Bcm Resources Corporation · TSXV:B
Bcm Resources — Investor Presentation (January 2025)
27 slides from Bcm Resources's investor presentation, Jan 30, 2025
Slide 1: Thompson Knolls - New Copper-Gold-Molybdenum Discovery in the Great Basin, Western Utah
Sergei Diakov Thompson Knolls - New Copper-Gold-Molybdenum Discovery in the Great Basin, Western Utah January 30, 2025 1
Slide 2: Cautionary Notes & Forward-Looking Statements
Cautionary Notes & Forward-Looking Statements • This presentation contains certain information that may be deemed “forward-looking statements,” or "forward-looking information” (as defined under applicable securities laws), with respect to BCM Resources Corp. (the “Company” or “BCM Resources,” or “B
Slide 3: BCM Resources: Management & Directors
BCM Resources: Management & Directors Scott Steeds Chairman of the Board of Directors •Over 20 years of experience at large successful Venture Capital firms working with high-net-worth individuals and Institutional investors actively financing/investing in high-profile mineral exploration projects w
Slide 4: BCM Resources: Technical Team
BCM Resources: Technical Team WORLD-RENOWNED EXPLORERS WITH PROVEN SUCCESSFUL DISCOVERY TRACK RECORD: Dr. Sergei Diakov, MSc (Hons) Economic Geology and Mining Engineering, PhD Economic Geology, Associate Professor, Peoples' Friendship University, Moscow, Russia •More than 30 years of global explora
Slide 5: Thompson Knolls: General Introduction
Thompson Knolls: General Introduction • BCM Resources Corporation (Symbol "B", TSX- Venture Exchange), (“Company”, “B”, “BCM”, “BCM Resources”) is a diversified Canadian mineral exploration company focused on the continued exploration of its flagship Thompson Knolls (TK) Porphyry Cu-Au-Ag-Mo project
Slide 6: Geographic Location
Geographic Location • Thompson Knolls is in Utah’s Millard County, 28 km (17 miles) east of the Nevada- Utah border, 4 km (2.5 miles) south of Highway 6/50 – the “Loneliest Road in America” TK TK TK 6
Slide 7: Regional Geology
Regional Geology • The TK Property lies west of the Confusion Range known for numerous outcropping gold- bearing jasperoids, including at the King’s Canyon gold deposit ~8 km (5 miles) to NE of TK • The Property ground is covered by post-mineral fanglomerates composed of products of weathered destru
Slide 8: TK Regional Geology
TK Regional Geology D D’ TK Project Legend TK Project location Gold-silver occurrences Base metal occurrences Copper occurrences 8
Slide 9: BCM's TK Landholdings
BCM’s TK Landholdings Legend Recently claimed BLM ground Company claims on BLM land Company leases on SITLA land Highway I50 from Ely to Delta Existing unpaved roads The TK Property comprises 225 BLM claims and 2 parcels of Utah State leased lands totaling 2,242 ha (5,540 acres) 9
Slide 10: Exploration History
Exploration History • Exploration history started with a U.S. Geological Survey aeromagnetic survey conducted in 1972. The survey outlined a prominent magnetic “high” anomaly at TK, which led to the later formulation of a porphyry copper deposit model for this target area • From 1989 to 1996, Crown
Slide 11: TKP Geophysical / Geological Data Integration
TKP Geophysical / Geological Data Integration • BCM technical team compiled all historical geophysical data into 3D geophysical model • Combined geophysical and geological drilling data with surface geology were used as base model for directing targeted drilling in highly mineralized parts of the TK
Slide 12: Thompson Knolls Project Current Status
Thompson Knolls Project Current Status • “B” is on the hunt for an “Elephant-size” porphyry copper deposit in Utah, and TK is essentially a blind target • The TKP Porphyry/Skarn system is buried under Fanglomerate cover of varying thickness • “B” applied for and received a 10-year Plan of Operation
Slide 13: TK Phase 1, -2 and -3 Drillhole Locations
