View ValuationPJX Resources 将来の成長Future 基準チェック /06現在、 PJX Resourcesの成長と収益を予測するのに十分なアナリストの調査がありません。主要情報n/a収益成長率n/aEPS成長率Metals and Mining 収益成長13.9%収益成長率n/a将来の株主資本利益率n/aアナリストカバレッジNone最終更新日n/a今後の成長に関する最新情報更新なしすべての更新を表示Recent updatesお知らせ • Apr 29PJX Resources Inc., Annual General Meeting, Jun 24, 2026PJX Resources Inc., Annual General Meeting, Jun 24, 2026. Location: ontario, toronto Canadaお知らせ • Aug 01PJX Resources Inc. announced that it has received CAD 1.65246 million in fundingOn July 31, 2025, PJX Resources Inc. closed the transaction. The company announced that it has issued 4,714,286 flow-through unit at an issue price of CAD 0.14 per unit for gross proceeds of CAD 660,000.04 and 2,000,000 Units on a non-flow through basis at an issue price of CAD 0.12 per unit for gross proceeds of CAD 240,000; aggregate gross proceeds of CAD 900,000.04 in second and final tranche. Each Flow Through Unit consists of one common share and one common share purchase warrant. Each Unit consists of one common share and one common share purchase warrant. Each warrant acquired, whether with a Flow Through Unit or a Unit, will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following the date of issuance. Certain directors of company, participated in the private placement. Finders’ fees comprised of CAD 36,236 cash and 283,520 non-transferable warrants may be paid in respect of the first tranche of the Private Placement. The warrants will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following issuance. No Finders’ fees were paid in respect to the second tranche. All securities issuable in connection with the Private Placement will be subject to a statutory hold period in Canada which will run for four months from the date of issuance. The Private Placement is subject to compliance with applicable securities laws and to receipt of the final approval and acceptance of the TSX Venture Exchange. The company has offered 12,430,905 units of the Company for gross proceeds of CAD 1,652,460 in connection with the transaction.お知らせ • Jul 10PJX Resources Inc. announced that it expects to receive CAD 1.65246 million in fundingPJX Resources Inc. announces a non brokered private placement to issue 12,430,905 units of the Company for gross proceeds of CAD 1,652,460 on July 9, 2025. The Company will issue units on a “flow through” basis and a non-flow through basis. The subscription prices for each of the foregoing are CAD 0.14 per Flow Through Unit and CAD 0.12 per Unit. The offering has been fully allocated and is expected to close on or about July 15, 2025. Each Flow Through Unit consists of one common share to be issued as a "flow-through share" within the meaning of the Income Tax Act (Canada) and one common share purchase warrant. Each Unit consists of one common share and one common share purchase warrant. Each warrant acquired, whether with a Flow Through Unit or a Unit, will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the Private Placement. Finders fees comprised of cash and non-transferable Warrants may be paid in respect of the Private Placement. The Warrants will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the Private Placement.お知らせ • Apr 29PJX Resources Inc., Annual General Meeting, Jun 26, 2025PJX Resources Inc., Annual General Meeting, Jun 26, 2025. Location: ontario, toronto Canadaお知らせ • Jan 17PJX Resources Inc.'s Drilling Confirms the Geological Potential to Develop A Sedex Deposit on the Dewdney Trail PropertyPJX Resources Inc. announced that drilling has identified 3 Sedimentary Exhalative (Sedex) horizons with each horizon having the potential to host a Sedex type deposit at depth and on strike. The horizons are defined by increased sulphide mineralization in the form of stacked narrow massive to semi massive sulphide beds, bands, and/or disseminated sulphides. Iron rich minerals (pyrrhotite and pyrite) are dominant with lesser concentrations of copper (chalcopyrite), zinc (sphalerite) and/or lead (galena). Drilling explored for the source of Sullivan style and grade mineralized boulders (Photo A) found in talus material at the base of a mountain slope on PJX's 100% owned Dewdney Trail Property in the Sullivan Mining District near Cranbrook, British Columbia, Canada. Although the source of the boulders was not encountered during this initial phase of drilling, the geological environment discovered by drilling supports an environment similar to the Sullivan basin hosting the Sullivan deposit. Features include stacked bedding conformable sulphides, syn-sedimentary faults defined by large blocks of zinc mineralized sediments in a chaotic breccia (Photo B), and a cross cutting vent (Photo C) that can function as a conduit to transport metals for the formation of deposits. The sulphide flooded vent intersected while drilling is predominantly iron sulphide with locally significant copper sulphide and less zinc or lead sulphide (see photo C and grades below). This combination of sulphides suggests a hotter part of the mineralizing system. The source of the more zinc and lead rich Sullivan style and grade boulders would likely be in a cooler part of the system. This could be higher in the mineralizing system, which is higher on the mountain slope above where we have drilled. The Kootenay King quartzite horizon, which hosts the Kootenay King sedex zinc-lead-silver deposit 6.5 km on strike to the south, occurs higher on the mountain and has not yet been drilled. Cooler parts of the mineralizing system that may be favourable for forming a zinc-lead-silver deposit, may also occur laterally away from the vent as shown by the location of sphalerite and galena in replacement ore. The 3 Sedex horizons encountered in drilling may be favourable mineralizing periods to form a deposit on strike and laterally away from the vent area. Two Sedex horizons occur in the footwall beneath the Estella workings at the base of the mountain. The third Sedex horizon occurs about one third of the way up the mountain slope. Drilling commenced in early August last year after the exploration permit amendment was received from the government in mid-July, 2024. The exploration permit is good until July 2029. Further assessment of the results along with geophysics will be undertaken this winter to help define drill pad locations to test the various targets. Additional information will be provided when available. 