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Korab Resources Uncovers Gallium and Rare Earths at Rum Jungle Near Darwin

BY WILLIAM HADRIAN ON JULY 29, 2026

Korab Resources Ltd

  • ASX Code: KOR
  • Market Cap: $2,936,400
  • Shares On Issue (SOI): 367,050,000

Korab Resources Strikes Gallium and Rare Earths at Rum Jungle Near Darwin

Korab Resources Limited (ASX: KOR) has reported the discovery of gallium oxide, Magnet Rare Earth Oxides (Magnet REO), and Heavy Rare Earth Oxides (HREO) at its Rum Jungle Project in the Northern Territory after re-assaying existing rock chip samples. The results came from 89 rock chip samples collected during earlier outcrop mapping, pointing to a broader critical minerals opportunity across a project area covering 243 square kilometres, located about 70 km south of Darwin.

For investors, the immediate point of interest is scale. Korab said around 24 km of strike length of the relevant geological formations sits within the project boundary, with about 23 km, or 95%, still untested for these newly identified minerals. With a market capitalisation of about $3 million, the announcement gives the market a new exploration angle at a project already known for exposure to multiple commodities.

What Was Found and Where?

In the announcement, Korab said the re-assayed samples were originally collected as part of an outcrop mapping programme focused on nickel and platinum group metals (PGM). The samples came mainly from the Mount Deane Volcanic (MDV) Member and Acacia Gap Quartzite (AGQ) Member within the Wildman Siltstone Formation, as well as the Koolpin Formation and nearby volcanic or doleritic rocks.

The assays were completed by Intertek using four-acid digest followed by ICP Mass Spectrometry and ICP Optical Emission Spectrometry. In simple terms, these are standard laboratory methods used to test rock for a broad suite of elements with high precision.

Rum Jungle sits within the Rum Jungle Mineral Field, part of the Pine Creek Orogen, a geologically complex district with a long exploration and mining history. That matters because complex geological settings can host multiple metals in different rock types, which is consistent with the diversity already reported across the broader Korab project area.

Gallium Oxide Results Show Broad Distribution

Korab said 75 of the 89 samples, or 84%, returned more than 20 ppm gallium oxide (Ga₂O₃). Of those, 25 samples, or 28%, graded above 40 ppm Ga₂O₃. The highest reported result was 72.86 ppm Ga₂O₃.

The best gallium oxide results reported in the announcement included:

Sample ID Ga₂O₃ (ppm) Lithology
128606 72.86 Mount Deane Volcanics
128602 66.27 Mount Deane Volcanics
128918 58.61 Felsic dyke/sill
128605 57.94 Mount Deane Volcanics
128917 55.78 Altered basic volcanic

The concentration of higher-grade gallium results in the Mount Deane Volcanics suggests that unit may be an important host rock. Furthermore, the presence of gallium in felsic and altered volcanic rocks indicates the mineral occurrence is not limited to one narrow rock type.

For early-stage exploration, distribution can be as important as peak grade. A wide spread of anomalous results across a sample set often provides a stronger basis for follow-up work than one isolated standout result.

Magnet REO Results Point to Permanent Magnet Exposure

The announcement defined Magnet REO as the combined oxides of dysprosium, neodymium, praseodymium, and terbium. These are the rare earths most closely associated with high-performance permanent magnets used in electric vehicles, wind turbines, and other electrification technologies.

Korab reported that 60 of 89 samples, or 67%, returned 50 ppm or more Magnet REO, with grades up to 371.46 ppm.

Selected higher-grade Magnet REO results were:

Sample ID Magnet REO (ppm) Lithology
128918 371.46 Felsic dyke/sill
128917 307.32 Altered basic volcanic
110992 272.62 Sheared chlorite rock
110994 254.67 Very weathered basic volcanic
128606 244.42 Mount Deane Volcanics
110993 189.20 Sheared chlorite rock

These results suggest that magnet-related rare earth mineralisation may be present across several lithologies, including felsic intrusions, altered volcanics, and sheared rocks. In exploration terms, that can be important because it broadens the number of geological settings that may warrant follow-up sampling or mapping.

Heavy REO Discovery Adds Another Layer

Heavy rare earths are generally less common than light rare earths and often attract closer market attention because of their specialised industrial uses. Korab reported that 30 of 89 samples, or 33%, returned 50 ppm or more HREO, with a top value of 507.38 ppm HREO.

The leading HREO results included:

Sample ID HREO (ppm) Lithology
128915 507.38 Felsic dyke/sill
128916 203.25 Felsic dyke/sill
128918 159.23 Felsic dyke/sill
111355 110.00 Carbonaceous siltstone
110994 108.82 Very weathered basic volcanic
128954 100.36 Intermediate volcanic

The strongest HREO values appear closely linked to felsic dyke and sill material. That does not establish an economic deposit, but it does help narrow the types of rocks that may be most prospective in future work.

Key results at a glance:

  • Gallium oxide: up to 72.86 ppm, with 84% of samples above 20 ppm
  • Magnet REO: up to 371.46 ppm, with 67% of samples at or above 50 ppm
  • Heavy REO: up to 507.38 ppm, with 33% of samples at or above 50 ppm
  • Untested strike length: about 23 km of a total 24 km

Understanding Gallium and Rare Earths

For non-specialist investors, this announcement is easier to interpret with some commodity context.

