FIN Resources Ltd
- ASX Code: FIN
- Market Cap: $17,574,088
FIN Resources Strikes High-Grade Gold at Cabin Lake: First Hole Delivers 26.2m at 12.0 g/t Au
FIN Resources Limited (ASX: FIN) has opened its 2026 drilling campaign at the Cabin Lake Gold Project in Canada's Northwest Territories with a standout result. The FIN Resources Cabin Lake gold drilling results in Canada have immediately captured attention, with the first hole intersecting 26.2 metres at 12.0 grams per tonne (g/t) gold from just 14.88 metres depth, confirming a broad, continuous, and structurally controlled high-grade gold system from near-surface.
The result from drillhole CL-26-001 at the Arrow Prospect is not an isolated spike. The intersection is characterised by multiple stacked high-grade zones with consistent internal grade continuity — the hallmark of a coherent sulphide-hosted system rather than erratic, nuggety mineralisation.
With eight additional holes completed across Arrow, Beaver, and Andrew South and results pending, this opening intercept sets a compelling tone for the remainder of the 2026 programme.
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The Numbers That Matter: Breaking Down CL-26-001
The headline result sits within a broader mineralised envelope that extends well beyond the primary high-grade zones, providing strong evidence of a large-scale system with significant vertical and lateral extent.
| Interval Type | From (m) | Length (m) | Grade (g/t Au) | Cut-off Applied |
|---|---|---|---|---|
| Broad mineralised envelope | 14.88 | 36.12m | 8.96 g/t Au | ~1 g/t |
| Primary high-grade interval | 14.88 | 26.2m | 12.0 g/t Au | Composite |
| Higher-grade sub-interval | 15.85 | 14.42m | 12.30 g/t Au | 5 g/t |
| High-grade sub-interval | 18.00 | 3.50m | 12.76 g/t Au | 8 g/t |
| High-grade sub-interval | 22.50 | 7.77m | 14.65 g/t Au | 8 g/t |
| Second high-grade zone | 31.46 | 9.54m | 13.89 g/t Au | 5 g/t |
| Including | 32.00 | 8.00m | 15.50 g/t Au | 8 g/t |
| Peak assay result | — | 0.50m | 34.6 g/t Au | Individual sample |
Note: All intervals reported as downhole lengths. True widths have not yet been determined.
Key observations from the assay data:
- Multiple individual samples returned assays above 10 g/t Au throughout the mineralised interval, including results of 16.5 g/t, 20.1 g/t, 20.8 g/t, 23.7 g/t, 28.0 g/t, 32.6 g/t, and a peak of 34.6 g/t Au
- Gold grades are consistently distributed with limited evidence of erratic high-grade spikes, supporting a non-nuggety, coherent sulphide-hosted system
- Mineralisation commences from shallow depth (14.88 metres), directly underlying overburden — a meaningful advantage for any future development scenario
- The hole extended beyond the main mineralised zone into lower-grade material at depth, suggesting the system remains open
Comparing to the Best Historical Result at Cabin Lake
CL-26-001 did not emerge from untested ground. Historical drilling at Arrow has already returned strong results, and the new hole reinforces and extends that picture considerably.
| Drillhole | Key Intercept | Grade | Depth From Surface |
|---|---|---|---|
| CL-20-08 (historical) | 31.4m | 15.2 g/t Au | 17.5m |
| CL-26-001 (2026) | 26.2m | 12.0 g/t Au | 14.88m |
The consistency between CL-20-08 and CL-26-001 — both showing broad, near-surface high-grade intervals from approximately 15–18 metres — provides important geological confirmation. Furthermore, higher-grade zones in both holes demonstrate a subparallel orientation to the host lithology, indicating a structurally controlled and laterally repeatable mineralised system rather than a localised anomaly.
Chairman Bruce McFadzean commented:
"These are exceptional results from the first hole of the programme and confirm we are into a strong, continuous gold system at Arrow. The intersection of 26.2 metres at 12.0 grams gold per tonne from 14.88 metres is supported by coherent higher-grade zones, including 14.42 metres at 12.30 grams per tonne and 7.77 metres at 14.65 grams per tonne, highlighting the strength and consistency of mineralisation. The scale of the intersection and continuity of high-grade zones provides strong confidence in the underlying system."