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.お知らせ • Dec 04PJX Resources' Dewdney Trail Property Sedex Deposit Potential UpdatePJX Resources Inc. announced that iron rich minerals (pyrrhotite and pyrite) with copper (chalcopyrite) and minor to trace zinc (sphalerite) and lead (galena) discovered in a venting geological environment by recent drilling appears consistent with mineralisation typically found within a vent beneath Sedex (Sedimentary Exhalative) type zinc-lead-silver mineralisation. This first phase of drilling commenced in August this year after PJX received a five year permit to explore and drill the large Dewdney Trail Property near Cranbrook, BC. Sedex deposits typically form where metal rich fluids rise from depth along pathways called vents that occur along faults. Deposit models suggest zinc and lead minerals (sphalerite and galena) are first to be deposited. Iron and copper rich mineralisation rise later along the vent and sometimes replace and/or remobilize zinc and lead and carry them higher in the venting system. The result is a zone of Sedex style zinc-lead-silver mineralisation above and/or laterally away from the location of iron and copper mineralisation. More drilling is required higher in the venting system which is higher on the mountain and laterally on strike to the south and north. 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 John Keating P.Geo. (qualified person for the purpose of National Instrument 43-101 Standards of Disclosure for Mineral Projects). Mr. Keating is the President, Chief Executive Officer and a Director of PJX.お知らせ • Nov 13PJX Resources Inc. Announces Drilling Identifies Sedimentary Exhalative (Sedex) MineralizationPJX Resources Inc. announced 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. 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). 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. Mineralized Feeder Vent Breccia: Drilling supports the view that the mineralized breccia/fragmental first intersected and announced in a news release dated September 5, 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 contains visible amounts of copper sulphide (chalcopyrite) and zinc sulphide (sphalerite), as well as fragments of iron sulphide mineralization. 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. Zinc in Outcrop: Drilling and additional mapping confirms that zinc mineralization discovered in outcrop late 2023, occurs as large blocks of sedimentary rock, about 10 metres 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. 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. 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 their current location.お知らせ • Sep 05PJX Resources Inc.'S Drilling Identifies Venting Type Environment That Supports Sullivan Style Sedex MineralisationPJX Resources Inc. announced that on-going drilling at the Dewdney Trail Property has encountered geology that supports the potential to discover a Sedimentary Exhalative (Sedex) type deposit. Of the 3 holes drilled to date the deepest into the mountain has intersected a 20m (estimated true width) fragmental with abundant to semi-massive sulphide mineralisation at 275m. The mineralisation appears to be predominantly iron sulphide (pyrrhotite and pyrite) with visible trace amounts of copper sulphide (chalcopyrite) and zinc sulphide (sphalerite). This style of mineralisation supports a venting environment, which is what occurs at the Sullivan Sedex deposit located approximately 20 km west of the Dewdney Trail Property in Southeastern British Columbia, Canada. Fragmental unit with iron sulphide (pyrRhotite and pyrite") in the matrix and what appear to be iron sulphide clasts in places. Zinc sulphide (sphalerites) and copper sulphide (chal copyrite) are locally visible in trace amounts (samples have been sent for analysis). The source of the Sullivan style and grade zinc, lead, and silver mineralisation discovered late last year at surface in boulders in talus material at the base of a mountain slope has not yet been identified by drilling. In addition, the zinc and lead mineralisation in outcrop discovered late last year appears to occur in large blocks and/or fragments of stratigraphy that may have collapsed into a sinking basin which can happen in Sedex environments. 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 mineralisation on PJX's Dewdney Trail Property that is over 150 km2 in size. The zinc, lead, silver, and other critical metal mineralisation 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. The mineralisation and geophysical anomaly have never been drilled. 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).お知らせ • Apr 21PJX Resources Inc., Annual General Meeting, Jun 18, 2024PJX Resources Inc., Annual General Meeting, Jun 18, 2024.