Litchfield Minerals Reframes Harts Range as a Copper-Nickel District

Litchfield Minerals Reframes Harts Range as a Belt-Scale Copper-Nickel District

BHP Xplor-backed research has led Litchfield Minerals Ltd (ASX: LMS) to reclassify the Harts Range in the Northern Territory from a group of isolated copper and nickel prospects into a district-scale copper-nickel mineral system. The Litchfield Minerals Harts Range copper nickel discovery reflects a significant shift in how the belt is understood, with the work suggesting it has the geological ingredients that may support large copper and nickel sulphide deposits, including potential tier-one style systems.

The research has also highlighted a key deep conductive feature, C2, that sits directly beneath known nickel-copper-platinum group element (Ni-Cu-PGE) prospects and is only visible in higher-resolution geophysical data. This has direct implications for how Litchfield Minerals Ltd plans its next phase of geophysics and target generation across its extensive Harts Range holdings.

Managing Director Matt Pustahya commented: "The input from BHP Xplor has fundamentally changed the way we see Harts Range. While Oonagalabi remains a key focus of our exploration efforts, our understanding of the region has evolved significantly. We are now viewing Oonagalabi within the context of a broader district-scale mineral system characterised by deep conductive architecture, long-lived mantle-tapping structures, repeated mafic and ultramafic magmatism with known sulphide mineralisation associated with major crustal pathways."

He further added: "The single most important lesson is C2: a deep conductor tied to known nickel-copper-PGE mineralisation. C2 provides a compelling proof point for our exploration model, demonstrating a direct link between deep conductive architecture and known sulphide mineralisation."

From Isolated Prospects to a District-Scale Mineral System

Historically, Harts Range was assessed as a set of separate copper and nickel-related deposits and prospects. However, according to Litchfield Minerals Ltd, the BHP Xplor-supported work has shifted that view by integrating:

• Magnetotelluric (MT) and seismic reflection data (Vox Geophysics)
• Gravity and magnetic datasets
• Structural interpretations (PGN Geoscience)
• Isotopic data from specialist studies (Dr Michael Green)
• Regional tectonic and geological mapping

This integrated analysis now maps key parts of the system from deep mantle source through to known sulphide occurrences. Furthermore, the company reports evidence of:

• Multiple episodes of mafic and ultramafic magmatism across the Irindina and Aileron provinces
• Long-lived, mantle-tapping crustal structures capable of transporting metals to the upper crust
• Existing copper and nickel sulphide mineralisation in the wider district, such as Blackadder and Baldrick (not on Litchfield tenements)
• A clear spatial association between known prospects and deep conductive features in MT and seismic datasets

According to Litchfield Minerals Ltd, this work supports a single, belt-scale mineral systems model that can be applied across its Harts Range tenure to generate and prioritise exploration targets.

The Four-Gate Mineral Systems Framework

Working within the BHP Xplor framework, Litchfield Minerals Ltd has assessed Harts Range against four critical "gates" that control whether large mineral deposits can form. In the announcement, the company states that each gate has returned a positive outcome.

According to the company, this framework provides a repeatable exploration model that can be extended across the 2 granted exploration licences and 19 applications that make up Litchfield Minerals Ltd's Harts Range position.

C2: The Key Deep Conductor Identified Under BHP Xplor

The most prominent individual result from the BHP Xplor-supported technical work is the C2 conductor, identified on reprocessed data from Geoscience Australia's 09GA-GA1 MT and seismic reflection line.

Litchfield Minerals Ltd reports that:

• C2 is a strong conductor of approximately 10 ohm-metres, located at around 10 km depth
• It lies along the basal fault of the Irindina Province
• It sits directly beneath the Blackadder and Baldrick Ni-Cu-PGE prospects, which are hosted in the sulphide-bearing Lloyd Gabbro
• It is linked via structures, including the Delny Shear Zone, toward the Hammer Hill area, where anomalous nickel, chromium and cobalt have been reported in rock chips

This configuration suggests a plausible deep pathway connecting mantle-level conductive bodies with known surface and near-surface mineral occurrences.

