Kangaroo Island project – South Australia

Summary

Lithium Australia NL (‘LIT’) holds two granted exploration licences (‘EL’) on Kangaroo Island (see Figure 1). The Dudley project is the result of LIT’s strategy to continue its Australia-wide search for strong domestic lithium holdings to add to its portfolio of projects.

Figure 1: Kangaroo Island project.

Geology

The Dudley ELs (EL 6212 and EL 6213) lie on the eastern side of Kangaroo Island, 100 kilometres (‘km’) south-southwest of Adelaide, and have a combined area of 90 km2.

At Dudley, the focus is the pegmatite intrusives into the Tapanappa Formation. The pegmatites form dykes and sills of predominately feldspar-quartz-muscovite, with varying amounts of topaz, tourmaline, graphite, citrine, and apatite. They are extensive, with up to a 5 km strike length presenting as discontinuous, partially buried exposures. Although there is mention of lepidolite in a report by the Geological Survey of South Australia, there has been no modern exploration for lithium minerals in the area.

The exploration licences contain the Dudley Mine, which operated during the early 1900s and 1980s. Gem tourmaline, ceramic-grade feldspar, silica, and kaolin for brickmaking were mined.

Exploration

Recent exploration by Lithium Australia identified lithium-anomalous pegmatite dykes at its Dudley prospect at the Kangaroo Island Project.

  • Lithium and tantalum pegmatite dykes identified.
  • Pegmatites cover greater than 5 km strike, with individual dykes up to 80 m thick.
  • Rock-chip samples return assays up to 0.43% Li2O lithium, 770 ppm tantalum, 460 ppm niobium and 1,600 ppm rubidium, despite strong weathering.
  • Tantalum values significant, as grades above 200 ppm considered economic.
  • Lithium minerals include elbaite tourmaline, lithium micas and petalite.

Despite strong weathering of outcrops and exposures in shallow historical tourmaline and tin-mine workings, the host pegmatites exhibit local, anomalous lithium, rubidium and tantalum.

Lithium Australia considers this significant, as lithium, which is very mobile, is usually leached from weathered rocks. The Dudley pegmatites intrude the Cambrian metasediment Tapanappa Formation and are variably exposed at surface. Currently, lithium pegmatites in Australia are attracting investment from some of the world’s largest lithium companies.

All data from this programme indicate that the Dudley prospect has the potential to host a lithium deposit in a location not previously identified for its lithium potential. The following factors indicate the potential to delineate a substantial lithium-caesium-tantalum (LCT) pegmatite system (LCT pegmatites host almost all of the world’s hard-rock lithium mines):

  • strongly anomalous assays (despite strong weathering and kaolinisation);
  • abundant lithium and pathfinder minerals and elements;
  • multiple dykes with widths up to 80 m occurring over a substantial strike, and
  • relatively shallow cover.

In light of these significant results, LIT is planning a geochemical soil-sampling programme over the Dudley prospect and surrounding areas where anomalous lithium values were obtained from pegmatite float. The follow-up work programme at Dudley will commence in the fourth quarter of 2019.