PJX Resources’ Drilling Identifies Sedimentary Exhalative (SEDEX) Mineralization
TSX VENTURE: PJX.V
OTCQB: PJXRF
PJX RESOURCES’ DRILLING IDENTIFIES SEDIMENTARY EXHALATIVE (SEDEX)
MINERALIZATION
Toronto, Ontario – November 12, 2024 – PJX Resources Inc. (“PJX” or the “Company”) is pleased to announce
that drilling at the Dewdney Trail Property has intersected multiple mineralized sedimentary horizons, a
mineralized vent breccia /fragmental, and a chaotic fault scarp breccia with large blocks and fragments of
sediments, some containing zinc mineralization. Geology and mineralization encountered during drilling and
mapping supports a Sedimentary Exhalative (Sedex) environment with potential to host a deposit. The drill core
continues to be logged and sampled. Sample results along with sections and maps will be released when
analyses are received and compiled.
Dave Pighin, consultant and former Cominco geologist, commented, “ What has been intersected i s impressive
as it indicates a large mineralizing system. Large systems support the potential to discover significant deposits.
Drilling this part of the Dewdney Trail Property is similar to drilling across the Sullivan Sedimentary Basin on
strike with the Sullivan Deposit.”
Mineralized Sedimentary Beds/Horizons
Sixteen holes totaling 5100 metres were drilled over a period of 2.5 months until the middle of October. Sedex
type mineralized beds or bands were intersected sporadically within about 500 metres of the stratigraphic
column that was tested during this first phase of drilling . Sixteen semi-massive to massive sulphide beds,
ranging in thickness from 3 cm to 30 cm, were encountered in the upper half of the stratigraphy. These sulphide
beds are predominantly pyrrhotite/pyrite (iron sulphides). Some beds or bands contain minor visible sphalerite
(zinc sulphide), galena (lead sulphide) and/or chalcopyrite (copper sulphide) (see photo A below).
Beneath the historical Estella mine, which is near the base of the 500 metres of the stratigraphic column tested,
there appears to be 2 Sedex horizons where the frequency of sulphide beds and mineralization is greater and
may represent a more robust mineralizing period during the formation of the sedimentary basin. These
horizons appear to range in true thickness from 8 metres to 12 metres. The Sedex horizons are about 30.0
stratigraphic metres apart.
Photo A – Bedding conformable semi -massive sulphide mineralization - predominantly iron sulphide (pyr ite) with minor
copper sulphide (chalcopyrite) and zinc sulphide (sphalerite).
Mineralized Feeder Vent Breccia
Drilling supports the view that the mineralized breccia/fragmental first intersected and announced in a news
release dated September 5th, 2024, is a possible discordant feeder vent estimated to be about 10 metres in true
thickness. Vents are important in the formation of deposits as they provide a pathway for iron, copper, zinc and
other sulphides to rise along and form Sedex style bedding conformable mineralization. The vent mineralization
is predominantly iron sulphide (pyrrhotite and pyrite) that locally contain s visible amounts of copper sulphide
(chalcopyrite) and zinc sulphide (sphalerite), as well as fragments of iron sulphide mineralization (see photos B
and C). These styles of mineralization support a venting environment where sulphide mineralization is exhaled
on to an ocean floor or replaced sediment beds in the immediate stratigraphy below the ocean floor.
Photo B – Breccia/Fragmental unit with iron sulphide (pyrrhotite and pyrite) and copper sulphide (chalcopyrite) in the
matrix.
Photo C – Breccia/Fragmental unit with iron sulphide (pyrrhotite and pyrite) in the matrix and locally as iron sulphide clasts.
Iron
Sulphide
Clasts
Zinc in Outcrop
Drilling and additional mapping confirms that z inc mineralization discovered in outcrop late last year (photo D),
occurs as large blocks of sedimentary rock, about 10 m etres in size , that are part of a chaotic breccia. The
chaotic breccia most likely formed along a fault scarp when the seafloor was breaking apart along faults and
forming sub-basins. The large blocks of sediments, some containing mineralization, presumably broke along
these escarpments and collapsed into the developing extensional basins in the seafloor.
The large blocks of sediment with zinc mineralization occur about halfway up the mountain slope. The source of
the blocks is expected to be higher in the stratigraphy and, hence, at higher elevations on the mountain. Higher
elevations were not drilled this year because of freezing water line potential and for worker safety during freeze
up when clouds and weather can limit helicopter support. The chaotic breccia with zinc mineralization in large
blocks of sediments is additional support of a Sedex deposit type environment. A similar chaotic breccia occurs
proximal to the Sullivan deposit.
Photo D – Outcrop Grab Sample G23-669B (5.57% zinc, 0.94% lead, 4.41 g/t silver) Reddish-brown coloured wispy bands
and beds of sphalerite (zinc sulphide) occur in a large block of sediment (10 m etres in size) in a chaotic breccia at surface.
