Slide 1: Para Technical Project
DRILL-READY EXPLORATION COMPANY POSITIONED FOR DRILL CATALYSTS IN 2026 PARA TECHNICAL PROJECT May 2026 TSXV: LXE Porphyry Cu-Mo System Year-Round Access Q3 2026 drilling
Slide 2: Highlights
Highlights Multiple Centers - Para presents evidence of porphyry style mineralization in multiple centers. Positive Geochemistry - Surface geochemical anomalies include stream sediment, talus and rocks. Positive Geophysics - Geophysical surveys including magnetic, induced polarization, and rad
Slide 3: Exploration Belt
Exploration Belt Cretaceous porphyry belt of Peru was historically recognized between Ica and Arequipa but now extended north of Lima following the discovery of ILLARI deposit (Newmont) and subsequent exploration successes. ELIDA Current exploration activities for copper are in progress looking
Slide 4: Regional Copper & Zinc Endowment
Regional Copper & Zinc Endowment ILLARI Maria Teresa (production to date 9.5 Mt, 2017). 7.44% Zn, 0.49% Cu, 1.39% Pb, 4.02 oz Ag/t. To SUMACWAYRA July 2018. (resource 8.7 Mt, 2018) 6.2% Zn, 1.1% Cu, 0.68 Pb, 1.93 oz Ag/t. LACSHA LEZARD La Palma (14.5 Mt measured and indicated) 5% Zn, 0.7% Pb and
Slide 5: Regional Geology
Regional Geology ILLARI Casma Group (Chilca Fm., Pamplona Fm.) and Rimac Group host the main VMS style mineralization. SUMACWAYRA The Santa Rosa and Tiabaya Super Units form part LACSHA of the Coastal Batholith and serve as the primary LEZARD hosts for younger porphyritic intrusions associated w
Slide 6: Structural Framework
Structural Framework ILLARI Deposits are strongly controlled by the intersection of major structural trends: SUMACWAYRA East-west low magnetic trends recognized by airborne magnetic surveys and. LACSHA major mapped fault systems trending northwest- LEZARD southeast Possible relationship to d
Slide 7: Stratigraphic Column
Stratigraphic Column Quaternary Quaternary deposit Huarochiri Fm. (Andesitic tuff) Neogene Cenozoic Rimac Group Paleogene (Andesitic tuff) v v v v v v v v v v v v PARA v v v v v v v v v v v v v v v v v v Post. Batholith v v v v v v Quilmana Fm. Upper v v v v v v (Andesitic flows) Intrusive Mesozoic
Slide 8: District Geology
District Geology TILLO The Coastal batholith from the Upper Cretaceous, PARA with its Tiabaya Super Unit are the principal host for porphyry copper mineralization. TAURIPAMPA Para Porphyry project VMS Mines Porphyry early or advance stage projects VMS early or advance stage projects LOS PINOS Mioc
Slide 9: Schematic Section
Schematic Section A B 3000 msal PARA TILLO vv v 1000 msal ` v v v 0 msal v v v 0 3km Para Porphyry Miocene Volcanic Package Costal Batholith: (S.U. Tiabaya, S.U. Patap) vvv v Mesozoic Volcanic Package Porphyry early or advance stage projects Mesozoic Fine Sediments 9
Slide 10: Political Distribution & Access
Political Distribution & Access The Para project is located in the Lima Department, specifically on the boundary between Huarochiri and Cañete provinces. The property is accessed from Lima, via Chilca (approximately 6 hours from Lima). LIMA Huarochiri LIMA Province Lima Department PARA Cañete Pr
Slide 11: Community & Claims
Community & Claims Para is located mostly in the community of San SAN FRANCISCO Francisco de Calahuaya, but part are under the DE CALAHUAYA domain of Calango community. Community Good relationship with Calahuaya and Calando communities. The property comprise 2,200 hectares (in 4 mining PARA pr
Slide 12: Stream Sediment
Stream Sediment An initial regional stream sediment survey was conducted revealing a very strong Cu anomaly at Para. 181 ppm Cu The area was defined by 4 samples This initial anomaly is 3 x 4 km in area 344 ppm Cu 151 ppm Cu 161 ppm Cu <150 ppm Cu 151-200 ppm Cu 0 1000m >200 ppm Cu 12
Slide 13: Talus Survey
621 304 Copper talus 20 12 Molybdenum talus Talus Survey 185 9 1 km 115 5 PPM PPM The zonation pattern identified Core Cu-Mo Target in the talus survey displays a Core Cu-Mo Target distinct core enriched in Cu- Mo anomalies with a corresponding depletion in Zn- Pb. This is surrounded by an outer
Slide 14: Rock Sampling
Rock Sampling A total of 389 rock chip samples were collected. The correlation between copper and molybdenum anomalies is a signature typical of porphyry systems. Rock chip sampling confirmed the talus anomaly. >10 ppm Mo <100 ppm Cu 101 - 250 ppm Cu 251 – 500 ppm Cu 501 – 1000 ppm Cu 0 1000m
Slide 15: Veinlets
Veinlets LEACHED C VEINLETS CUTTING MONZODIORITE B VEINLETS IN RHYODACITIC PORPHYRY LEACHED C VEINLEST CUTTING GRANODIORITE Py>Cpy DISSEMINATED IN RHYODACITIC PORPHYRY 15
Slide 16: Geology
Geology Post batholith intrusions hosting porphyry type mineralization in this central part. Two systems of faults; one Northwest- Southeast and other almost East-West, control the emplacement of the porphyritic intrusion related to copper mineralization. 0 1000m Andesitic/Dioritic Dikes Andesit
Slide 17: Lithology
Lithology ANDESITE ANDESITIC DIKE ANDESITE RHYOLITIC PORPHYRY MONZODIORITE GRANODIORITE 17
Slide 18: Magnetic Survey
Magnetic Survey 17 West-East lines were surveyed Magnetic susceptibility 2.6 km long line. Plan view at 1500 msal Separation between lines 400 m. Total survey 34 km. A strong low magnetic anomaly correlates with an area of sericitic alteration identified at surface. B A 0 1000m 1800 msal M
Slide 19: Chargeability Survey
Chargeability Survey 7 West-East lines Chargeability Plan view 2.5 km long line at 1500 msal Separation between lines 400 m Total survey 18km The strong high chargeability anomaly is interpreted to be caused by sulfides within mV/V the system. B A 0 1000m 1800 msal Chargeability 1500 msal
Slide 20: Resistivity Survey
Resistivity Survey 7 West-East lines 2.5 km long line. Separation between lines 400 m. Total survey 18km This strong moderate to high resistivity anomaly could corresponds to the potassic alteration core, a hallmark signature of porphyry-style mineralization. B 0 1000m A 1800 msal Resistiv
Slide 21: Highlights
Highlights Multiple Centers - Para presents evidence of porphyry style mineralization in multiple centers. Positive Geochemistry - Surface geochemical anomalies include stream sediment, talus and rocks. Positive Geophysics - Geophysical surveys including magnetic, induced polarization, and rad
Slide 22: Contact
CONTACT Elyssia Patterson Eduardo Leon 778-683-4324 604-638-3456 www.latin-explore.com info@latin-explore.com 22