Lion Copper Corp. · CSE:LCU
Lion Copper — Lion Copper and Gold — Investor Presentation (January 2022)
18 slides from Lion Copper's investor presentation, January 2022
Slide 1: Chaco Bear & Ashton Properties
CHACO BEAR & ASHTON Properties Pipeline Projects in British Columbia, Canada TSX-V: LEO | OTCQB: LCGMF www.lioncg.com ASSET PRESENTATION January 2022 TSX-V: LEO | OTCQB: LCGMF
Slide 2: Cautionary Notes to US Persons & Forward-Looking Statements Disclaimer
Cautionary Notes to US Persons & Forward- Looking Statements Disclaimer The information contained in this presentation is provided solely for general knowledge purposes. This presentation is not intended to be a comprehensive review of all matters and developments concerning the Company and we assum
Slide 3: Chaco Bear Property and Ashton Property
Chaco Bear Property BC, Canada LOCATED DIRECTLY EAST OF THE GOLDEN TRIANGLE Ashton Property BC, Canada LOCATED IN EMERGING SPENCES BRIDGE GOLD BELT 3
Slide 4: BC Copper-Gold Prospects
BC Copper-Gold Prospects PARALLEL TO METAL-RICH SYSTEMS THROUGHOUT THE PACIFIC RIM Evidence of all 3 distinct ore systems on both properties: 1. Porphyry Copper-Gold 2. High-Sulphidation Epi- Mesothermal Copper-Gold 3. Porphyry related Low Sulphidation Epi- Mesothermal Gold THESE SYSTEMS OF ORE DEPO
Slide 5: Chaco Bear Regional Geology
Chaco Bear REGIONAL GEOLOGY GOLDEN TRIANGLE STRIKING SIMILARITIES BETWEEN THE CHACO BEAR AND ESKAY CREEK LITHOLOGIES COPPER CORRIDOR TSX-V: LEO | OTCQB: LCGMF 5
Slide 6: Chaco Bear
Chaco Bear Location: – Northern B.C., Driftwood River, Bear Lake Area Andesite flows and tuffs Geological Info: – Located within the Stikine Terrane – Mineralization hosted by the Telkwa Formation Rusty Lake: Highest stream of the Hazelton Group, separated from the sediment anomaly younger Hazelton
Slide 7: Same Lithologic Units at Eskay Creek and Chaco Bear
Chaco Bear SAME LITHOLOGIC UNITS AT ESKAY CREEK AND CHACO BEAR andesite/dacite flows Upper part of Hazelton not yet identified mineralized rhyolite Unmapped terrain to the east Lower part of Hazelton identified at Chaco Bear MINERALIZED ZONES SYNOVOLCANIC FAULTS AND INTRUSIVES Chaco Bear; looking no
Slide 8: Primary Exploration Targets
Chaco Bear PRIMARY EXPLORATION TARGETS • Eskay Creek type mineralization east (above) rhyolite unit • Epithermal Gold at Round Lake • Epithermal Gold & Base Metals at Dave/Ron & BearNx Zones • Step-outs at Coccola - drill intercepts with Cu/Au mineralization in rhyolite • Porphyry Copper near Rusty
Slide 9: Epithermal Vein Mineralization; Rhyolite & Andesite Hosted Gold Mineralization
Chaco Bear EPITHERMAL VEIN MINERALIZATION RHYOLITE & ANDESITE HOSTED GOLD MINERALIZATION Sulfide-rich vein filling Drill Core of flow banded rhyolite in (0.75 opt Au, 6 opt Ag, 14% Cu) drill core with assay of 6.37 ppm Au Massive sulfide vein Drill Core of flow banded rhyolite 37% Cu, 307 opt Au TSX
Slide 10: Additional Exploration Targets
Chaco Bear ADDITIONAL EXPLORATION TARGETS • Potential for epithermal gold and related base metal mineralization • Target deposit types are: – High grade epithermal gold-silver vein and/or network vein mineralization hosted in the andesite-dacite volcanics – Porphyry-copper-gold prospect (Rusty Lake
Slide 11: Ashton: Spences Bridge Gold Belt
Ashton SPENCES BRIDGE GOLD BELT TSX-V: LEO | OTCQB: LCGMF
Slide 12: Porphyry Copper Gold Potential
Ashton PORPHYRY COPPER GOLD POTENTIAL Location: • Within 10 km of Lytton in southern BC • 19 km south of Spences Bridge on the east bank of the Thompson River • Within a few hundred meters of the Trans‐Canada Highway and the mainline of the Canadian Pacific Railway History: • Situated near, and like
Slide 13: Past Exploration
Ashton PAST EXPLORATION • 1968-1969. A large copper soil-anomaly was found • 1989-1990. A very low frequency electromagnetic (VLF-EM) survey outlined a prominent north‐striking magnetic anomaly • 1992. Geochemical sampling and a limited mapping program confirmed the copper anomaly; a significant cha
Slide 14: Local Geology and Alteration
Ashton LOCAL GEOLOGY AND ALTERATION Strong propylitic alteration at Ashton indicates the presence of a concealed porphyry system • Propylitic alteration of a diorite intrusive can be subdivided into a central actinolite dominant zone and a more distal epidote-chlorite-calcite zone • The central acti
Slide 15: Gold Skarn Potential
Ashton GOLD SKARN POTENTIAL • The interpreted porphyry is based on IP and MMI geochemical surveys • The gold skarn target to the east is GOLD SKARN TARGET interpreted from an EM conductor • The composite intrusive system at Ashton is noted as (“mafic”) diorite with a fractionated quartz-diorite phas
Slide 16: Additional Gold Potential
Ashton ADDITIONAL GOLD POTENTIAL • Gold mineralization is found to the south of the copper porphyry at Ashton (MMI anomaly) • Additional gold pathfinder elements associated with Au anomaly (As, Te, Hg, Sb, Se, and Ag) • Epithermal gold can have a direct relationship with a porphyry system • Low sulf
Slide 17: Going Forward – Exploration Strategy
Ashton GOING FORWARD – EXPLORATION STRATEGY • Additional geological mapping and surface prospecting of property • Further mapping and surface sampling will be focused on the southern portion of the Ashton Project where there are extensive gold in soil anomalies • Drilling to evaluate a potential gol
Slide 18: Lion Copper & Gold Corp. Corporate Communications
LION COPPER & GOLD CORP. Corporate Communications [email protected] www.lioncg.com TSX-V: LEO | OTCQB: LCGMF TSX-V: LEO | OTCQB: LCGMF 18
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