Slide 1: Auquis Technical Project
DRILL-READY EXPLORATION COMPANY POSITIONED FOR DRILL CATALYSTS IN 2026 AUQUIS TECHNICAL PROJECT May 2026 TSXV: LXE Porphyry Cu-Mo System Year-Round Access Q3 2026 drilling
Slide 2: Highlights
Highlights Location – Auquis is located 400 km south of Lima, Peru. Discovery – Identified through regional geochemical interpretation of the Cretaceous Porphyry Belt. Ownership – 100% owned by Latin Explore Inc. Positive Geochemistry – Soil and rock geochemistry used to define target areas.
Slide 3: Exploration Belt
Exploration Belt Cretaceous Porphyry Belt – The Cretaceous porphyry belt of Peru was historically recognized between Ica and Arequipa but has since been extended north of Lima following the discovery of the Illari deposit (Newmont) and subsequent exploration successes. ELIDA Active Exploration –
Slide 4: Copper Endowment
Copper Endowment TILLO MARIA GRACIA PARA Lara Project drill highlights include 218m @ 0.57% copper and 0.04% molybdenum. TAURIPAMPA LEZARD Tingo Project drill highlights include 30m @ 0.32% copper (RC drilling). The northern portion of the belt remains underexplored, with many projects represe
Slide 5: Regional Geology
Regional Geology TILLO MARIA GRACIA PARA Casma Group (Chilca Fm., Pamplona Fm.) and the Rimac Group host the main VMS-style mineralization. TAURIPAMPA The Santa Rosa and Tiabaya Superunits form part of the Coastal Batholith and act as the primary hosts for younger porphyritic intrusions associat
Slide 6: Structural Framework
Structural Framework TILLO MARIA GRACIA PARA Deposits are strongly controlled by the intersection of major structural trends: East-west low magnetic trends identified through airborne magnetic surveys. Major mapped fault systems trending northwest-southeast. A possible relationship to deeper
Slide 7: Stratigraphic Column
Cenozoic Stratigraphic Column Quaternary Sacsaquero / Castrovirreyna Neogene (Volcanics) AUQUIS Chulec formation Upper (Limestone) Cretaceous Mesozoic V V V V V V V V V V V V V V V V V V Lower V Gd V V V V V V V V Copara volcanics Cretaceous V V Tn V V V V V V V (Andesitic flows) V V V V V V V V V V
Slide 8: District Geology
District Geology The Upper Cretaceous Coastal Batholith JATUM ORCCO (Tiabaya Superunit) is the primary host of porphyry copper mineralization. AUQUIS PUQUIO TINGO Auquis Skarn/Porphyry Project PUCACORRAL VMS Mines Porphyry early or advance stage projects 0 10km VMS early or advance stage projects
Slide 9: Schematic Section
Schematic Section A B AUQUIS JATUN ORCCO 5000 msal PUQUIO v v v v v v v v v v v v v v ` v v v v v v v v v v v v v v v v v v v v 2000 msal v v v v v v v v v v vv v v v vv v 0 msal 0 5km Auquis Skarn/Porphyry Miocene Volcanic Package Costal Batholith: (S.U. Tiabaya, S.U. Patap) vvv Porphyry early or a
Slide 10: Political Distribution & Access
Political Distribution & Access 0 30km The Auquis Project is located in the Huancavelica Department, specifically in the southern part of Huaytara Province. The project has established road access from Lima via Ica, HUANCAVELICA with an approximate driving time of 9 hours. LIMA AUQUIS ICA Huanca
Slide 11: Community & Claims
Community & Claims Auquis is located between two communities: Santo Domingo de Capillas and San Francisco de Sangayaico. The Company maintains strong relationships with both communities. Prospecting permits are in place, and the exploration permit required for drilling is advancing toward appr
Slide 12: Geology
Geology Post-batholith intrusions host porphyry- style mineralization, with northwest– southeast and east-west fault systems controlling intrusion emplacement and copper mineralization. BLANCO ZONE Young volcanics ROSE ZONE Tuff volcanics Limestone Skarn Monzonite Granodiorite 0 1km Modified after
Slide 13: Lithology