お知らせ • Apr 16PJX Resources Inc. announced that it expects to receive CAD 3.6 million in fundingPJX Resources Inc. announces non brokered private placement 4,444,444 Flow Through Units at a issue price of CAD 0.36 per Flow Through Unit for gross proceeds CAD 1,599,999.84, 6,666,667 Strategic Units at a issue price of CAD 0.225 per Strategic Unit for gross proceeds CAD 1,500,000.075, 2,500,000 Non-Strategic Units at a issue price of CAD 0.20 per Non-Strategic Unit for gross proceeds of CAD 500,000 resulting aggregate gross proceeds of CAD 3,599,999.915 on April 15, 2024. Each Flow Through Unit consists of one common share and one-half of one common share purchase warrant. Each whole warrant acquired as part of a Flow Through Unit will entitle the holder to purchase one common share at an exercise price of CAD 0.45 for 24 months following completion of the Private Placement. Each Strategic Unit and Non-Strategic Unit consists of one common share and one-half of one common share purchase warrant. Each whole warrant acquired as part of a Strategic Unit will entitle the holder to purchase one common share at an exercise price of CAD 0.45 for 24 months following completion of the Private Placement. The transaction will include participation from Linda Brennan and James Clare, directors of company have subscribed for a total of 375,000 Non-Strategic Units. The securities issuable in connection with the Private Placement will be subject to a statutory hold period in Canada which will run for four months from the date of the respective closings of the Private Placement. The component of the Private Placement that has not already been completed, being the issuance of the Non-Strategic Units, is expected to close on April 15, 2024. The Private Placement is subject to compliance with applicable securities laws and to receipt of the final approval and acceptance of the TSX Venture Exchange.お知らせ • Jan 15Pjx Resources Inc. Discovers 5.57% Zinc Mineralization in Outcrop Above Recently Discovered Sullivan Style Massive Sulphide BouldersPJX Resources Inc. announced recently received results of significant zinc and lead mineralization in outcrop that further supports the potential to discover a Sullivan type deposit on the Company's Dewdney Trail Property in the Sullivan Mining District in southeastern British Columbia, Canada. Two rock samples taken from outcrop, G23-699B and G23-699C below, returned values of 5.57% zinc, 0.94% (9450ppm) lead, 4.41g/t (4.41ppm) silver, and 4.72% zinc, 1.28% lead, 6.07g/t (6.07ppm) silver, respectively. The sediment hosted zinc and lead mineralization appears as bands or beds. The bedrock exposures of mineralization occur upslope and north of semi-massive to massive sulphide boulders containing Sullivan deposit style and grade mineralization announced in the news release dated October 12, 2023. Semi-massive to massive sulphide boulderers occur in talus at the base of the mountain slope. Outcrop with sediment hosted zinc-lead-silver mineralization occurs up-slope and to the north of the boulders' location. (photo looking northeast); The strongly magnetic semi-massive to massive sulphides boulders occur at the base of the mountain slopes and on the edge of a large (about 500m diameter) strong magnetic geophysical anomaly (pink to red coulours on the airborne magnetic map) that occurs upslope from the boulders; Zinc-lead-silver sulphide mineralization in outcrop is only very weakly magnetic. This supports the potential for a vertically or laterally zoned deposit with varying magnetic signatures. The outcrop mineralization appears to be associated with a less magnetic trend (orange to red coulours) in the airborne geophysics survey that occurs for possibly 1.6 km along strike.お知らせ • Dec 11PJX Resources Inc. announced that it has received CAD 0.55125 million in fundingOn December 11, 2023, PJX Resources Inc., closed the transaction. The transaction was oversubscribed and the company issued 5,250,000 units at a price of CAD 0.105 for the gross proceeds of CAD 551,250. As a part of the transaction, the company paid CAD 40,042.08 as finder fee and 381,360 warrants.お知らせ • Dec 05PJX Resources Inc. announced that it expects to receive CAD 0.5355 million in fundingPJX Resources Inc. announced a non-brokered private placement of up to 5,100,000 units through the issuance of flow-through units at a price of CAD 0.105 per unit for gross proceeds of up to CAD 535,500 on December 4, 2023. Each flow-through unit will consist of one common share to be issued as a flow-through share and one common share purchase warrant. Each warrant will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the offering. The offering, and any modifications to it, is subject to compliance with applicable securities laws and to receipt of the approval and acceptance of the TSX-V. The company reserves the right to increase the size of the offering or to modify the type, nature and price of the units for any reason. The securities issuable in connection with this offering will be subject to a hold period in Canada which will run for four months and one day from the date of the closing of the offering. The company may pay finders' fees, in accordance with the policies of the TSX-V.お知らせ • Nov 23PJX Resources Inc. announced that it has received CAD 2.152149 million in fundingOn November 22, 2023, PJX Resources Inc. closed the transaction. The company now issued 13,816,422 Flow Through Units at a price of CAD 0.105 per Flow Through Unit for the gross proceeds of CAD 1,450,724.31 and 7,793,616 Non-flow Through Units at a price of CAD 0.09 per Unit for the gross proceeds of CAD 701,425.44; for the aggregate gross proceeds of CAD 2,152,149.75. Each Flow-through Unit consists of one common share and one common share purchase warrant. Each Unit consists of one common share and one common share purchase warrant. Each warrant, whether acquired as part of a Flow-through Unit or Unit, entitles the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the Offering. Subject to TSXV Exchange approval, Finders’ fees of CAD 30,337.20 cash and 291,709 Finders’ Warrants will be paid in relation to the completion of the Offering. The Finders Warrants will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the Offering. The securities issuable in connection with this Offering will be subject to a hold period in Canada which will run for four months from the date of the closing of the Offering. The Offering has received conditional approval from the TSXV Exchange. The transaction was oversubscribed. The transaction also included participation from certain insiders.