Aankondiging • 1h
Super Copper Corp Defines 3.5 Km Magnetic Corridor At Cordillera Cobre Project Super Copper Corp. reported results from its 3D magnetic vector inversion of ground magnetic data at the Cordillera Cobre Project, near Copiapó, Chile. The new MVI is the first geophysical evidence linking El Alto and Calcite Hill within a single coherent magnetic corridor. The MVI defines a coherent magnetic corridor extending approximately 3.5 kilometres across the central target area and shows positive spatial correlation with the previously reported chargeability anomaly from induced polarization surveying. Together with historical drill core assay results, these datasets define coherent targets at depth that have not been tested by drilling. MVI modelling has identified a coherent magnetic corridor along a NW–SE structural trend across the El Alto and Calcite Hill target areas, the first geophysical evidence linking these two areas within a single coherent magnetic corridor. The strongest magnetic zones and the strongest chargeability zones overlap at depth, two independent methods detecting the same target. This overlap reduces the likelihood that either anomaly is caused by something other than mineralization. Historical drill holes returned up to 14 m at 0.508% Cu, including 2 m at 1.605% Cu (DVP-01), from the outer margin of the combined geophysical anomalies. The highest-intensity magnetic and chargeability core at depth has not been tested by drilling to date. The Company is finalizing drill targeting using the integrated 3D geophysical model and will announce its plans for the phase 1 diamond drill program in a subsequent news release. While IP surveys target charge and conductive anomalies attributed to the occurrence of metallic sulphide mineralization, magnetic data identifies zones of anomalous magnetic susceptibility naturally occurring in association with abundant ferromagnetic minerals. The combination of these two geophysical responses is typical of IOCG systems within the Atacama region. Magnetic vector inversion models the orientation and strength of subsurface magnetization. Through an MVI model ground magnetic data can be visualized in three dimensions allowing for identification of bodies with magnetic orientations that do not align with the earth's magnetic field. These areas of high magnetization and contrasting orientations to the Earth's field direction can be interpreted as zones of potential ferromagnetic mineralization that exhibit a remnant magnetic response. At El Alto, anomalies interpreted as remnant magnetic responses were identified for the first time allowing to determine zones of interest to target iron oxide bodies expected to be associated with copper. At El Alto, the MVI model shows large zones of strong magnetism that extend from near surface to depths well below historical drilling (~200 m). The strongest magnetic responses form coherent bodies trending northwest-southeast and dipping sub-vertically. These bodies are spatially associated with previously determined chargeability anomalies identified by the Company's IP survey. In the accompanying 3D MVI model, pink and magenta blocks represent the strongest magnetic responses with magnetic orientations that do not align with the earth's field direction. These areas could be attributed to iron oxide occurrence which is closely related to copper mineralization in typical IOCG systems. Blue blocks are background signatures representing rock with no significant magnetic response. The key finding is that the strongest magnetic responses and the strongest chargeability responses have positive correlations at depth. These are two independent geophysical methods measuring two different physical properties, both highlighting the same target area. In IOCG systems, magnetite and copper sulphides are deposited by the same mineralizing fluids, detecting both signatures in the same zone strengthens the possibility that El Alto hosts a copper-bearing system at depth. This association is characteristic of productive IOCG deposits within Chile's Atacama Fault System. The Company has integrated the 3D MVI model with the previously reported 2D IP chargeability inversions and historical drill core assay results to develop a comprehensive exploration model at El Alto. Anomalous zones in the 3D MVI model are closely related spatially with areas of high chargeability identified from previously reported IP surveys. Magnetic data can identify areas of potential iron oxide bearing rocks; while IP chargeability is helpful in targeting sulphides and other metallic minerals that occur in the subsurface. The combination of these two responses is characteristic of iron oxide copper-gold systems in the Atacama region. Both datasets define targets that plunge to the southeast and extend for over one kilometre along a NW–SE structural corridor. The MVI model provides the three-dimensional geometry that the 2D IP sections did not fully