Duyuru • Jun 18
Gt Resources Initiates Field Work At Cd Gold-Copper Porphyry Project Yukon GT Resources Inc. has begun the 2026 field program on the CD Project in Yukon's Dawson Range Gold Belt, located near Carmacks. CD hosts a gold - copper porphyry target, with valid drill permits until 2033 and co-incident soil and geophysical anomalies. The CD Project exhibits significant geological parallels to Western Copper and Gold's Casino deposit, situated 90 kilometers to the northwest. The current work program includes a focused airborne MobileMT survey. This natural-field EM technology was specifically chosen for its ability to map subsurface resistivity and conductivity to help identify disseminated sulphide mineralization, porphyry alteration, and structure that VTEM surveys may not detect. Integrating MobileMT data with the existing ground-based IP and magnetics, will allow GT to develop a comprehensive 3D model to refine the highest-priority drill targets. The 2026 field season is dedicated to high-resolution data acquisition to refine targets before GT's maiden drilling program at CD, which is located in the Dawson Range Gold Belt, an area of heightened exploration activity in recent years. An airborne MobileMT survey will be flown over the Maloney porphyry target mapping subsurface resistivity and conductivity features, to help identify disseminated sulphide mineralization, porphyry-style alteration, and structure. Additionally, field reconnaissance mapping, prospecting, and soil sampling will be undertaken over the Maloney porphyry and Schist vein targets to gain additional understanding of the lithology, alteration, and structure of these areas. Following the survey and field program, GT will integrate the new data with existing ground-based IP and magnetics to develop a comprehensive 3D model to target the highest priority drill targets. New MobileMT data integrated with existing datasets will allow GT to improve the definition of Maloney porphyry targets, to reduce the reliance on broadly spaced or conceptual drill testing, and to support more efficient allocation of exploration capital. GT currently intends to conduct a 2,500 to 3,000 meter diamond drill program. This campaign will be designed to systematically test the gold-rich copper porphyry potential and the high-grade gold-silver vein targets at CD. CD hosts a 1,200 m x 400 m gold-copper-molybdenum anomaly. Historical drilling (only 6 holes) demonstrated the presence of a mineralized system but notably failed to test the recently defined primary IP and gold in-soil target further to the northeast. Drilling (1970s) 0.15% Cu over 15.2 m (hole 76-2) 0.09 g/t Au, 0.10% Cu over 21.3 m (hole 76-4) Trenching (1970s) 0.43 g/t Au, 0.15% Cu, 196 ppm Mo over 5 m Grab Samples (2011-2018) 0.81 g/t Au, below a 632 ppm Au-in-soil sample Soils (2011-2018) Peak soil values of 1,270 ppm Au, 1,485 ppm Cu, and 42 ppm Mo. Schist target, an untested vein hosted gold-silver system Undrilled Large gold-arsenic in-soil anomaly (2,000m x 500m). 1.67 g/t Au over 6.5 meters in historical (2011) trench chip samples. 6.29 g/t Au and 7.6 g/t Ag; 2.78 g/t Au and 25.7 g/t Ag in historical (2013-2015) grab samples. Duyuru • May 06
GT Resources Inc., Annual General Meeting, Jul 17, 2026 GT Resources Inc., Annual General Meeting, Jul 17, 2026. Duyuru • Jan 14
GT Resources Inc. Provides an Update on the Lantinen Koillismaa Copper - Nickel - Palladium - Platinum Project, Located in Northcentral Finland GT Resources Inc. provided an update on the Lantinen Koillismaa ("LK") Copper - Nickel - Palladium - Platinum Project, located in northcentral Finland. Highlights. The Company has commenced an extensive assay infill and re-assay program for the Kaukau Zone of the existing LK deposit. Over 5,000 samples from across the Kaukua Zone are expected to be analysed to better define known mineralization. This work is being conducted in preparation for a potential Resource Update and Preliminary Economic Assessment ("PEA"). Background. LK is the Company's most advanced project having an existing NI43-101 Palladium - Platinum - Copper dominated open pit Resource Estimate as follows: Indicated Resources: 1.1 Million ounces Total Precious Metals (Palladium + Platinum + Gold) ("TMP"), 111 Million pounds of Copper., 92 Million pounds of Nickel, contained in 38.2 million tonnes. Inferred Resources: 1.1 million ounces TMP, 173 Million Pounds Copper, 152 Million Pounds Nickel, contained in 49.7 million tonnes. The LK project remains open for expansion laterally and at depth, notably along the 17-km long Haukiaho Trend. The historic drill programs did not sample 100% of the drill core, and potential remains to identify additional in pit resources. A total of ~500 infill samples are being collected and will be submitted for