お知らせ • Nov 15PJX Resources Inc. Announces Soil Survey Supports Potential for Copper and Gold to Be Associated with Sullivan Style Zinc-Lead-Silver DiscoveryPJX Resources Inc. announced that highly anomalous gold and copper occur in soil material along with zinc, lead, and silver up slope from the discovery of Sullivan deposit style and grade semi-massive to massive sulphide boulders. The new sediment-hosted discovery of Sullivan style zinc-lead-silver mineralization in boulders occurs on the Company's Dewdney Trail Property in the Sullivan Minng District in southeastern British Columbia, Canada. Boulders of Sullivan style and grade mineralization were discovered in an area of about 50 metres (m) by 150 m at the base of a talus slope. The boulders are strongly magnetic and appear to have not moved far down the slope of the mountain from a possible bedrock source as some are large and angular. Soil samples taken from talus material up-slope from the boulders are highly anomalous in zinc, lead, silver, gold, and copper. The soils coincide with the strong airborne magnetic anomaly immediately up-slope from the boulderers. The highly anomalous zinc, lead, silver, gold, and copper content in soils are also coincident with a moderately strong magnetic anomaly for about 500 m along strike to the north of the 500 m long strong magnetic anomaly.お知らせ • Oct 13PJX Resources Inc. Discovers Sullivan Style Massive Sulphide Mineralization with Grades Up to 9.33% Zinc, 2.48% Lead, and 14.62 G/T SilverPJX Resources Inc. announce the discovery of massive and semi-massive sulphide boulders of Sullivan deposit style zinc, lead, silver, cadmium, and indium mineralization. This significant new sediment-hosted discovery is on the Company's Dewdney Trail Property in the Sullivan Mining District in southeastern British Columbia, Canada. PJX's prospecting team discovered boulders with sulphide mineralization in an area about 50 metres (m) by 150 m at the base of a talus slope. Some sulphide boulders display layering and breccia textures with grades of zinc-lead-silver mineralization similar to ore at the Sullivan deposit. The sulphide boulders with zinc (sphalerite mineral), lead (galena), and iron (pyrite and pyrrhotite) are magnetic. The boulders occur at the base of the mountain slope and on the edge of a large magnetic anomaly identified by Expert Geophysics from the 875 line-kilometre airborne geophysical survey flown for PJX in 2021. Sample SMT-23-1 (6.71% zinc, 2.23% lead, 16.05 g/t silver, 1,258.9 ppm or 0.12% copper) Sphalerite (zinc sulphide), galena (lead sulphide), and iron sulphides (pyrite, pyrrhotite) occur in fragments that are locally banded or bedded in apearance as seen above. The mineralization also occurs in the groundmass of the rock. Sample SMT-23-8 (3.55% zinc, 0.98% lead, 7.5 g/t silver, 442.1 ppm or 0.04% copper) Although this sample is lower in grade it tells an important story. The individual massive sphalerite fragments are a possible indicator of higher grade zinc rich massive sulphides possibly buried under the talus slope. Sample SMT-23-7 (9.33% zinc, 2.48% lead, 14.62 g/t silver, 495 ppm or 0.04% copper) Alternating dark and light coloured bands with sulphides (zinc, lead, iron) appear to be sulphide-rich beds that have been broken apart possibly by slumping during deposition on the ocean floor, or the beds may have broken apart during later folding. Airborne Magnetic Map: Massive sulphide boulders occur downslope from a magnetic anomaly (red to pink area). The boulders are magnetic. The initial target area with deposit potential is defined by an elevated magnetic signature that is over 1.5 km along strike. Stronger magnetic anomalies (pink colour) may represent more iron rich (pyrrhotite mineral) zones similar to those that occur at the Sullivan deposit. Less strong magnetic anomalies (red to orange colour) may represent areas with more zinc or lead sulphide mineralization that would be more weakly magnetic. The 160 million tonne Sullivan deposit produced ore containing some 17 million tonnes of zinc and lead metal and more than 285 million ounces of silver during 90 years of operation before closing in 2001.お知らせ • Jun 30PJX Resources Inc. Commences 2023 Exploration with Discovery of New Iron-Oxide Zone That Expands Copper-Gold-Silver Potential on Dewdney Trail PropertyPJX Resources Inc. announced that field work on the Dewdney Trail Property has begun in preparation to advance and drill test copper-gold-silver mineralization associated with alkalic porphyritic intrusions discovered last year. Recent prospecting has discovered an additional iron-oxide breccia zone with localized copper mineralization. This new zone is approximately 1500 m southeast of a series of stacked bedding parallel quartz veins that contain up to 63 g/t gold. The new zone expands the potential to discover multiple gold-copper-silver and possible molybdenum deposits related to porphyry intrusions. The zone is approximately 3 km southwest of the Estella Basin where a cluster of intrusions and hydrothermal breccias occur with anomalous gold, copper, silver, molybdenum, arsenic and other elements in soils and rock samples. The zone may also be related to a large (5 km diameter) circular shaped feature defined by an 895 line-km airborne magnetic and Mobile MT (EM) survey flown by Expert Geophysics for PJX over an 80 km2 area. The Estella Basin and new breccia zone occur proximal to the rim of the circular feature that may reflect the margin of a collapsed pluton at depth. Porphyry copper-gold deposits are known to occur along the margin of plutons. このセクションでは通常、投資家が会社の利益創出能力を理解する一助となるよう、プロのアナリストのコンセンサス予想に基づく収益と利益の成長予測を提示する。