Understanding the Geology: Why Sulphide-Hosted Gold in BIF Matters
What Is Banded Iron Formation (BIF)-Hosted Gold?
Banded Iron Formation, or BIF, is an ancient rock type composed of alternating layers of iron-rich minerals and silica. In certain geological settings — particularly within Archaean-age cratonic terranes — BIF sequences can act as chemical and structural traps for gold-bearing hydrothermal fluids. When those fluids interact with the iron-rich rock, sulphide minerals such as pyrite and pyrrhotite precipitate, and gold is deposited with them.
Why Does This Matter to Investors?
- BIF-hosted gold systems tend to be laterally and vertically extensive, following the geometry of the original iron formation stratigraphy
- Gold in these systems is typically fine-grained and hosted within sulphide minerals, meaning grades are often consistent and predictable — exactly what FIN is observing at Arrow
- The deposit style is well understood and has been successfully mined elsewhere in the Slave Province, including the Lupin Gold Mine, which produced more than 3.3 million ounces at grades above 10 g/t Au from a similar geological setting
Glossary of Key Terms
| Term | Plain-English Meaning |
|---|---|
| BIF (Banded Iron Formation) | Ancient layered rock that can host sulphide-bearing gold mineralisation |
| Sulphide-hosted gold | Gold that occurs within sulphide minerals like pyrite, rather than as free gold |
| Structurally controlled | Mineralisation that follows geological structures such as faults or folds |
| g/t Au | Grams of gold per tonne of rock — the standard measure of gold grade |
| Downhole length | The distance measured along the drill hole, not the true width of the mineralised zone |
| Cut-off grade | The minimum grade used to define a reported mineralised interval |
| IP (Induced Polarisation) | A geophysical method used to detect sulphide minerals underground |
| JORC Code | The Australian standard for reporting mineral exploration results and resources |
Three Prospects, One Integrated System: The Cabin Lake Big Picture
The Cabin Lake Gold Project covers approximately 400 hectares in the Northwest Territories, located ~105 kilometres northwest of Yellowknife in Canada. The project targets a continuous ~15 kilometre strike extent of the Bugow Iron Formation, with multiple active prospects.
| Prospect | 2026 Drilling Status | Assay Status |
|---|---|---|
| Arrow | CL-26-001, CL-26-002, CL-26-003 completed | CL-26-001 reported; CL-26-002 and CL-26-003 pending |
| Beaver | CL-26-004, CL-26-005, CL-26-006 completed | Pending — logging, sampling, and interpretation underway |
| Andrew South | CL-26-007 (163m), CL-26-008 (200m) completed | Pending — testing alternative plunge orientation and potential stacked lenses |
The multi-prospect approach is significant. Rather than concentrating drill activity on a single zone, FIN is simultaneously testing the lateral extent of the Bugow Iron Formation gold system across multiple priority targets.
Andrew South is particularly notable — the two most recently completed holes are testing an alternative plunge orientation, which could reveal stacked or offset mineralised lenses within the BIF sequence, potentially adding a new dimension to the project's geometry.
Geophysics Adds a Powerful Layer to Targeting
Alongside the drill programme, FIN is running an integrated geophysical campaign designed to map the sulphide system at depth and along strike — and to guide the next phase of drilling with greater precision.
The programme includes three complementary techniques:
- Downhole Induced Polarisation (DHIP) — being trialled during the current programme to detect sulphide-rich zones from within the drill hole itself, allowing direct comparison with assay results
- Surface Dipole-Dipole IP Surveys — identifying chargeability anomalies associated with sulphide mineralisation across a broader footprint
- Ground Magnetics Surveys — mapping structural features and contacts within the Bugow Iron Formation
These datasets are being integrated with geological logging and drilling results to:
- Identify sulphide-rich zones by their chargeability responses
- Map the geometry of mineralised bodies along strike and at depth
- Identify structures that may be focusing gold mineralisation
- Refine targets for follow-up drilling
The combination of a strong first hole and an expanding geophysical dataset consequently positions FIN to make increasingly targeted drilling decisions as the 2026 programme advances.
