometry finish. Samples over 25 parts per million gold were fire assayed with
gravimetric finish. All samples were analyzed by four-acid digestion with multielement ICP-MS, with silver
and base metal overlimits being reanalyzed by emission spectrometry. MSA Labs' quality system
complies with the requirements for the international standards ISO 17025 and ISO 9001. MSA Labs is
independent of the company.
Qualified Person
Ed Kruchkowski, P.Geo., President of Decade Resources Ltd., is a Qualified Person as defined by
National Instrument 43-101 and has reviewed and approved the technical contents of this news release.
He also conducted the sampling reported in this press release.
About Decade Resources Ltd.
Decade Resources Ltd. is a Canadian based mineral exploration company actively seeking
opportunities in the resource sector. Decade holds numerous properties at various stages of
development and exploration from basic grass roots to advanced ones. Its properties and projects are
all located in the "Golden Triangle" area of northern British Columbia. or at For a complete listing of the
Company assets and developments, visit the Company website at
www.decaderesources.ca
. For
investor information please call the Company at
250- 636-2264 or Gary Assaly at 604-377-7969.
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.
Forward-Looking Statements
This release includes certain statements and information that may constitute forward-looking information
within the meaning of applicable Canadian securities laws. All statements in this news release, other
than statements of historical facts, including statements regarding future estimates, plans, objectives,
timing, assumptions or expectations of future performance, including without limitation, that the Company
will receive regulatory approval of the Option, the exercise of the Option, exploration plans for the
Property and the use of funds for the recently completed private placement are forward-looking
statements and contain forward-looking information. Generally, forward-looking statements and
information can be identified by the use of forward-looking terminology such as "intends" or
"anticipates", or variations of such words and phrases or statements that certain actions, events or
results "may", "could", "should" or "would" or occur.
Forward-looking statements are based on certain material assumptions and analysis made by the
Company and the opinions and estimates of management as of the date of this press release, including
that Company will be able to receive regulatory approval for the Option, that the Company will be able or
willing to make the Option Payments in order to exercise the Option, that the Company will have the
necessary funds and resources to conduct its exploration plans on the Property and that the Company
will use the proceeds from the private placement as anticipated.
These forward-looking statements are subject to known and unknown risks, uncertainties and other
factors that may cause the actual results, level of activity, performance or achievements of the Company
to be materially different from those expressed or implied by such forward-looking statements or
forward-looking information. Important risks that may cause actual results to vary, include, without
limitation, the risk that the Company is unable to receive regulatory approval for the Option Agreement;
that the Company may be unable or unwilling to make all Option Payments and exercise the Option; that
the Company may be unable to conduct its exploration plans on the Property as anticipated, or at all; and
that the Company may not use the proceeds from the private placement as anticipated.
Although management of the Company has attempted to identify important factors that could cause
actual results to differ materially from those contained in forward-looking statements or forward-looking
information, there may be other factors that cause results not to be as anticipated, estimated or
intended. There can be no assurance that such statements will prove to be accurate, as actual results
and future events could differ materially from those anticipated in such statements. Accordingly, readers
should not place undue reliance on forward-looking statements and forward-looking information.
Readers are cautioned that reliance on such information may not be appropriate for other purposes. The
Company does not undertake to update any forward-looking statement, forward-looking information or
financial outlook that are incorporated by reference herein, except in accordance with applicable
securities laws.
References
Logan, J.M., and Mihalynuk, M.G., 2013. Bonaparte gold: another 195 Ma Au-Cu porphyry deposit in southern British Columbia? In: Geological
Fieldwork 2012, British Columbia Ministry of Energy, Mines and Natural Gas. British Columbia Geological Survey Paper 2013-1, 71-80.
Minfile BC
NI 43-101 Technical Report on the Bonaparte Gold Project by R. Kemp, P.Geo.
**Reduced intrusion-related gold systems (RIRGS) are characterized by widespread arrays of sheeted auriferous quartz veins that preferentially
form in the brittle carapace at the top of small plutons, where they form bulk-tonnage, low-grade Au deposits characterized by a Au-Bi-Te-W metal
assemblage, such as the Fort Knox and Dublin Gulch deposits.
https://www.researchgate.net/publication/277131625_Reduced_Intrusion-
related_Gold_Systems
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