analysis. The primary focus of the program is to produce a homogenous assay database at Kaukua with all samples analysed using the same analytical techniques. Historic drill programs used the "Aqua Regia" digestion method. Aqua Regia is a partial digestion method which covers the total nickel grade as it only digests sulphide hosted nickel. The majority of the drill hole samples at Kaukua were completed by the Company and were analysed with the "Four Acid" digestion method which provides a more complete digestion of the sample and representation of total nickel grade. All the Metallurgical testing by the Company and the Net Smelter Return ("NSR") calculation used in the 2022 Mineral Resource Estimate assumed all samples were analysed using the Four Acid digestion method. This resulted in a two-fold effect: it under reported total nickel grades and secondly applied an unnecessarily harsh nickel recovery to historic drill holes. Re-assaying historic samples analysed by Aqua Regia was one of the recommendations from the 2022 technical report. A total of 4,600 drill core pulps are being collected and will be submit for analysis. Once these results have been compiled and analyzed on the Kaukua Zone the re-assay program may be extended to the Haukiaho Zone which has an even larger proportion of historic drill holes. Resource Expansion Potential. The 17-kilometer long Haukiaho trend represents the nearest term expansion potential. The Haukiaho Deposit currently occupies only 2 kilometers of this trend. Historic drilling along this trend, primarily by Outokumpu in the 1960's was only sampled for copper and nickel, partial resampling of historic drill core by the Company in 2022 returned significant platinum and palladium grades. Duyuru • Jun 14
GT Resources Inc. Provide an Update with Regard to Plans for the North Rock Project (Canada) and the Läntinen Koillismaa ("Lk") Project (Finland) Both Copper-Palladium-Platinum Projects GT Resources Inc. provide an update with regard to plans for the North Rock Project (Canada) and The Läntinen Koillismaa ("LK") Project (Finland) both Copper-Palladium-Platinum projects. North Rock Copper - Palladium - Platinum ("PGE") Project, Ontario, Canada The 2024 exploration program identified off hole geophysical conductors adjacent to historic high-grade footwall vein intercepts which returned up to 14.6 g/t Palladium, 0.5 g/t Platinum, 0.3 g/t Gold and 2.3% Copper, and 0.6% Nickel over 0.6 meters in NR07-062. Upcoming exploration programs include additional Bore Hole Electro Magnetic ("BHEM") surveys of more historic holes, followed by detailed drill plans to target high-grade massive sulphide footwall style copper-palladium rich veins. LK is the Company's most advanced project with a substantial Palladium-Platinum-Copper rich open pit resource. Indicated Resources: 1.1 Million ounces Total Precious Metals (Palladium + Platinum + Gold) ("TMP") (0.89 g/t), 111 Million pounds of Copper (0.13%), 92 Million pounds of Nickel (0.11%), and contained in 38.2 million tonnes. Inferred Resources: 1.1 Million ounces TMP (0.68 g/t), 173 Million Pounds Copper (0.16%), 152 Million Pounds Nickel (0.14%), and contained in 49.7 million tonnes. The North Rock project is located in Northwest Ontario, boasts excellent infrastructure (bisected by a paved provincial highway and a railroad) and is crossed by power lines. The mineralization consists of copper-rich magmatic sulphide, along a 13-kilometer basal contact of mafic and ultramafic volcanic rocks. The mineralization occurs in two main styles; a more copper-rich "gabbro hosted" disseminated to locally net-textured sulphide within the basal heterolithic, varitextured gabbro, and as massive copper-palladium-rich sulphide "footwall vein" style within the footwall volcanic rocks. Two very shallow zones have been discovered to date, the most significant of which is the Beaver Pond Zone, which hosts a Historic Resource Estimate1 of 1 million tons grading 1.2%Copper. The Beaver Pond Zone was discovered by Noranda in 1958 and subsequently explored from underground via a 90-meter deep shaft and one drift on the 70m level. The LK Project, located in central Finland represents the Company's most advanced project with a significant NI 43-101 compliant open pit resource and is well position to supply the European Union with critical minerals, notably copper, palladium and platinum, of which Europe is heavy dependant on imports with only one producing mine (Boliden's Kevitsa mine in Finland). Boliden also operates both copper and nickel smelters in Finland, thereby providing LK a potential competitive advantage. Duyuru • Apr 29
GT Resources Inc., Annual General Meeting, Jul 11, 2025 GT Resources Inc., Annual General Meeting, Jul 11, 2025. Duyuru • Jan 28
