Latin Explore Inc. · TSXV:LXE
Latin Explore — Technical Presentation (October 2026)
22 slides from Latin Explore's technical presentation, October 2026
Slide 1: Para Project Technical Presentation
DRILL-READY EXPLORATION COMPANY POSITIONED FOR DRILL CATALYSTS IN 2026 PARA PROJECT TECHNICAL PRESENTATION October 2026 TSXV: LXE Porphyry Cu-Mo System Year-Round Access Q4 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 chips. ▪ Positive Geophysics - Geophysical surveys including magnetic, induced polarization, a
Slide 3: Project Portfolio
Project Portfolio Foundation assets with scale and discovery potential Peru – 100% Owned Projects ELIDA ELEMENT 29 Para Near-term drilling on a large, undrilled porphyry system Strong technical dataset supports first drill testing in Q4 2026 Lima Auquis District-scale copper–base metal system with m
Slide 4: Metallogenic Belts
Metallogenic Belts ▪ Cretaceous porphyry belt of Peru was historically recognized between Ica and Arequipa but now extends north of Lima following the discovery of the ILLARI deposit (Newmont) and subsequent exploration successes. ELIDA ▪ Current exploration activities for copper are in progress loo
Slide 5: Regional Metal Endowment
Regional Metal Endowment ILLARI Coastal batholith Para Porphyry project Miocene volcanics Package Eocene-Miocene Sedimentary Package SUMACWAYRA VMS Mines Mesozoic Fine Sediments Porphyry early or advance stage projects vvv v Cretaceous Volcanic Package LACSHA VMS early or advance stage projects Meso
Slide 6: Regional Geology
Regional Geology ▪ The regional geology is dominated by the coastal batholith, a large intrusive complex formed during ILLARI the upper Cretaceous to lower Tertiary period. ▪ Complex is dominated by granodiorite-tonalite SUMACWAYRA plutonic rocks. ▪ The Santa Rosa, Patap, and Tiabaya Super Units LAC
Slide 7: Structural Framework
Structural Framework • The regional structural framework of the region is a key ILLARI control on the emplacement and preservation of porphyry- style mineralization. SUMACWAYRA Two dominant structural trends have been identified: LACSHA • NW-SE fault system: These major regional faults are LEZARD ma
Slide 8: 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 v v v v v v PARA v v v v v v Post. Batholith v v v v v v v v v v v v Quilmana Fm. Tabiya super unit Upper v v v v v v (Andesitic flows) I
Slide 9: District and Local Geology
District and Local Geology • The Project is underlain by intrusive rocks of the Coastal Batholith, specifically the Upper Cretaceous Tiabaya and Patap Super Units, which serve as the principal hosts for porphyry-style mineralization in the region. • These rock types are dominantly dioritic in nature
Slide 10: Project Geology
Project Geology • The structural framework of the Project is a key control on the emplacement and preservation of Latin Explore Inc porphyry-style mineralization. • The Project area is situated within a structurally complex segment of the Coastal Batholith, where multiple fault systems intersect and
Slide 11: Stream Sediment
Stream Sediment • A total of four stream sediment composite samples were collected in the Project area in 181 ppm Cu 2021, as part of a regional prospecting program to identify areas prospective for porphyry-style copper-molybdenum mineralization. <150 ppm Cu 344 ppm Cu • The program was designed to
Slide 12: Talus Survey
Talus Survey 621 Copper talus 20 Molybdenum talus 304 12 185 9 ▪ The zonation pattern identified 1 km 115 5 in the talus survey displays a PPM PPM distinct core enriched in Cu- Core Cu-Mo Target Mo anomalies with a Core Cu-Mo Target corresponding depletion in Zn- Pb. ▪ This is surrounded by an outer
Slide 13: Rock Chip Sampling
Rock Chip Sampling Copper Rock Chip Samples • Total of 389 rock chip samples collected. Core Cu-Mo anomaly • Results showed anomalous copper >10 ppm Mo concentrations ranging from >100 ppm to a maximum of 17,090 ppm, with elevated <100 ppm Cu molybdenum values (>10 ppm up to 89.9 ppm) 101 - 250 ppm
Slide 14: Lithology
Lithology • The Project features a sequence of post-batholith intrusions, including monzodiorite, granodiorite, and porphyritic rocks, which are spatially associated with copper- molybdenum mineralisation identified in surface sampling. • Andesitic and dioritic dykes crosscut the earlier intrusive p
Slide 15: Mineralization and Alteration
Mineralization and Alteration At the Central Anomaly, phases hosting copper mineralization include: • A greenish-brown, medium-grained porphyritic andesite with weak sericite alteration and mineralization characterized by copper oxides, associated with hematite and goethite. The mineralization is pr
Slide 16: Mineralization and Alteration
Mineralization and Alteration LEACHED C VEINLETS CUTTING MONZODIORITE B VEINLETS IN RHYODACITIC PORPHYRY COPPER CARBONATES IN FRACTURES IN DIORITE LEACHED C VEINLEST CUTTING GRANODIORITE Py>Cpy DISSEMINATED IN RHYODACITIC PORPHYRY COPPER CARBONATES IN FRACTURES IN DIORITE 16
Slide 17: Geophysics – Magnetic Survey
Geophysics – Magnetic Survey ▪ 17 West-East lines were surveyed Magnetic susceptibility ▪ 2.6 km long line. Plan view at 1400 masl ▪ Separation between lines 400 m. ▪ Total survey 34 km. ▪ A strong low magnetic anomaly correlates with an area of sericitic alteration identified at surface. 0 1000m Ge
Slide 18: Geophysics – Chargeability Survey
Geophysics – Chargeability Survey ▪ 7 West-East lines Chargeability Plan view at 1400 masl ▪ 2.5 km long line ▪ Separation between lines 400 m ▪ Total survey 18km ▪ The strong high chargeability anomaly is interpreted to be caused by sulfides within the system. mV/V 0 1000m Geophysical information p
Slide 19: Coincident Magnetic and IP anomalies
Coincident Magnetic and IP anomalies Large, coherent, and well-defined magnetic low Coincident with Prominent, coherent chargeability anomaly measuring 1.8km X 1.6km up to 800 depth Underlying a well- defined surface copper-molybdenum anomaly Geophysical information provided by VALE, reinterpreted b
Slide 20: 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 21: 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 22: Contact
CONTACT Donovan Pienaar Eduardo Leon 604-312-1595 604-638-3456 www.latin-explore.com info@latin-explore.com 22
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