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Smart Science for Exploration and Mining

Location of Rocklands project area on the nose of the northeast plunging Duck Creek Anticline, Quamby-Malbon Zone, Eastern Succession, Mt Isa Inlier. Faults and major units shown.
Rocklands Copper-Cobalt-Gold Deposits, Cloncurry: Geology and Mineralisation.
September 2, 2017
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December 10, 2017

Smart Science for Exploration and Mining

Proceedings of the 10th Biennial SGA Meeting of The Society for Geology Applied to Mineral Deposits Townsville Australia 17th – 20th August 2009

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Edited by P.J. Williams et al. James Cook University Townsville, Australia

Volume 1

Geology and Mineralisation of the Rocklands CopperCobalt-Gold Deposits, Cloncurry District, North West Queensland, Australia

Simon D. Beams Terra Search Pty Ltd :(Consultant Geologist to Cudeco Limited). PO Box 981 Castletown, Hyde Park, Qld, Australia, 4812.

Abstract. The Rocklands deposits represent a significant near surface discovery in the outcropping portion of the Proterozoic Mt Isa Inlier. Several linear copper, cobalt, gold lodes are present which are currently receiving extensive geological evaluation. The general geological setting and style of mineralisation is described. The deposits are structurally controlled occurring in linear, dilatant mineralized channel ways. There is a close association with steeply dipping dolerite dykes which cut, at a high angle, the shallow dipping predominantly siliciclastic host metasedimentary sequence. Infill of both vein material and hydrothermal breccia occur, together with slivers of apparently in situ shattered and altered wall rock. In the primary zone, the moderate to high temperature mineral assemblage consists of chalcopyrite, pyrite, magnetite, actinolite, calcite, quartz, biotite, with minor cobalt sulphides. Leaching, deep oxidation and supergene enrichment of copper has resulted in some very high grade zones with spectacular development of native copper and chalcocite accompanied by higher gold grades.

Keywords: Copper, Cobalt, Gold, Native Copper, Supergene, Dilatant Structures, Hydrothermal Breccia, IOCG

1 Introduction

In April, 2006, Cudeco Directors Wayne McCrae and the late Tim Koitka made a major discovery of copper mineralization in their solely owned Rocklands tenement, 15 km west of Cloncurry. This discovery, by non geologists, of significant outcropping mineralisation in the “mature exploration terrain” of the Eastern Succession of the Proterozoic Mt Isa Inlier, north west Queensland challenges the current accepted wisdom that new discoveries will only be made using sophisticated technology under cover.

Since the Rocklands discovery, Cudeco have built up an extensive geological data set with surface mapping and an intensive drilling program which in March 2009 is in the order of 900 plus holes, 124000 metres of reverse circulation percussion and 18000 metres of diamond drill core. Other data sets include ground and airborne magnetics, radiometrics, SAM (Sub audio magnetics), IP, and soil and bedrock drilling geochemistry. This paper reports the current geological understanding of the Rocklands copper-cobalt-gold deposits.

Figure 1. Location of Rocklands project area on the nose of the northeast plunging Duck Creek Anticline, Quamby-Malbon Zone, Eastern Succession, Mt Isa Inlier. Faults and major units shown. Source: Taylor Wall et al (2000).

2 Geological Setting

Mineralization at Rocklands is hosted in a series of sub parallel, east south east trending, linear zones. The mineralised lodes occur within a metamorphosed sedimentary sequence of siltstone, sandstone/quartzite, quartz magnetite/jaspilite lenses, calcareous beds and calc silicates of Proterozoic age. The lower siliciclastic dominated sequence has been assigned to the Mitakoodi Quartzite with the jaspilite and enclosing units assigned to the Overhang Jaspilite. These stratigraphic units occur within the nose of the Duck Creek Anticline; a major fold structure which south of the project area has a crosslimb width of 40km (Figure 1). The general attitude of the metasedimentary sequence is an east south east strike with shallow dip and younging to the north east.

Figure 2. Simplified surface geology, drilling and main mineralised zones at Rocklands.

Medium grained, intrusive dolerite of Proterozoic age is very prominent in the area. Although several styles of intrusive dolerite bodies may be present, the majority are steeply dipping, cross-cutting, linear and dyke-like. In general, mineralization follows the same structures as the dolerite dykes and cross cuts both dolerite and the intruded sedimentary sequence. Shallow surficial cover, of Recent or Tertiary age colluvium and alluvium, partially obscure some of the basement outcrop (Figure 2). In general, depth of weathering in unmineralised areas is a shallow 15 to 20 metres.

3 Mineralisation Description

3.1 Primary mineralisation

Primary chalcopyrite-pyrite mineralisation occurs within steeply dipping, through-going, west northwest trending, linear, structures that cut the shallow dipping metasedimentary sequence at a high angle (Figure 3). The structures represent mineralised channel-ways or “plumbing systems” containing a host of lithologies, including vein material and hydrothermal breccias, together with slivers of apparently in situ shattered and altered wall rock.

Thin, scattered planar veins and alteration selvedges, filled with red (probably albitic) feldspar and pyritechalcopyrite cut the sedimentary and dolerite wall rocks peripheral to the main structures.