しかし、PJX Resources は十分な過去のデータを提供しておらず、アナリストの予測もないため、過去のデータを外挿したり、アナリストの予測を使用しても、その将来の収益を確実に算出することはできません。 シンプリー・ウォール・ストリートがカバーする企業の97%は過去の財務データを持っているため、これはかなり稀な状況です。 業績と収益の成長予測OTCPK:PJXR.F - アナリストの将来予測と過去の財務データ ( )CAD Millions日付収益収益フリー・キャッシュフロー営業活動によるキャッシュ平均アナリスト数12/31/2025N/A-2-3-3N/A9/30/2025N/A-2-3-3N/A6/30/2025N/A-3-3-3N/A3/31/2025N/A-6-4-4N/A12/31/2024N/A-6-4-4N/A9/30/2024N/A-6-2-2N/A6/30/2024N/A-4-1-1N/A3/31/2024N/A-1-1-1N/A12/31/2023N/A-1-1-1N/A9/30/2023N/A-1-1-1N/A6/30/2023N/A-1-2-2N/A3/31/2023N/A-1-2-2N/A12/31/2022N/A-1-2-2N/A9/30/2022N/A-1-1-1N/A6/30/2022N/A-2-1-1N/A3/31/2022N/A-2-2-2N/A12/31/2021N/A-1-1-1N/A9/30/2021N/A-1-1-1N/A6/30/2021N/A-1-1-1N/A3/31/2021N/A000N/A12/31/2020N/A-2-1-1N/A9/30/2020N/A-1-1-1N/A6/30/2020N/A-2-2-2N/A3/31/2020N/A-2-2-2N/A12/31/2019N/A-2-2-2N/A9/30/2019N/A-3N/A-2N/A6/30/2019N/A-3N/A-3N/A3/31/2019N/A-3N/A-3N/A12/31/2018N/A-2N/A-2N/A9/30/2018N/A-3N/A-2N/A6/30/2018N/A-2N/A-2N/A3/31/2018N/A-2N/A-2N/A12/31/2017N/A-2N/A-3N/A9/30/2017N/A-3N/A-3N/A6/30/2017N/A-2N/A-2N/A3/31/2017N/A-2N/A-2N/A12/31/2016N/A-2N/A-1N/A9/30/2016N/A-1N/A-1N/A6/30/2016N/A-1N/A-1N/A3/31/2016N/A-2N/A-1N/A12/31/2015N/A-2N/A-2N/A9/30/2015N/A-2N/A-1N/Aもっと見るアナリストによる今後の成長予測収入対貯蓄率: PJXR.Fの予測収益成長が 貯蓄率 ( 3.5% ) を上回っているかどうかを判断するにはデータが不十分です。収益対市場: PJXR.Fの収益がUS市場よりも速く成長すると予測されるかどうかを判断するにはデータが不十分です高成長収益: PJXR.Fの収益が今後 3 年間で 大幅に 増加すると予想されるかどうかを判断するにはデータが不十分です。収益対市場: PJXR.Fの収益がUS市場よりも速く成長すると予測されるかどうかを判断するにはデータが不十分です。高い収益成長: PJXR.Fの収益が年間20%よりも速く成長すると予測されるかどうかを判断するにはデータが不十分です。一株当たり利益成長率予想将来の株主資本利益率将来のROE: PJXR.Fの 自己資本利益率 が 3 年後に高くなると予測されるかどうかを判断するにはデータが不十分です成長企業の発掘7D1Y7D1Y7D1YMaterials 業界の高成長企業。View Past Performance企業分析と財務データの現状データ最終更新日（UTC時間）企業分析2026/05/26 18:41終値2026/05/18 00:00収益2025/12/31年間収益2025/12/31データソース企業分析に使用したデータはS&P Global Market Intelligence LLC のものです。本レポートを作成するための分析モデルでは、以下のデータを使用しています。データは正規化されているため、ソースが利用可能になるまでに時間がかかる場合があります。パッケージデータタイムフレーム米国ソース例会社財務10年損益計算書キャッシュ・フロー計算書貸借対照表SECフォーム10-KSECフォーム10-Qアナリストのコンセンサス予想+プラス3年予想財務アナリストの目標株価アナリストリサーチレポートBlue Matrix市場価格30年株価配当、分割、措置ICEマーケットデータSECフォームS-1所有権10年トップ株主インサイダー取引SECフォーム4SECフォーム13Dマネジメント10年リーダーシップ・チーム取締役会SECフォーム10-KSECフォームDEF 14A主な進展10年会社からのお知らせSECフォーム8-K* 米国証券を対象とした例であり、非米国証券については、同等の規制書式および情報源を使用。特に断りのない限り、すべての財務データは1年ごとの期間に基づいていますが、四半期ごとに更新されます。これは、TTM（Trailing Twelve Month）またはLTM（Last Twelve Month）データとして知られています。詳細はこちら。分析モデルとスノーフレーク本レポートを生成するために使用した分析モデルの詳細は当社のGithubページでご覧いただけます。また、レポートの使用方法に関するガイドやYoutubeのチュートリアルも掲載しています。シンプリー・ウォールストリート分析モデルを設計・構築した世界トップクラスのチームについてご紹介します。業界およびセクターの指標私たちの業界とセクションの指標は、Simply Wall Stによって6時間ごとに計算されます。アナリスト筋PJX Resources Inc. 0 これらのアナリストのうち、弊社レポートのインプットとして使用した売上高または利益の予想を提出したのは、 。アナリストの投稿は一日中更新されます。0
お知らせ • Apr 29PJX Resources Inc., Annual General Meeting, Jun 24, 2026PJX Resources Inc., Annual General Meeting, Jun 24, 2026. Location: ontario, toronto Canada
お知らせ • Aug 01PJX Resources Inc. announced that it has received CAD 1.65246 million in fundingOn July 31, 2025, PJX Resources Inc. closed the transaction. The company announced that it has issued 4,714,286 flow-through unit at an issue price of CAD 0.14 per unit for gross proceeds of CAD 660,000.04 and 2,000,000 Units on a non-flow through basis at an issue price of CAD 0.12 per unit for gross proceeds of CAD 240,000; aggregate gross proceeds of CAD 900,000.04 in second and final tranche. Each Flow Through Unit consists of one common share and one common share purchase warrant. Each Unit consists of one common share and one common share purchase warrant. Each warrant acquired, whether with a Flow Through Unit or a Unit, will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following the date of issuance. Certain directors of company, participated in the private placement. Finders’ fees comprised of CAD 36,236 cash and 283,520 non-transferable warrants may be paid in respect of the first tranche of the Private Placement. The warrants will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following issuance. No Finders’ fees were paid in respect to the second tranche. All securities issuable in connection with the Private Placement will be subject to a statutory hold period in Canada which will run for four months from the date of issuance. The Private Placement is subject to compliance with applicable securities laws and to receipt of the final approval and acceptance of the TSX Venture Exchange. The company has offered 12,430,905 units of the Company for gross proceeds of CAD 1,652,460 in connection with the transaction.
お知らせ • Jul 10PJX Resources Inc. announced that it expects to receive CAD 1.65246 million in fundingPJX Resources Inc. announces a non brokered private placement to issue 12,430,905 units of the Company for gross proceeds of CAD 1,652,460 on July 9, 2025. The Company will issue units on a “flow through” basis and a non-flow through basis. The subscription prices for each of the foregoing are CAD 0.14 per Flow Through Unit and CAD 0.12 per Unit. The offering has been fully allocated and is expected to close on or about July 15, 2025. Each Flow Through Unit consists of one common share to be issued as a "flow-through share" within the meaning of the Income Tax Act (Canada) and one common share purchase warrant. Each Unit consists of one common share and one common share purchase warrant. Each warrant acquired, whether with a Flow Through Unit or a Unit, will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the Private Placement. Finders fees comprised of cash and non-transferable Warrants may be paid in respect of the Private Placement. The Warrants will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the Private Placement.