Super Unit Tiabaya Lithology Chulec Formation Post Coastal Batholith Mineralization Event Tonalite Granodiorite Monzonite Limestone Calcrete Porphyry Dacite Rhyodacite 13
Slide 14: Soil sampling
Soil sampling A total of 253 soil samples were collected and sent to the laboratory for ICP analysis, and 291 samples were analyzed using pXRF. The correlation between copper and molybdenum anomalies is characteristic of porphyry systems in the southeast part of the property. BLANCO ZONE A zin
Slide 15: Soil Survey
Soil Survey Cu Rose Zone 2 km x 1 km zone. ROSE ZONE Blanco Zone 2 km x 1 km zone. 2820 ppm 958 ppm 128 ppm 330 ppm 610 ppm 30 % 30 % 20 % 10 % 10 % Pb Zn BLANCO ZONE BLANCO ZONE 192 ppm 354 ppm 71 ppm 45 ppm 356 ppm 20 ppm 29 ppm 124 ppm 163 ppm 213 ppm 30 % 30 % 20 % 10 % 10 % 0 1km 30 % 30 %
Slide 16: Rock Sampling
Rock Sampling A total of 456 rock chip samples were collected across the property. Strong anomalous values within the copper and molybdenum zone, identified by the soil survey, were further tested with rock chip sampling. BLANCO ZONE Results confirm the presence of high- grade copper mineraliz
Slide 17: Alteration in Rock Chips
Alteration in Rock Chips The Na/Al diagram indicates dominant sericite alteration, with a potassic overprint characterized by secondary biotite. Strong Sericite Moderate Sericite Sericite-Chlorite Secondary biotite? 17
Slide 18: Veinlets
Veinlets The primary geological expression of economic copper mineralization in the Lima–Ica segment of the Coastal Batholith is the presence of leached iron oxide (FeOx) veinlets filling fractures. This expression extends over a width of 1 to 2 km, as shown in the upper image. The core zone of
Slide 19: Mineralization
Mineralization Mineralization in Rose Zone Green copper and chalcopyrite in fractures and stains Mineralization in Blanco Zone Copper carbonates sulfates and silicates in skarn zones 19
Slide 20: Rose Zone
Rose Zone 3.01%Cu 0.36%Cu The strong copper and molybdenum anomaly identified by the soil survey was subsequently 4.74%Cu tested with rock chip sampling. 1.27%Cu, 219ppmMo Results confirm high-grade copper mineralization, with porphyry-style veinlets and associated 0.59%Cu mineralization also ob
Slide 21: Blanco Zone
Blanco Zone 0.23%Cu The strong zinc–copper anomaly identified by the soil survey was subsequently tested with rock chip sampling. Results confirm high-grade zinc–copper–silver– 6.04% Pb, 9.30% Zn, 1.40% Cu, 82.7 ppm Ag lead mineralization in the area, where skarn 4.66% Pb, 0.81% Zn, 0.54% Cu, 17
Slide 22: Skarn Stages
Skarn Stages Prograde Skarn Stage Brown garnets Pyroxenes Retrograde A Stage Epidote Amphibole Quartz Retrograde B Stage Chlorite Sulfides Supergene Stage Green coppers 22
Slide 23: Magnetic Survey
3400 A BLANCO ZONE B ZONE ROSE ZONE B 3400 C ROSE ZONE P ZONE D Magnetic Survey 2900 2900 2400 2400 A total of 19 west–east lines were surveyed. Line lengths range from 2 to 7 km. Line spacing is 200 m. 0 1km Total survey coverage is 34 km. The Rose area exhibits a dominant low P ZONE magnetic
Slide 24: Schematic Sections
Schematic Sections Conceptual model following the magnetic survey. Several copper occurrences have been identified, indicating potential for both porphyry and skarn-style mineralization. A DCIP survey is planned to further refine targeting. Cu-Mo in Soils and Rock Chips Young Volcanics Cpy-Mo
Slide 25: Highlights
Highlights Location – Auquis is located 400 km south of Lima, Peru. Discovery – Identified through regional geochemical interpretation of the Cretaceous Porphyry Belt. Ownership – 100% owned by Latin Explore Inc. Positive Geochemistry – Soil and rock geochemistry used to define target areas.
Slide 26: Contact
CONTACT Elyssia Patterson Eduardo Leon 778-683-4324 604-638-3456 www.latin-explore.com info@latin-explore.com 26