Observations made during logging of drill holes at Rocklands have led to the interpretation of an evolving sequence of paragenesis and breccia textures within the mineralised structures. Hydrothermal fluid was pumped into pre-existing structures which are typically occupied by dolerite dykes, and caused hydraulic fracturing of impermeable lithologies such as siltstone and dolerite wall rock. Continued fluid flow into the structure resulted in jigsaw type breccias, with little evidence of rotation, which were then replaced by milled matrix supported breccias with rounded clasts. The paragenetic mineralogical sequence began with wall rock blocks mantled by secondary biotite, followed by infill of actinolite and magnetite, commonly in a typical “crackle” or jigsaw breccia. Continued hydrothermal development resulted in infill calcite, pyrite, chalcopyrite, magnetite and quartz. Some breccias are clearly polymict, clast supported with little matrix. There is a possibility that these polymict breccias have arisen from leaching of carbonate from the structure and subsequent collapse. Coarse unbrecciated sparry calcite appears to have been a late infill vein phase.

Primary copper mineralization is evident as coarse splashes of irregular chalcopyrite with coarse well formed pyrite, particularly associated with calcite, quartz, actinolite, magnetite vein and breccia infill. Total sulphide content is variable, generally in the range from 1% to 10%, however thin (1m-5m) massive zones are presentwith greater than 50% chalcopyrite-pyrite.

Alteration associated with the mineralization is a moderate to high temperature assemblage of biotite, actinolitic amphibole, red feldspar (probably both potassium feldspar and albite), magnetite, calcite, and quartz. Other minerals noted include minor garnet, fluorite and rare molybdenite.

Cobalt assays within the mineralized drill intersections are generally in the order of 500ppm to 1800 ppm, occasionally up to 0.5% Co. Although, visible primary silver-metallic cobalt sulphides (probably cobaltite) are present, particularly in brecciated siltstone, the bulk of the cobalt mineralization would appear to be associated with fine grained cobalt minerals with pyrite.

Gold grade of the primary mineralisation is generally in the 0.2g/t to 0.5 g/t Au range.

Figure 3. Las Minerale cross section 11400E looking grid west. Simplified geology and drilling. Intersections in Table 1.

3.2 Oxide and supergene mineralisation

Oxidation of sulphidic mineralized structures at Las Minerale and Rocklands South/Double Oxide generated acid fluids which resulted in leaching, deep oxidation and supergene enrichment of copper. Surface outcrops over the main lodes are sparse and dominantly siliceous breccia. Oxide copper minerals cuprite and malachite occur as minor patches and fracture fillings at or just below the surface.

Within the oxidized zone, copper has been leached from near surface areas and re-deposited as coarse nuggets of native copper. Copper carried in solution to below the base of oxidation, replaced existing chalcopyrite and pyrite with chalcocite. This leaching and reprecipitation is responsible for some of the spectacular high copper grades. Oxidation at Las Minerale has been observed at vertical depths in excess of 100m (Figure 4).

Figure 4. Las Minerale cross section 11300E looking grid west. Simplified geology and drilling. Intersections in Table 2

Coarse nuggets of native copper are particularly associated with the oxidized versions of quartz rich breccia characterized by abundant supergene green clay. The close spatial relationship between polymict breccia, native copper development and base of oxidation further supports the surficial, carbonate-leach, collapse origin for the polymict breccia. Native copper occurs as fracture fillings often coating iron-rich rocks such as dolerite blocks and lumps of magnetite. Fluctuations in water table depth and oxidation levels have resulted in a complex relationship between native copper and chalcocite. Zones of strong chalcocite development can occur well above the base of oxidation and often have undergone subsequent partial oxidation.

Cobalt assays within the oxide zone are similar to the primary grade i.e. in the range 500 ppm Co to 1800ppm Co. The nature of the oxide cobalt mineralogy is yet to be determined. High gold assays in the 1 g/t to greater than 10 g/t Au range have been returned from the oxide and supergene zones. This latter gold enrichment has not yet been studied in detail.

4 Surface Geophysical Signature

Surface geophysical methods have been effective in mapping out the mineralised structures at Rocklands. Strong magnetite development has helped close- spaced ground magnetics successfully delineate the lodes. The sulphidic nature of the mineralised structures means that they can be tracked with electrical geophysics. Conductivity trends produced from SAM (Sub Audio Magnetic) surveying proved particularly effective at an early stage in exploration in determining the attitude and trend of the mineralisation (Figure 5).

5 Conclusions and Future Developments

The Rocklands Project area contains several structural/breccia zones with ore grade and thickness copper and significant cobalt, by-product gold. Close spaced drill programs have demonstrated mineralization over strike lengths of hundreds of metres. Drilling through 2007 & 2008 has significantly increased the envelope of mineralization and intersected some spectacularly high “bonanza” copper grades. Extensive drill programs and resource evaluation are actively underway.

The associated primary mineral assemblage of magnetite, actinolite, and red felspar suggests possible iron oxide copper gold (IOCG) affinities. However petrological and ore-fluid studies are required before any concrete conclusions could be made about the genesis of the deposits. In comparison to other IOCG deposits in the region, the structural setting suggests copper mineralization at Rocklands occurs well into the late brittle stage of deformation.

Figure 5. Copper-cobalt zones in relation to conductivity and magnetic trends Rocklands Project.

Acknowledgements

The Cudeco Director’s role in the discovery and hands on guidance of the exploration program is gratefully acknowledged as is the permission of the Cudeco Board to deliver this paper. The assistance of the Rocklands Geological team, Terra Search’s support staff and GIS geologist Rob Lewis is gratefully appreciated.

References

Taylor Wall & Associates, QDME, SRK Consulting Pty Ltd & ESRI Australia, 2000. North-west Queensland Mineral Province Report, Queensland Department of Mines and Energy, Brisbane.