お知らせ • Apr 29PJX Resources Inc., Annual General Meeting, Jun 26, 2025PJX Resources Inc., Annual General Meeting, Jun 26, 2025. Location: ontario, toronto Canada
お知らせ • Jan 17PJX Resources Inc.'s Drilling Confirms the Geological Potential to Develop A Sedex Deposit on the Dewdney Trail PropertyPJX Resources Inc. announced that drilling has identified 3 Sedimentary Exhalative (Sedex) horizons with each horizon having the potential to host a Sedex type deposit at depth and on strike. The horizons are defined by increased sulphide mineralization in the form of stacked narrow massive to semi massive sulphide beds, bands, and/or disseminated sulphides. Iron rich minerals (pyrrhotite and pyrite) are dominant with lesser concentrations of copper (chalcopyrite), zinc (sphalerite) and/or lead (galena). Drilling explored for the source of Sullivan style and grade mineralized boulders (Photo A) found in talus material at the base of a mountain slope on PJX's 100% owned Dewdney Trail Property in the Sullivan Mining District near Cranbrook, British Columbia, Canada. Although the source of the boulders was not encountered during this initial phase of drilling, the geological environment discovered by drilling supports an environment similar to the Sullivan basin hosting the Sullivan deposit. Features include stacked bedding conformable sulphides, syn-sedimentary faults defined by large blocks of zinc mineralized sediments in a chaotic breccia (Photo B), and a cross cutting vent (Photo C) that can function as a conduit to transport metals for the formation of deposits. The sulphide flooded vent intersected while drilling is predominantly iron sulphide with locally significant copper sulphide and less zinc or lead sulphide (see photo C and grades below). This combination of sulphides suggests a hotter part of the mineralizing system. The source of the more zinc and lead rich Sullivan style and grade boulders would likely be in a cooler part of the system. This could be higher in the mineralizing system, which is higher on the mountain slope above where we have drilled. The Kootenay King quartzite horizon, which hosts the Kootenay King sedex zinc-lead-silver deposit 6.5 km on strike to the south, occurs higher on the mountain and has not yet been drilled. Cooler parts of the mineralizing system that may be favourable for forming a zinc-lead-silver deposit, may also occur laterally away from the vent as shown by the location of sphalerite and galena in replacement ore. The 3 Sedex horizons encountered in drilling may be favourable mineralizing periods to form a deposit on strike and laterally away from the vent area. Two Sedex horizons occur in the footwall beneath the Estella workings at the base of the mountain. The third Sedex horizon occurs about one third of the way up the mountain slope. Drilling commenced in early August last year after the exploration permit amendment was received from the government in mid-July, 2024. The exploration permit is good until July 2029. Further assessment of the results along with geophysics will be undertaken this winter to help define drill pad locations to test the various targets. Additional information will be provided when available. 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.
お知らせ • Dec 04PJX Resources' Dewdney Trail Property Sedex Deposit Potential UpdatePJX Resources Inc. announced that iron rich minerals (pyrrhotite and pyrite) with copper (chalcopyrite) and minor to trace zinc (sphalerite) and lead (galena) discovered in a venting geological environment by recent drilling appears consistent with mineralisation typically found within a vent beneath Sedex (Sedimentary Exhalative) type zinc-lead-silver mineralisation. This first phase of drilling commenced in August this year after PJX received a five year permit to explore and drill the large Dewdney Trail Property near Cranbrook, BC. Sedex deposits typically form where metal rich fluids rise from depth along pathways called vents that occur along faults. Deposit models suggest zinc and lead minerals (sphalerite and galena) are first to be deposited. Iron and copper rich mineralisation rise later along the vent and sometimes replace and/or remobilize zinc and lead and carry them higher in the venting system. The result is a zone of Sedex style zinc-lead-silver mineralisation above and/or laterally away from the location of iron and copper mineralisation. More drilling is required higher in the venting system which is higher on the mountain and laterally on strike to the south and north. 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 John Keating P.Geo. (qualified person for the purpose of National Instrument 43-101 Standards of Disclosure for Mineral Projects). Mr. Keating is the President, Chief Executive Officer and a Director of PJX.
お知らせ • Nov 13PJX Resources Inc. Announces Drilling Identifies Sedimentary Exhalative (Sedex) MineralizationPJX Resources Inc. announced 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. 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). 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. Mineralized Feeder Vent Breccia: Drilling supports the view that the mineralized breccia/fragmental first intersected and announced in a news release dated September 5, 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 contains visible amounts of copper sulphide (chalcopyrite) and zinc sulphide (sphalerite), as well as fragments of iron sulphide mineralization. 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. Zinc in Outcrop: Drilling and additional mapping confirms that zinc mineralization discovered in outcrop late 2023, occurs as large blocks of sedimentary rock, about 10 metres 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. 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. 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 their current location.
お知らせ • Sep 05PJX Resources Inc.'S Drilling Identifies Venting Type Environment That Supports Sullivan Style Sedex MineralisationPJX Resources Inc. announced that on-going drilling at the Dewdney Trail Property has encountered geology that supports the potential to discover a Sedimentary Exhalative (Sedex) type deposit. Of the 3 holes drilled to date the deepest into the mountain has intersected a 20m (estimated true width) fragmental with abundant to semi-massive sulphide mineralisation at 275m. The mineralisation appears to be predominantly iron sulphide (pyrrhotite and pyrite) with visible trace amounts of copper sulphide (chalcopyrite) and zinc sulphide (sphalerite). This style of mineralisation supports a venting environment, which is what occurs at the Sullivan Sedex deposit located approximately 20 km west of the Dewdney Trail Property in Southeastern British Columbia, Canada. Fragmental unit with iron sulphide (pyrRhotite and pyrite") in the matrix and what appear to be iron sulphide clasts in places. Zinc sulphide (sphalerites) and copper sulphide (chal copyrite) are locally visible in trace amounts (samples have been sent for analysis). The source of the Sullivan style and grade zinc, lead, and silver mineralisation discovered late last year at surface in boulders in talus material at the base of a mountain slope has not yet been identified by drilling. In addition, the zinc and lead mineralisation in outcrop discovered late last year appears to occur in large blocks and/or fragments of stratigraphy that may have collapsed into a sinking basin which can happen in Sedex environments. 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 mineralisation on PJX's Dewdney Trail Property that is over 150 km2 in size. The zinc, lead, silver, and other critical metal mineralisation 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. The mineralisation and geophysical anomaly have never been drilled. 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).