Boulders in Talus with Sullivan Style and Grade of Mineralization
Boulders with Sedex mineralization similar in style and grade to the Sullivan deposit were discovered late last
year in talus at the base of the mountain slope and announced in a PJX news release October 12, 2023 (see
photo E). The Sedex style of massive sulphide mineralization intersected by drilling is more iron sulphide
dominant than the semi-massive to massive zinc-lead-silver and critical metal-rich sulphide boulders at the base
of the mountain slope. The source of the boulders may be from higher on the mountain slope than was tested
by drilling ; possibly from the Kootenay King stratigraphic horizon that occurs higher on the mountain.
Alternatively, the source of the boulders may be to the south of the ir current location. This would be higher in
the cirque and possibly on strike with the 2 mineralized horizons encountered beneath the historical Estella
Mine mentioned above.
Photo E - Sample STM-23-1 (6.71% zinc, 2.23% lead, 16.05 g/t silver, 1258.9 ppm or 0.12% copper) Strongly
magnetic boulder found in talus at base of the mountain slope late last year. Sphalerite (zinc sulphide), galena
(lead sulphide), and iron sulphides (pyrite, pyrrhotite) occur banded or bedded in a ppearance as seen above.
The mineralization also occurs in the groundmass of the rock.
John Keating, President of PJX, commented, “Drilling confirms that we are in a geological environment
favourable to host a Sedex type deposit, possibly similar to the historical Sullivan Sedex deposit located 20 km to
the west , or to the historical Kootenay King Sedex deposit located 4.5 km along strike to the south. While
Sullivan style and grade mineralization discovered in boulders at the base of the mountain slope last year were
not encountered, their presence along with the large mineralizing system encountered by preliminary drilling
supports the potential to discover a deposit in the vicin ity. At present we believe the source of the boulders
may be higher on the mountain and/or higher in the cirque. We will be in a better position to vector to a source
when all the sample analyses are received and data compiled. PJX has an exploration permit in place that is
good for 5 years.”
PJX’s New Discovery Potential Background
PJX owns 100% of the mineral rights to multiple properties totaling over 680 km² of mineral claims in the
Sullivan Mining District of Southeastern British Columbia, Canada. Exploration in late 2023 discovered boulders
and outcrop of Sullivan deposit style and grade mineralization on PJX’s Dewdney Trail Property that is over 150
km² in size. The zinc, lead, silver, and other critical metal mineralization discovered at surface on the Dewdney
Trail Property is magnetic and appears to be associated with a strong to moderate magnetic airborne
geophysical anomaly that can be traced for approximately 1.6 km. This recent first phase of drilling on part of
the anomalous trend confirms a geological environment with sulphide mineralization that supports the potential
to discover a Sedex type deposit.
The geological disclosure and content of this news release has been reviewed and approved by Dave Pighin,
P.Geo., and John Keating P.Geo. (qualified persons for the purpose of National Instrument 43 -101 Standards of
Disclosure for Mineral Projects). Mr. Pighin is one of a number of consulting geologists for PJX on the D ewdney
Trail Property. Mr. Keating is the President, Chief Executive Officer and a Director of PJX.
About PJX Resources Inc.
PJX is a mineral exploration company focused on building shareholder value and community opportunity through the
exploration and development of mineral resources with a focus on gold, silver , zinc, lead, copper, cobalt, and other critical
metals. PJX’s properties are located in the historical Sullivan Mine District and Vulcan Gold Belt near Cranbrook and
Kimberley, British Columbia.
Please refer to our web site http://www.pjxresources.com for additional information.
FOR ADDITIONAL INFORMATION PLEASE CONTACT:
Linda Brennan, Chief Financial Officer
(416) 799-9205
Cautionary Note Regarding Forward-Looking Information
The information in this news release has been prepared as at the date noted above. Certain statements in this news release, referred to herein as
"forward-looking statements", constitute "forward -looking statements" under the provisions of Canadian provincial securities laws. These
statements can be identified by the use of words such as "expected", "may", "will" or similar terms.
Forward-looking statements are necessarily based upon a number of factors and assumptions that, while considered reasonable by PJX
Resources Inc. as of the date of such statements, are inherently subject to significant business, economic and competitive uncertaintie s and
contingencies. Many factors, known and unknown, could cause actual results to be materially different from those expressed or implied by suc h
forward-looking statements. Readers are cautioned not to place undue reliance on these forward -looking statements, which speak only as of
the date made. Except as otherwise required by law, PJX Resources Inc. expressly disclaims any obligation or undertaking to release
publicly any updates or revisions to any such statements to reflect any change in PJX Resources Inc.’s expectations or any change in events,
conditions or circumstances on which any such statement is based.
Cautionary Note to US Investors:
This news release may contain information about adjacent properties on which PJX Resources Inc. has no right to explore or mi ne. We advise U.S.
investors that the SEC's mining guidelines strictly prohibit information of this type in documents filed with the SEC. U.S. i nvestors are cautioned
that mineral deposits on adjacent properties are not indicative of mineral deposits on our properties. This news release may contain forward-
looking statements including but not limited to comments regarding the timing and content of upcoming work programs, geologic al
interpretations, receipt of property titles, potential mineral recovery processes, etc. Forward -looking statements address future events and
conditions and therefore involve inherent risks and uncertainties. Actual results may differ materially from those currently anticipated in such
statements.
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accepts responsibility for the adequacy or accuracy of this release.