GT Resources Inc. Samples 8.2% Copper and Identifies BHEM Conductors at the North Rock Copper-Nickel-PGE Project, Ontario, Canada GT Resources Inc. announced that several Bore Hole ElectroMagnetic ("BHEM") conductors have been identified on the North Rock copper - nickel - platinum group element project located in Northwestern Ontario, Canada. The North Rock project encompasses a strikingly underexplored 13-kilometre long mineralized basal gabbroic contact along the Grassy Portage Gabbroic Complex. The limited, approximately 12,000 meters, of historic drill testing demonstrates Cu-Ni-PGE (copper-nickel-palladium and platinum) mineralization throughout the tested zones of the favorable basal contact. A historic resource estimate of 1 million tons grading 1.2% copper was outlined by Noranda in 1958 on the Beaver Pond Zone. Having completed historic data compilation and analysis, the Company views the North Rock project as a copper exploration project with meaningful polymetallic enhancement opportunities, in a highly favorable environment with proven mineralization. The Company intends to target 'footwall style' semi- massive to massive sulphide along the basal contact. Historically, BHEM surveys were not undertaken. The fourth quarter 2024 BHEM survey has proven the worth of this geophysical technique by identifying several conductors along the deepest holed drilled to date. The Company believes that the use of modern electromagnetic geophysical techniques including BHEM to expand know zones and to target new zones is a priority for effective drill testing of higher-grade mineralization. Fourth quarter 2024 exploration highlights include: 8.2% Copper in grab sample NP-NR-24-001 from the Historic Beaver Pond Zone. First use of BHEM geophysics has identified several in and off-hole conductors, an important first step in targeting blind, net-textured to massive sulphides below historic shallow drilling. The North Rock Project: The North Rock project is located in Northwest Ontario, and covers over 7,000 hectares. The project boasts excellent infrastructure and is crossed by a paved provincial highway, a railroad, and hydro lines. North Rock is hosted by the Archean aged, 20 kilometer long Grassy Portage Gabbro Complex. The mineralization is copper-rich magmatic sulphide, and is focused along the basal contact of the Complex with mafic and ultramafic volcanic rocks. The mineralization occurs in two main styles; "gabbro hosted" disseminated to locally net-textured sulphide within the basal heterolithic, varitextured gabbro, and as massive copper-PGE-rich sulphide "footwall vein" style within the footwall volcanic rocks. Two very shallow zones have been discovered to date, the most significant of which is the Beaver Pond Zone, which hosts a Historic Resource Estimate of 1 million tons grading 1.2% Cu. The Beaver Pond Zone was discovered by Noranda in 1958 and subsequently explored from underground via a 90-meter deep shaft and one drift on the 70m level. Reconnaissance Prospecting: The grab samples presented in this news release were collected during fourth quarter 2024 from a 10,000-ton surface stockpile of material recovered from underground development of the Beaver Pond Zone in the 1970's. The samples are roughly representative of high, mid and low-grade material present within the pile. The mineralization is notably copper-rich, with chalcopyrite being by far the most abundant sulphide. Of note was the presence of molybdenite (with assay up to 0.10% Mo), normally rare in a magmatic Cu-Ni-PGE systems, molybdenum was likely assimilated during the emplacement of the Gabbro complex, as evidenced by numerous partially assimilated wall rock clasts within the heterolithic, varitextured gabbro which hosts the mineralization. BHEM Survey: The Company undertook a BHEM survey in fourth quarter 2024 on select historic holes located within the Beaver Pond zone. This was the first BHEM survey conducted on the property and was a "test case" to see if the North Rock mineralization was amenable to BHEM techniques. A prime focus of the survey was hole NR07-062, which at 780m is by far the deepest hole drilled on the project. Of significant note, this hole intersected footwall style Cu-PGE rich mineralization at ~450m depth but was drilled down dip of the Zone, and never exited the footwall volcanics into the main gabbro hosted mineralization. The fact that high-grade footwall mineralization was intersected, suggests that untested disseminated gabbro hosted style mineralization occurs proximal to the hole. This hole returned several conductors which have been modelled as Maxwell EM plates with some corresponding to known footwall style mineralization that was intersected within the hole "in hole" plus "off hole" conductors potentially representing untested footwall style mineralization. 