お知らせ • Apr 21PJX Resources Inc., Annual General Meeting, Jun 18, 2024PJX Resources Inc., Annual General Meeting, Jun 18, 2024.
お知らせ • Apr 16PJX Resources Inc. announced that it expects to receive CAD 3.6 million in fundingPJX Resources Inc. announces non brokered private placement 4,444,444 Flow Through Units at a issue price of CAD 0.36 per Flow Through Unit for gross proceeds CAD 1,599,999.84, 6,666,667 Strategic Units at a issue price of CAD 0.225 per Strategic Unit for gross proceeds CAD 1,500,000.075, 2,500,000 Non-Strategic Units at a issue price of CAD 0.20 per Non-Strategic Unit for gross proceeds of CAD 500,000 resulting aggregate gross proceeds of CAD 3,599,999.915 on April 15, 2024. Each Flow Through Unit consists of one common share and one-half of one common share purchase warrant. Each whole warrant acquired as part of a Flow Through Unit will entitle the holder to purchase one common share at an exercise price of CAD 0.45 for 24 months following completion of the Private Placement. Each Strategic Unit and Non-Strategic Unit consists of one common share and one-half of one common share purchase warrant. Each whole warrant acquired as part of a Strategic Unit will entitle the holder to purchase one common share at an exercise price of CAD 0.45 for 24 months following completion of the Private Placement. The transaction will include participation from Linda Brennan and James Clare, directors of company have subscribed for a total of 375,000 Non-Strategic Units. The securities issuable in connection with the Private Placement will be subject to a statutory hold period in Canada which will run for four months from the date of the respective closings of the Private Placement. The component of the Private Placement that has not already been completed, being the issuance of the Non-Strategic Units, is expected to close on April 15, 2024. The Private Placement is subject to compliance with applicable securities laws and to receipt of the final approval and acceptance of the TSX Venture Exchange.
お知らせ • Jan 15Pjx Resources Inc. Discovers 5.57% Zinc Mineralization in Outcrop Above Recently Discovered Sullivan Style Massive Sulphide BouldersPJX Resources Inc. announced recently received results of significant zinc and lead mineralization in outcrop that further supports the potential to discover a Sullivan type deposit on the Company's Dewdney Trail Property in the Sullivan Mining District in southeastern British Columbia, Canada. Two rock samples taken from outcrop, G23-699B and G23-699C below, returned values of 5.57% zinc, 0.94% (9450ppm) lead, 4.41g/t (4.41ppm) silver, and 4.72% zinc, 1.28% lead, 6.07g/t (6.07ppm) silver, respectively. The sediment hosted zinc and lead mineralization appears as bands or beds. The bedrock exposures of mineralization occur upslope and north of semi-massive to massive sulphide boulders containing Sullivan deposit style and grade mineralization announced in the news release dated October 12, 2023. Semi-massive to massive sulphide boulderers occur in talus at the base of the mountain slope. Outcrop with sediment hosted zinc-lead-silver mineralization occurs up-slope and to the north of the boulders' location. (photo looking northeast); The strongly magnetic semi-massive to massive sulphides boulders occur at the base of the mountain slopes and on the edge of a large (about 500m diameter) strong magnetic geophysical anomaly (pink to red coulours on the airborne magnetic map) that occurs upslope from the boulders; Zinc-lead-silver sulphide mineralization in outcrop is only very weakly magnetic. This supports the potential for a vertically or laterally zoned deposit with varying magnetic signatures. The outcrop mineralization appears to be associated with a less magnetic trend (orange to red coulours) in the airborne geophysics survey that occurs for possibly 1.6 km along strike.
お知らせ • Dec 11PJX Resources Inc. announced that it has received CAD 0.55125 million in fundingOn December 11, 2023, PJX Resources Inc., closed the transaction. The transaction was oversubscribed and the company issued 5,250,000 units at a price of CAD 0.105 for the gross proceeds of CAD 551,250. As a part of the transaction, the company paid CAD 40,042.08 as finder fee and 381,360 warrants.
お知らせ • Dec 05PJX Resources Inc. announced that it expects to receive CAD 0.5355 million in fundingPJX Resources Inc. announced a non-brokered private placement of up to 5,100,000 units through the issuance of flow-through units at a price of CAD 0.105 per unit for gross proceeds of up to CAD 535,500 on December 4, 2023. Each flow-through unit will consist of one common share to be issued as a flow-through share and one common share purchase warrant. Each warrant will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the offering. The offering, and any modifications to it, is subject to compliance with applicable securities laws and to receipt of the approval and acceptance of the TSX-V. The company reserves the right to increase the size of the offering or to modify the type, nature and price of the units for any reason. The securities issuable in connection with this offering will be subject to a hold period in Canada which will run for four months and one day from the date of the closing of the offering. The company may pay finders' fees, in accordance with the policies of the TSX-V.
お知らせ • Nov 23PJX Resources Inc. announced that it has received CAD 2.152149 million in fundingOn November 22, 2023, PJX Resources Inc. closed the transaction. The company now issued 13,816,422 Flow Through Units at a price of CAD 0.105 per Flow Through Unit for the gross proceeds of CAD 1,450,724.31 and 7,793,616 Non-flow Through Units at a price of CAD 0.09 per Unit for the gross proceeds of CAD 701,425.44; for the aggregate gross proceeds of CAD 2,152,149.75. Each Flow-through Unit consists of one common share and one common share purchase warrant. Each Unit consists of one common share and one common share purchase warrant. Each warrant, whether acquired as part of a Flow-through Unit or Unit, entitles the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the Offering. Subject to TSXV Exchange approval, Finders’ fees of CAD 30,337.20 cash and 291,709 Finders’ Warrants will be paid in relation to the completion of the Offering. The Finders Warrants will entitle the holder to purchase one common share at an exercise price of CAD 0.20 for 24 months following completion of the Offering. The securities issuable in connection with this Offering will be subject to a hold period in Canada which will run for four months from the date of the closing of the Offering. The Offering has received conditional approval from the TSXV Exchange. The transaction was oversubscribed. The transaction also included participation from certain insiders.