resolve. Historical drill core assay results show that copper grades increase with proximity to the combined MVI and IP anomalies. DVP-01 returned 14 m at 0.508% Cu, including 2 m at 1.605% Cu, with the highest grades occurring at the nearest approach to the geophysical anomaly. This relationship provides direct geochemical validation that the geophysical targets are associated with copper mineralization. All historical drill holes terminated at shallow depths (~200 m) and intersected only the upper and peripheral portions of the recently defined geophysical anomalies. The MVI and IP anomalies at depth have never been tested by drilling. The Company is finalizing drill targeting at El Alto using the integrated 3D geophysical model, under the supervision of the Qualified Person, Michael Dufresne, M.Sc., P.Geol., P.Geo., and its geological consultants at APEX Geoscience Ltd. Details of the phase 1 diamond drill program, including hole count, meterage, and target prioritization, will be disclosed in a subsequent news release. Geophysical data collection and processing were conducted by Argali Geofísica (IP and ground magnetics survey) and APEX Geoscience Ltd. (MVI modelling). The IP survey utilized a pole-dipole array configuration with d=50 m, N=1 to 20, and chargeability integration window of 400–1840 ms. The MVI model was generated using Seequent VOXI Earth Modelling. All geophysical data and interpretations have been reviewed by the Qualified Person. Super Copper follows industry standard procedures for the work carried out on the Cordillera Cobre Project, with a quality assurance/quality control (QA/QC) program. For the core samples, blank, duplicates and standard samples were inserted into the sample sequence sent to the laboratory for analysis (~10% of samples). Samples were cut from available core (Half or quarter core) from select intervals containing visible copper mineralization and packed in polyethylene bags with unique sample numbers that were also kept in sample data log. Aankondiging • Apr 11
Super Copper Corp Identifies Kilometre-Scale Anomaly Corridor with Multiple Large Chargeability Cores Open At Depth Super Copper Corp. reported the induced polarization survey at the Cordillera Cobre Project near Copiapo, Chile has defined a kilometre-scale potential sulphide corridor characterized by strong, coherent chargeability responses. The responses extend over a minimum 800 metres of strike and approximately 400 metres in vertical extent. Integration of the new geophysical data with newly sampled historical diamond drill core confirms that copper mineralization occurs along the margins of the system, while the highest-intensity chargeability core at depth remains entirely untested. Kilometre-scale copper bearing trend defined at El Alto and coincident with higher chargeability expression at depth in five consecutive IP lines (Lines 2800–3600) spaced 200 metres apart, demonstrating strong lateral continuity over a minimum 800 metres of strike, open along strike and at depth. Consistent high chargeability anomalies at El Alto identified at depth, measuring up to approximately 400 metres in width and 300–400 metres in vertical extent, with increasing chargeability towards the southeast and at depth. Chargeability responses ranging from greater than 0.5 to greater than 5.0 mV/V, consistent with copper-bearing systems in Chile's Atacama belt. Historical diamond drilling confirms copper mineralization at the margins of the IP corridor, validating the geophysical interpretation. Highlight intercepts from newly sampled core include: 14 metres at 0.508% Cu, including 2 metres at 1.605% Cu (DVP-01); 10 metres at 0.324% Cu, including 2 metres at 1.36% Cu (DVP-02); 8 metres at 0.216% Cu, including 1 metre at 1.365% Cu (DVP-03); 4 metres at 0.493% Cu (DVP-06). Historical holes intersected only upper and peripheral portions of the chargeability anomalies, while the highest-intensity chargeability zones at depth remain entirely untested. Integrated IP and ground magnetic data define a structural corridor extending for over one kilometre, providing a clear vector for the Company's planned Second Quarter 2026 diamond drill program targeting the interpreted core of the sulphide system. The IP survey was completed by Argali Geofisica on behalf of Super Copper. This survey included two grids, one at Calcite Hill and one at El Alto, both consisting of five 1 km IP lines at 200 metres spacing. At El Alto a large, coherent chargeability corridor extending over a minimum 800 metres of strike across five consecutive survey lines (Lines 2800–3600) was defined. The corridor comprises multiple high-intensity chargeability centres that appear to coalesce at depth into a broader zone extending towards the southeast. The principal chargeability zones measure up to approximately 200–400 metres in width and extend to depths of at least 300–400 metres below surface, with the strongest responses increasing towards the