Crucially, C2 is:

• Clearly resolved in the 2009 MT dataset at 10 km station spacing along the 09GA-GA1 line
• Not resolved in the broader AusLAMP dataset, which has 50 km station spacing

This resolution difference is important for investors and technical readers. It demonstrates that deposit-scale features like C2 may not appear in coarse regional datasets, even when they sit directly beneath known mineralisation.

What Is Magnetotellurics and Why Does It Matter?

Magnetotellurics in Simple Terms

Magnetotellurics (MT) is a geophysical method that measures natural variations in the Earth's electric and magnetic fields at the surface. From these measurements, geophysicists calculate the electrical resistivity of rocks at depth:

• High resistivity: rocks that poorly conduct electricity (for example, many crystalline rocks)
• Low resistivity (conductors): rocks or zones that conduct electricity well, which may contain sulphides, salty fluids, graphite, or certain clay-rich or altered rocks

MT is particularly useful because it can image structures deep into the crust and upper mantle, well beyond the depth of drilling.

Why MT Is Relevant for Copper and Nickel Exploration

In the context of copper and nickel exploration:

• Metal sulphide minerals (such as chalcopyrite, pentlandite) are electrically conductive
• Zones containing sulphide accumulations, saline fluids, or graphite may appear as conductors in MT models
• MT can therefore highlight deep conductive zones associated with magmatic bodies, fluid pathways or alteration systems that might not be visible at surface

However, a conductor is not proof of mineralisation. Conductivity can be caused by several materials, so MT is primarily used to map architecture (faults, shear zones, intrusions) and highlight targets where conductive zones correlate with favourable geology, structures and other datasets such as gravity and magnetics.

According to Litchfield Minerals Ltd, joint inversion of MT with gravity is particularly important for features like C2 to help discriminate whether the conductor is more likely related to sulphides or graphite.

Why Does Station Spacing Matter?

The spacing between MT stations controls how fine the resulting image can be:

• 50 km spacing (AusLAMP) — designed for lithosphere-scale imaging across the continent, good for very large features, but too coarse to consistently resolve deposit-scale anomalies in the upper crust
• 10 km spacing (09GA-GA1 line) — provides better resolution along a single profile, revealing C2 at about 10 km depth, which does not appear in the 50 km AusLAMP model
• 1 km spacing (planned survey by Litchfield Minerals Ltd) — aimed at resolving upper crustal conductors at depths of up to ~5 km, intended to provide the detail required to define and rank drill-ready targets

For exploration investors, the key point is that higher-resolution MT surveys can identify targets that broader regional datasets miss, which is central to Litchfield Minerals Ltd's current program.

Glossary of Key Terms

Next Phase: Two 50 km MT and Gravity Lines Over Harts Range

On the back of the C2 result and the mineral systems work, Litchfield Minerals Ltd is commencing a new MT and gravity survey program designed to detect additional C2-style conductors across its Harts Range portfolio.

According to the announcement:

• Two ~50 km MT lines will be acquired
• MT stations will be spaced at 1 km intervals
• Gravity stations will be spaced at 500 m intervals
• Additional off-profile stations will be collected in an irregular grid to improve coverage

Both lines will cross the boundary between the Aileron and Irindina provinces, targeting the full structural architecture. One line will pass through the Oonagalabi project, while the other will lie about 20 km to the east.

The Northern Territory Geological Survey has awarded $100,000 co-funding toward the Oonagalabi MT survey under Round 19 of the GDC program, consequently reducing the direct cost of this next phase of data acquisition.