Gallium is a minor metal mostly recovered as a by-product from other industrial processes, especially alumina and zinc refining. It is used in semiconductors, power electronics, LEDs, and some solar technologies. Because supply is relatively concentrated, explorers identifying gallium in new geological settings can attract investor interest, although a discovery at rock chip stage is still a long way from a defined commercial source.

Magnet rare earths usually refer to neodymium (Nd), praseodymium (Pr), dysprosium (Dy), and terbium (Tb). These are used in high-strength permanent magnets. Among them, NdPr is particularly important for magnet manufacturing, while Dy and Tb help magnets perform at higher temperatures.

Heavy rare earth oxides (HREO) include the heavier part of the rare earth suite, such as dysprosium, terbium, yttrium, erbium, gadolinium, and others. They are generally harder to find in meaningful concentrations and can be valuable depending on chemistry, metallurgy, and recoverability.

Why Do Rock Chip Results Matter at This Stage?

A rock chip sample is a surface sample taken directly from exposed rock or nearby rock fragments. It is a first-pass exploration tool used to identify whether a target area contains elevated concentrations of the elements being tested.

Rock chip assays are useful because they can highlight where mineralisation reaches surface. However, they do not define a JORC Mineral Resource. They do not show thickness, continuity at depth, mining conditions, or metallurgical recoveries. What they can do is support the case for more detailed work, such as:

  • Additional mapping
  • Systematic soil sampling
  • More rock chip sampling
  • Trenching
  • Drilling

That distinction is important for investors. The current results identify exploration targets, not mineable resources.

A Large Part of the Target Area Remains Untested

One of the more material points in the announcement is how little of the prospective geology has been tested for the newly identified minerals.

Korab said interpreted geology mapping shows about 24 km of strike length of the Wildman Siltstone Formation, including the MDV and AGQ members, and the Koolpin Formation within the project area. Of that, about 23 km remains untested for gallium, Magnet REO, and HREO.

This means the current discovery is based on sampling from only about 5% of the prospective strike length. For investors assessing early-stage explorers, this kind of exploration runway can be relevant, as it suggests the current results are an initial dataset rather than a final picture of project potential.

The fact that these discoveries came from re-assaying archived samples also matters. It indicates Korab may have additional stored samples elsewhere on the project that could be reviewed for the same commodities using the same analytical approach.

Rum Jungle Remains a Multi-Commodity Project

The announcement also confirmed Korab's previously reported scandium discovery at Rum Jungle, a speciality metal used in certain alloys and fuel cell applications. In addition, Korab's broader project inventory across Rum Jungle includes exposure to:

  • Gold and silver
  • Tin, zinc, lead, and copper
  • Nickel and cobalt
  • Scandium and gallium
  • Rare earth oxides
  • Lithium, iron ore, manganese, uranium, and phosphate

That breadth reflects the geological complexity of the district. It can be viewed in two ways by investors. On one hand, multi-commodity exposure can provide optionality if one target type gains traction. On the other, a wide commodity list does not remove the need to identify which targets are large, continuous, and potentially economic.

The exploration results in the ASX announcement were reviewed by Malcolm Castle, MAusIMM, of Agricola Mining Consultants Pty Ltd, who consented to the inclusion of the information in the form and context presented.

What Comes Next?

Korab did not provide a detailed timetable in the announcement, but said the results will form the basis for further exploration programmes, analysis, and reviews. Based on the work described, the likely next steps may include:

  1. More systematic surface sampling along the remaining untested strike
  2. Re-assaying additional archived samples for gallium and rare earths
  3. Geological and structural interpretation to rank the most prospective zones
  4. Drilling if surface work defines targets strong enough to justify subsurface testing

The company also noted that the Rum Jungle area has previously been covered by gravity, magnetic, electromagnetic, TEMPEST, and radiometric surveys by earlier operators and government geological bodies. Those existing datasets may assist target generation as Korab refines where the strongest critical minerals responses occur.

Why ASX Investors May Watch Korab From Here

At a market capitalisation of about $3 million and a last traded share price of 0.8 cents, Korab remains firmly in the micro-cap end of the ASX resources sector. That means market expectations may be relatively modest, but it also means the company is still at an early exploration stage.

The investment relevance from this announcement rests on several points:

  • The discoveries were made from existing samples, which is a comparatively low-cost exploration pathway
  • The mineralisation appears widespread in the sample set, rather than confined to one isolated point
  • About 95% of the interpreted prospective strike length remains untested
  • The project is located relatively close to Darwin, which is relevant from a logistics perspective
  • The findings add a new critical minerals angle to a project already known for multiple commodity targets

That said, the next phase of work will be important. Surface geochemistry can indicate prospectivity, however investors typically look for progression from anomalous sampling to coherent targets and then to drilling evidence.

Korab's announcement has therefore expanded the geological interest at Rum Jungle. The key question now is whether follow-up exploration can demonstrate continuity, scale, and target quality across the much larger untested portion of the project.

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Stock Codes: ASX: KOR

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