southeast. Chargeability values range from greater than 0.5 to greater than 5.0 mV/V, typical of IOCG-style and/or porphyry copper systems within the Atacama belt. The corridor remains open along strike and at depth. Ground magnetic data indicates the structural controls extend for over one kilometre, suggesting potential for additional strike continuity beyond the current IP coverage and at depth. Chargeability responses at depth are interpreted to reflect primary sulphide mineralization within bedrock, distinct from near-surface oxide or supergene enrichment horizons. Historical drilling confirms copper mineralization along the margins of the corridor, providing direct validation of the geophysical targets. In 2007, a previous operator completed eight diamond drill holes (DVP-01 through DVP-08) at El Alto, totalling approximately 1,555 metres. The program was designed to test near-surface targets and was not guided by IP data, which had not yet been acquired. All eight holes terminated at relatively shallow depths, reaching a maximum of approximately 200 metres downhole. At El Alto, the Company re-logged select intervals of previously unsampled historical diamond drill core from six drill holes (DVP-02, DVP-03, DVP-05, DVP-06 and DVP-07) originally drilled in 2007 and sampled them for assay. Additionally, the Company resampled drill holes DVP-01 and DVP-08 for drill hole verification and up-to-date analytical procedures. New Risk • Mar 23
New major risk - Share price stability The company's share price has been highly volatile over the past 3 months. It is more volatile than 90% of Canadian stocks, typically moving 19% a week. This is considered a major risk. Share price volatility increases the risk of potential losses in the short-term as the stock tends to have larger drops in price more frequently than other stocks. It may also indicate the stock is highly sensitive to market conditions or economic conditions rather than being sensitive to its own business performance, which may also be inconsistent. Currently, the following risks have been identified for the company: Major Risks No financial data reported. Share price has been highly volatile over the past 3 months (19% average weekly change). Shareholders have been substantially diluted in the past year (66% increase in shares outstanding). Minor Risk Market cap is less than US$100m (CA$28.5m market cap, or US$20.7m). Aankondiging • Mar 20
Super Copper Corp Discovers New High-Grade Copper Zones At Cordillera Cobre Project SUPER COPPER CORP. reported Phase 1 exploration results from its flagship Cordillera Cobre Project, located in Chile's Atacama region. Cordillera Cobre is one of two copper exploration assets held by the Company in the Atacama belt, alongside the Castilla Project, which Super Copper acquired in 2025 and is advancing through early-stage exploration. Phase 1 represents its most significant field program to date: two new high-grade copper zones discovered in a completely undrilled area, with excellent surface grades confirmed across three distinct target areas, and structural controls on mineralization mapped across 800+ hectares via ground magnetometry. The IP survey is now complete, with chargeability data being processed for near term release. Highlights Two new high-grade copper zones discovered in the northern project area, returning up to 7.13% Cu and 4.78% Cu from rock grab samples of outcrop, in an area with no prior drill testing 24 of 102 rock grab samples exceeded 1% copper, with 10 samples returning greater than 3% Cu, demonstrating widespread high-grade mineralization across multiple target areas Excellent surface grades confirmed at three distinct target areas: Northern Showing: 7.13% Cu with 98.7 g/t Ag (new discovery) Anima Mine Trend: 6.92% Cu over 1 m in chip samples Calcite Hill: 3.40% Cu over 1 m in chip samples El Alto Historical Trench T-267A returned 17 m grading 0.34% Cu, including 2 m at 1.48% Cu in chip samples, demonstrating continuity and width potential, and potentially indicative of a structurally controlled system at depth An IP survey is now complete across El Alto and Calcite Hill target areas; chargeability results to be released imminently Super Copper's Phase 1 results at Cordillera Cobre include samples grading up to 7.13% Cu across multiple target areas, well above typical mine grades in the region. The combination of high-grade copper exposed at surface, multiple mineralized zones, and structural controls now defined by geophysics de-risks the path to targets and provides a technical foundation for high-confidence drill target selection. These combined results indicate the potential for a larger, structurally controlled copper system rather than isolated high-grade occurrences. New High-Grade Results in the North: Phase 1 prospecting identified two previously unknown high-grade copper zones in the northern portion of Cordillera Cobre, an area not covered by historical drilling. The