TK Phase 1, -2 and -3 Drillhole Locations TK14 Magnetic anomaly area 1 N Magnetic anomaly area 2 Drillholes completed in Phase 3 drillholes* Magnetic anomaly TKP property Phases 1 and 2 areas 1 and 2 boundary Note: * TK11 and TK13 remain undrilled, TK12 is only partially drilled 13
Slide 14: Longitudinal Section Line DG
Longitudinal Section Line DG NWW SEE TK12 G U D Note TK6, TK14, TK7 and TK4 are projected to cross-section 14
Slide 15: Selected Images of Mineralized Core
Selected Images of Mineralized Core Photo 1. Drill hole TK6 at 1,042.4 m (3,420 ft) depth. Sulfide-rich magnetite breccia in 70.1 m (230 ft) core interval of the “Eureka” skarn zone Photo 2. Drill hole TK6 a 9.1 m (30 ft) interval from 1,036.3 to 1,045.5 m (3,400 to 3,430 ft) that assayed 0.97% Cu,
Slide 16: Selected Images of Mineralized Core
Selected Images of Mineralized Core Photo 3. TK8 drill hole interval from Photo 4. TK8 drill hole 10-ft (3 m) interval 664.5-667.5 m (2,180 to 2,190 ft) with from 676.7-679.7 m (2,220 to 2,230 ft) intense sulfide-magnetite brecciated detail with massive sulfide-magnetite- marble skarn that assayed 1
Slide 17: Research Prelude
Research Prelude • In Summer 2023, BCM, together with Crescat Capital, became a part of the CASERM program at Colorado School of Mines (CSM) • CASERM researchers: Dr. Mathias Burisch Hassel (CSM Associate Professor) and Chad Abarbanel (CSM MS Student) were assigned to review the TK core • In April 2
Slide 18: Core Re-Logging Summary
Core Re-Logging Summary • The new logging data imply discontinuous skarn packages that are intersected in drill holes TK6, TK8, TK9 and TK14 as well as at the very bottom of TK5 • Intersected skarn intervals are represented mainly by distal skarn mineral assemblages of pyroxene and serpentine, where
Slide 19: Schematic Geological Model of the Thompson Knolls Porphyry/Skarn System
Schematic Geological Model of the Thompson Knolls Porphyry/Skarn System Looking NW 19
Slide 20: Research Results
Research Results • The geometry and mineralogy of skarn alteration intersected to date indicate that the Copper core of the Skarn and Porphyry system remains outside the area of recent exploration drilling • Relatively high Cu grades associated with this intermediate-distal skarn is encouraging beca
Slide 21: Our Interpretation
Our Interpretation Legend TK Mag anomaly a b Base metal ratio isolines: a) supported by drilling results Vector of fluid movement b) interpreted extensions 21
Slide 22: Conclusions & Recommendations
Conclusions & Recommendations • The fluid migration pathways deduced from these observations could be from the SW to the NE, or from both the SW and N • The most obvious scenario is that the fluids came from SW from the geophysical anomalous Area 2, hence this area deserves primary attention for fol
Slide 23: Future Drilling Plans
Future Drilling Plans • Company’s vector path to the core of the TK mineralized system continues to be refined with each phase of drilling. After Phase 3 with more drilling data available we are now able to apply a more scientific approach in our exploration program • Our focus will turn to drilling
Slide 24: Planned Drillholes Under Plan of Operations: Proposed Holes in Area 2
Planned Drillholes Under Plan of Operations: Proposed Holes in Area 2 N TK6 TK5 TK14 TK9 TK8 TK3a TK10 TK3 Area 1 TK15 TK11 TK1 TK16 TK7 TK2 TK17 TK4 TK12 TK13 Legend Company claims on BLM land DK14 DK DK13 1 Company leases on SITLA land DK Previously drilled holes 8 DK12 Area 3 Area 2 DK10 Drill ho
Slide 25: Future Exploration
Future Exploration • With the successful outcome of the proposed Phase 4 drill program delivering economic intercepts in skarn and porphyry mineralization, our focus will be directed at the western anomalous Area 2 with additional drill testing of its southern extension • Anticipated economic interc
Slide 26: For further information to this presentation please contact
For further information to this presentation please contact: Sergei Diakov Phone: (760) 803-0506 Email: sdiakov@gmail.com or sdiakov@bcmresources.com 26
Slide 27: END
BCM Resources Corp END