Trailbreaker Resources Ltd · TSXV:TBK
Trailbreaker Resources — Investor Presentation (January 2025)
17 slides from Trailbreaker Resources's investor presentation, Jan 28, 2025
Slide 1: Liberty Project
A Canadian mineral exploration company focused on precious TSX.V: TBK metals and copper in British Columbia and Yukon Territory. LIBERTY PROJECT PROJECT HIGHLIGHTS • LOCATION - Central British Columbia • ACCESS - 60 km WNW of Quesnel • INFRASTRUCTURE - Year-round access via network of Forest Service
Slide 2: Location and Infrastructure
LOCATION AND INFRASTRUCTURE • 6,895 hectare claim package, covering prospective Mesozoic intrusions • Located ~60 northwest of Quesnel, BC • High-density network of forest service roads throughout the property • Low annual precipitation means access to the property can be achieved year-round • Gentl
Slide 3: Regional Geology and Deposit Model
REGIONAL GEOLOGY AND DEPOSIT MODEL Cu-Mo Porphyry Potential • The Liberty project sits along the western edge of the Cache Creek terrane, which is host to Cu-Mo porphyry deposits including Taseko’s Gibraltar Mine, north of Williams Lake, BC, which is the second largest open-pit copper mine in Canada
Slide 4: Gibraltar Analog
GIBRALTAR ANALOG • Gibraltar Mine, located ~110 km southeast of Liberty, is mineralized for >8 km strike length • The main areas that were historically mined define a ~3.3 km high- grade core to the system • The lower-grade shoulders of the deposit are now proposed to be mined • The low-grade should
Slide 5: Liberty Exploration History
Property Geology from 2013 Assessment Report LIBERTY EXPLORATION Historic claim boundaries HISTORY • Rio Tinto conducted exploration from 1967 to 1970, due to anomalous Cu in stream sediment samples. Work consisted of soil sampling, IP, trenching, and diamond drilling exploring for porphyry-style an
Slide 6: Exploration Coverage
HISTORIC DATA TRAILBREAKER EXPLORATION COVERAGE Geochemistry • Historic exploration efforts were primarily focussed on a narrow area around a soil geochemical anomaly and mineralized outcrops • These past exploration surveys did not account IP - Chargeability for glacial transportation of till • Pas
Slide 7: Property Geology
PROPERTY GEOLOGY PROPERRYT HISTROY • The property covers a Mesozoic, N-S trending polyphase granodiorite to diorite intrusive complex, which has intruded into the volcanic and sedimentary rocks of the Cache Creek Group • Endako Group and Chilcotin Group basalts overly the Cache Creek Group rocks loc
Slide 8: Drilling
DRILLING • 2,442 m drilled in 7 holes during 2024 • Widespread Cu-Mo porphyry and skarn mineralization, with multiple holes ending in mineralization • Cu grades increase toward the southeast, with increased phyllic alteration, where mineralization is open • Mineralization is associated with chargeab
Slide 9: Copper-Molybdenum Porphyry Mineralization
COPPER-MOLYBDENUM PORPHYRY MINERALIZATION Quartz-sulphide and sulphide veining, associated with phyllic alteration within granodiorite intrusion. LIB24-001 between ~301 m and 304 m. Sample 5232009 (302 m to 303.5 m) assayed 0.41% Cu, 6.5 g/t Ag, 278 ppm Mo. Mineral Legend Cpy = chalcopyrite Mo = mol
Slide 10: High-Grade Copper
HIGH-GRADE COPPER Ultramafic hosted skarn-style alteration with heavily disseminated Cpy-Mo-Py 410.2 m LIB24-003 410.2-416.1 m (5.9 m) assay composite of 0.69% Cu, 1994 ppm Mo, and 5.15 g/t Ag. Mottled skarn alteration 416.1 m Cpy Mo Cpy Mottled skarn alteration Mineral Legend Cpy = chalcopyrite Ma
Slide 11: Geochemistry
GEOCHEMISTRY PROPERRYT HISTROY • A 10 km+ arcuate Cu-in-soil anomaly is defined across the property • Locally anomalous Cu is coincident with Au, Ag, and Mo anomalies • The large scale of the elevated copper is indicative of a large hydrothermal system, as well as glacial transportation • Ice-flow m
Slide 12: Geophysics - ZTEM
GEOPHYSICS - ZTEM • ZTEM surveying defines a property-scale resistive feature interpretated to be an intrusive complex. • 2-3 km wide • Trending N-S to NE-SW • Extends to >2000 m depth • This ‘intrusive complex’ is variably magnetic, which may be caused by: • Different intrusive phases containing va
Slide 13: Geophysics - IP
GEOPHYSICS - IP • IP surveying defines a large arcuate IP anomaly along the southern extent of the resistive ‘intrusive complex’ • This IP chargeability response is strongly coincident with the ‘magnetic destructive’ halo observed in the ZTEM magnetic data • The area of >7 mV/V chargeability respons
Slide 14: Target Summary
TARGET SUMMARY • Based on the ZTEM modelling, the Intrusive Complex appears to extend to at least 2.0 km vertical depth • The IP survey reads to ~700 m vertical depth, but shows that the coincident chargeability feature extends beyond the survey window • Strong chargeability near the ‘High-grade Cu’
Slide 15: Target Summary
TARGET SUMMARY • The strongest coincident high-resistivity (e.g. intrusive complex) and IP- chargeability (e.g. sulphides) is directly 1.0-1.5 km up ice of the strongest coincident multi-element geochemical anomaly • In addition, rock sampling to the north and south of this feature indicate a large
Slide 16: Poised for Discovery
POISED FOR DISCOVERY Underexplored • The surface geochemical signature suggests 2024 drilling may have encountered the margin of a large Cu-Mo porphyry system • Cu-Mo ± Au-Ag-Re porphyry and skarn style mineralization was encountered in all drillholes • The strongest coincident targets are under ove
Slide 17: Contact
Please contact us for more information: Daithi Mac Gearailt, President and CEO Tel: (604) 681-1820 info@trailbreakerresources.com www.trailbreakerresources.com A Canadian mineral exploration company focused on precious TSX.V: TBK metals and copper in British Columbia and Yukon Territory.
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