Survey Objectives and Planned Workflow

The stated objectives of the MT and gravity program are to:

1. Identify additional C2-style conductors over Oonagalabi and the western tenement package at depths up to approximately 5 km
2. Use concurrent gravity data to detect dense bodies that may represent mafic-ultramafic intrusions
3. Prioritise anomalies where strong conductors coincide with gravity highs, as these may represent the most prospective sulphide targets
4. Build a ranked pipeline of targets for follow-up geophysics and drilling

The planned exploration sequence is summarised as follows:

Investment Context: Why This Reframing Matters

For investors focusing on ASX-listed explorers, the Harts Range update from Litchfield Minerals Ltd carries several themes that may be relevant to valuation and risk assessment.

From Single Prospects to Belt-Scale Opportunity

The shift in thinking from individual deposits to a district-scale mineral system changes how the Harts Range tenure may be viewed. In particular:

• The belt now appears to contain the full mineral systems pathway, from fertile mantle source to known sulphide occurrences
• Litchfield Minerals Ltd controls 2 granted exploration licences and 19 applications in the area, giving broad exposure to this interpreted system
• The mineral systems framework is repeatable, allowing consistent ranking of targets across the land position

This can be relevant for investors who distinguish between single-asset prospect risk and multi-target belt-scale exposure.

Existing Mineralisation in the Wider District

Although not on Litchfield Minerals Ltd tenements, historical work across the broader Harts Range and Irindina Province provides proof-of-concept that the system can concentrate metals. For instance:

• Blackadder and Baldrick (magmatic Ni-Cu-PGE in the Lloyd Gabbro) returned rock chips up to 3.8% Ni, 9.6% Cu and 1.7 g/t PGE at Blackadder and up to 2.3% Ni and 2.4% Cu at Baldrick, with drilling at Baldrick reporting 9 m at 0.48% Cu and 0.37% Cu from 4 m (Mithril Resources, 2009)
• The Basil copper-cobalt deposit (hydrothermal Cu-Co, not on Litchfield ground) has an inferred Mineral Resource reported by Mithril Resources in 2012 of 26.5 Mt at 0.57% Cu and 0.05% Co at a 0.3% Cu cut-off

These examples suggest that both orthomagmatic Ni-Cu-PGE and hydrothermal Cu-Co styles of mineralisation are present within the broader architecture that Litchfield Minerals Ltd is now assessing.

Underexplored Covered Areas

Litchfield Minerals Ltd notes that much historical exploration in Harts Range has focused on outcropping areas where mineralisation is visible at surface. The company's current thesis is that some of the most prospective targets may lie beneath shallow cover, where earlier surface-focused explorers generated limited or no anomalies.

The proposed MT and gravity work is specifically designed to look below this cover and image conductors and dense bodies that may represent concealed sulphide systems. For investors, this represents both risk (targets are conceptual and not yet drilled) and potential upside (covered belts can host large undiscovered deposits).

Why Investors May Keep Litchfield Minerals Ltd on Watch

According to the ASX announcement, the Litchfield Minerals Harts Range copper nickel discovery narrative is evolving from conceptual mineral systems work into a more targeted, data-intensive exploration phase. Key factors that may interest investors include:

• Technically supported model — the mineral system has been evaluated across source, generation, migration and concentration, with positive indications at each gate
• C2 as a validation point — a deep conductor is now directly associated with known Ni-Cu-PGE prospects, supporting the conceptual model that deep conductive architecture can be tied to surface mineralisation
• High-resolution survey catalysts — the planned 1 km-spaced MT and 500 m-spaced gravity lines represent clear upcoming data catalysts that may materially influence target generation

Ready to Learn More About Litchfield Minerals' Harts Range Copper-Nickel Opportunity?

With BHP Xplor-backed research reshaping Harts Range into a district-scale copper-nickel mineral system, and a high-resolution MT and gravity survey now underway, Litchfield Minerals Ltd (ASX: LMS) is entering a data-rich exploration phase with multiple upcoming catalysts. Investors looking to understand the full scope of the company's Harts Range position, its exploration model, and its pathway to drill-ready targets can visit the official Litchfield Minerals website at www.litchfieldminerals.com.au for the latest company news, announcements, and project updates.