お知らせ • Nov 15PJX Resources Inc. Announces Soil Survey Supports Potential for Copper and Gold to Be Associated with Sullivan Style Zinc-Lead-Silver DiscoveryPJX Resources Inc. announced that highly anomalous gold and copper occur in soil material along with zinc, lead, and silver up slope from the discovery of Sullivan deposit style and grade semi-massive to massive sulphide boulders. The new sediment-hosted discovery of Sullivan style zinc-lead-silver mineralization in boulders occurs on the Company's Dewdney Trail Property in the Sullivan Minng District in southeastern British Columbia, Canada. Boulders of Sullivan style and grade mineralization were discovered in an area of about 50 metres (m) by 150 m at the base of a talus slope. The boulders are strongly magnetic and appear to have not moved far down the slope of the mountain from a possible bedrock source as some are large and angular. Soil samples taken from talus material up-slope from the boulders are highly anomalous in zinc, lead, silver, gold, and copper. The soils coincide with the strong airborne magnetic anomaly immediately up-slope from the boulderers. The highly anomalous zinc, lead, silver, gold, and copper content in soils are also coincident with a moderately strong magnetic anomaly for about 500 m along strike to the north of the 500 m long strong magnetic anomaly.
お知らせ • Oct 13PJX Resources Inc. Discovers Sullivan Style Massive Sulphide Mineralization with Grades Up to 9.33% Zinc, 2.48% Lead, and 14.62 G/T SilverPJX Resources Inc. announce the discovery of massive and semi-massive sulphide boulders of Sullivan deposit style zinc, lead, silver, cadmium, and indium mineralization. This significant new sediment-hosted discovery is on the Company's Dewdney Trail Property in the Sullivan Mining District in southeastern British Columbia, Canada. PJX's prospecting team discovered boulders with sulphide mineralization in an area about 50 metres (m) by 150 m at the base of a talus slope. Some sulphide boulders display layering and breccia textures with grades of zinc-lead-silver mineralization similar to ore at the Sullivan deposit. The sulphide boulders with zinc (sphalerite mineral), lead (galena), and iron (pyrite and pyrrhotite) are magnetic. The boulders occur at the base of the mountain slope and on the edge of a large magnetic anomaly identified by Expert Geophysics from the 875 line-kilometre airborne geophysical survey flown for PJX in 2021. Sample SMT-23-1 (6.71% zinc, 2.23% lead, 16.05 g/t silver, 1,258.9 ppm or 0.12% copper) Sphalerite (zinc sulphide), galena (lead sulphide), and iron sulphides (pyrite, pyrrhotite) occur in fragments that are locally banded or bedded in apearance as seen above. The mineralization also occurs in the groundmass of the rock. Sample SMT-23-8 (3.55% zinc, 0.98% lead, 7.5 g/t silver, 442.1 ppm or 0.04% copper) Although this sample is lower in grade it tells an important story. The individual massive sphalerite fragments are a possible indicator of higher grade zinc rich massive sulphides possibly buried under the talus slope. Sample SMT-23-7 (9.33% zinc, 2.48% lead, 14.62 g/t silver, 495 ppm or 0.04% copper) Alternating dark and light coloured bands with sulphides (zinc, lead, iron) appear to be sulphide-rich beds that have been broken apart possibly by slumping during deposition on the ocean floor, or the beds may have broken apart during later folding. Airborne Magnetic Map: Massive sulphide boulders occur downslope from a magnetic anomaly (red to pink area). The boulders are magnetic. The initial target area with deposit potential is defined by an elevated magnetic signature that is over 1.5 km along strike. Stronger magnetic anomalies (pink colour) may represent more iron rich (pyrrhotite mineral) zones similar to those that occur at the Sullivan deposit. Less strong magnetic anomalies (red to orange colour) may represent areas with more zinc or lead sulphide mineralization that would be more weakly magnetic. The 160 million tonne Sullivan deposit produced ore containing some 17 million tonnes of zinc and lead metal and more than 285 million ounces of silver during 90 years of operation before closing in 2001.
お知らせ • Jun 30PJX Resources Inc. Commences 2023 Exploration with Discovery of New Iron-Oxide Zone That Expands Copper-Gold-Silver Potential on Dewdney Trail PropertyPJX Resources Inc. announced that field work on the Dewdney Trail Property has begun in preparation to advance and drill test copper-gold-silver mineralization associated with alkalic porphyritic intrusions discovered last year. Recent prospecting has discovered an additional iron-oxide breccia zone with localized copper mineralization. This new zone is approximately 1500 m southeast of a series of stacked bedding parallel quartz veins that contain up to 63 g/t gold. The new zone expands the potential to discover multiple gold-copper-silver and possible molybdenum deposits related to porphyry intrusions. The zone is approximately 3 km southwest of the Estella Basin where a cluster of intrusions and hydrothermal breccias occur with anomalous gold, copper, silver, molybdenum, arsenic and other elements in soils and rock samples. The zone may also be related to a large (5 km diameter) circular shaped feature defined by an 895 line-km airborne magnetic and Mobile MT (EM) survey flown by Expert Geophysics for PJX over an 80 km2 area. The Estella Basin and new breccia zone occur proximal to the rim of the circular feature that may reflect the margin of a collapsed pluton at depth. Porphyry copper-gold deposits are known to occur along the margin of plutons.