What's Coming Next: Near-Term Catalysts
With eight holes completed and only one set of results reported, the news flow from the FIN Resources Cabin Lake gold drilling results in Canada is just getting started. Investors should watch for the following catalysts in the coming weeks:
| Upcoming Catalyst | Holes Involved | Significance |
|---|---|---|
| Arrow follow-up assays | CL-26-002, CL-26-003 | Test continuity and lateral extent of Arrow mineralisation |
| Beaver assay results | CL-26-004, CL-26-005, CL-26-006 | First 2026 results from Beaver — three holes completed |
| Andrew South assay results | CL-26-007, CL-26-008 | Testing alternative plunge and potential stacked lenses in new area |
| Integrated geophysics interpretation | All prospects | Expected to refine targets and vector towards high-grade extensions |
| Follow-up drill target refinement | Across 15km corridor | Eight high-priority, fully permitted targets remain along strike |
The Company has confirmed that all targets are fully permitted, removing a key execution risk from the near-term exploration timeline.
The Investment Case for FIN Resources
FIN Resources is building a case for a large-scale, high-grade, structurally controlled gold system in one of Canada's most established mining jurisdictions. The key pillars of the investment thesis are as follows.
1. High-grade gold from near surface
The combination of 12.0 g/t Au over 26.2 metres starting at less than 15 metres depth is genuinely exceptional for an early-stage exploration project. Near-surface high-grade mineralisation is rare and carries significant optionality value.
2. A coherent, non-nuggety system
The internal grade consistency throughout CL-26-001 — confirmed by multiple samples above 10 g/t across a broad interval — indicates a systematic sulphide-hosted deposit rather than an erratic occurrence. This is a positive indicator for geological predictability.
3. Scale potential across 15 kilometres
With three active prospects and eight fully permitted targets along a 15 km mineralised corridor, the project has meaningful exploration upside beyond what has been drilled to date.
4. Proven geological address
The Slave Province of Canada's Northwest Territories has a documented endowment of more than 14 million ounces of historical gold production. The Bugow Iron Formation hosts the same geological style as the Lupin Gold Mine (3.3 Moz at >10 g/t Au), providing a credible geological analogue at project scale.
5. Active engagement with Traditional Owners
FIN has established access agreements and an active Winter Access Road Agreement with the Tłı̨chǫ Government, supporting operational continuity and responsible exploration.
6. Multiple near-term results pending
With eight holes completed and results pending across three prospects, the coming weeks represent a concentrated period of potential news flow that could materially advance the market's understanding of the system's scale and grade.
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Why Investors Should Keep Watching FIN Resources
The first drillhole of FIN's 2026 campaign has done what many opening holes fail to do — it has returned a result that materially advances the geological understanding of the project whilst simultaneously raising the stakes for what the rest of the programme might deliver.
A broad, near-surface, high-grade intercept in hole one is a strong opening statement. However, the real question — one that the next seven sets of results will begin to answer — is how far the system extends laterally and at depth across a 15 kilometre mineralised corridor in a jurisdiction with proven gold endowment.
The FIN Resources Cabin Lake gold drilling results in Canada confirm a genuine high-grade gold system with its very first hole of 2026, returning 26.2 metres at 12.0 g/t Au from near surface. With seven additional sets of results pending across three separate prospects, a fully permitted 15 km target corridor, and an integrated geophysics programme sharpening the drill bit for future campaigns, FIN is entering a period of concentrated exploration news flow that warrants close investor attention.
Ready to Follow One of the Most Compelling Early-Stage Gold Stories on the ASX?
FIN Resources (ASX: FIN) has opened its 2026 drilling campaign at Cabin Lake with a genuinely standout result — 26.2 metres at 12.0 g/t Au from just 14.88 metres depth — and with seven additional sets of assay results still pending across three prospects, the most significant news flow may still be ahead. With a fully permitted 15 kilometre target corridor, a proven geological address in Canada's Northwest Territories, and an integrated geophysics programme sharpening future drill targets, this is an exploration story that warrants a closer look. Visit finresources.com.au to access the latest announcements, project information, and investor materials directly from the company.