newly designated Northern Showing returned 7.13% Cu with 98.7 g/t Ag and 4.78% Cu in rock grab samples from outcrop. Mineralization is hosted in breccias and veins within diorite (northernmost cluster) and volcaniclastic rocks, and appears structurally controlled, with the two zones located approximately 1.5 kilometres apart. The 1.5-kilometre separation between the two zones, combined with consistent structural orientation, suggests these are not isolated occurrences but surface expressions of a broader mineralized system, one that has received no drill testing to date. The Northern Showing is now a priority target for follow-up work alongside El Alto and Calcite Hill. Ground magnetometry across 800+ hectares reveals a coherent set of northwest-trending structural corridors controlling mineralization at both Calcite Hill and El Alto. Magnetic low anomalies, reflecting magnetite destruction by hydrothermal fluids, a hallmark of Atacama copper systems, are spatially coincident with the project's highest-grade surface samples. The magnetometry data has now been integrated with an Induced Polarization (IP) survey across both the El Alto and Calcite Hill target areas. IP chargeability results will be released in a subsequent announcement. While magnetics define where the hydrothermal system was active, IP chargeability pinpoints potential disseminated sulphide concentrations at depth, which will help convert structural targets into high-confidence drillable targets. The full dataset will advance the Company toward its Phase 1 drill program, targeted for Second Quarter 2026. The Phase 1 campaign marks the Company's most comprehensive field program to date at Cordillera Cobre, designed to validate historical drill results and generate new data across multiple high-priority copper zones to support drill target definition.All rock samples were submitted to ALS Laboratories in Chile for geochemical analysis. The geophysical survey was carried out by Argali Geophysics. These results form the foundation for Super Copper's next phase of target definition, with Phase 1 drilling targeted for Second Quarter 2026. New Risk • Mar 09
New major risk - Shareholder dilution The company's shareholders have been substantially diluted in the past year. Increase in shares outstanding: 71% This is considered a major risk. Shareholder dilution occurs when there is an increase in the number of shares on issue that is not proportionally distributed between all shareholders. Often due to the company raising equity capital or some options being converted into stock. All else being equal, if there are more shares outstanding then each existing share will be entitled to a lower proportion of the company's total earnings, thus reducing earnings per share (EPS). While dilution might not always result in lower EPS (like if the company is using the capital to fund an EPS accretive acquisition) in a lot cases it does, along with lower dividends per share and less voting power at shareholder meetings. Currently, the following risks have been identified for the company: Major Risks No financial data reported. Shareholders have been substantially diluted in the past year (71% increase in shares outstanding). Minor Risks Share price has been volatile over the past 3 months (18% average weekly change). Market cap is less than US$100m (CA$33.8m market cap, or US$24.9m). Aankondiging • Mar 07
Super Copper Corp. announced that it has received CAD 9.750001 million in funding On March 6, 2026, Super Copper Corp closed the transaction. The company issued 13,000,000 units at a price of CAD 0.75 per unit for aggregate gross proceeds of CAD 9,750,000. Each Unit is comprised of one common share in the capital of the Company and one Share purchase warrant. 6,566,666 of the Units issued were comprised of Series A Warrants and 6,433,334 of the Units issued were comprised of Series B Warrants. Each Series A Warrant entitles the holder to acquire one additional Share at a price of CAD 1.15 per Share for a period of 36 months following the closing of the Offering. Each Series B Warrant entitles the holder to acquire one additional Share at a price of CAD 1.15 per Share from the date that is 61 days from the closing of the Offering until the date that is 36 months from the closing of the Offering. In connection with the Offering, the Agents received a cash commission equal to 6.0% of the gross proceeds of the Offering and the Company issued to the Agents non-transferable warrants ("Broker Warrants") representing 6.0% of the aggregate number of Units sold pursuant to the Offering. Each Broker Warrant entitles the holder to purchase one Share of the Company at a price of CAD 1.15 per Share for a period of 36 months from the closing of the Offering. Securities issued to the Agents in connection with the Offering were subject to a hold period under applicable Canadian securities laws expiring four months and one day from the closing date of the Offering. 
