Peake Denison
Peake and Denison
Peake and Denison
Principal target is interpreted to be analogous to Ernest Henry and ranks highly in CUS’s selection methodology.
- Located at the northern end of the Peake and Denison Ranges, consisting in part of outcropping Paleoproterozoic rocks showing widespread copper occurrences
- A number of targets identified by recent 3D scans which rank very highly using CUS protocols
- The majority of targets are located east of the Mt Dutton Fault in area of relatively shallow Mesozoic and possible Permian cover
- Target 1 is interpreted to be an Ernest Henry-type analogue, and ranks very highly using CUS methodology
- Priority Targets 14, 16, and 17 are located west of the Mt Dutton Fault, and also rank highly
- Historic rock chip samples collected from T14 and Copper Top West area show significant copper assays
- CUS has confirmed outcropping copper mineralisation at intervals along the Mt Dutton Fault (see below).

Outcropping copper mineralisation Peake and Denison Project


Composite pipe-like body identified, which is estimated to be approximately 350m below surface.
- Peake and Denison area shows regional scale alteration similar to other IOCG provinces such as the Stuart Shelf and Cloncurry district.
- Local copper gold geochemical anomalism seen in rock chip and drill holes seen as good support for working IOCG systems in the northern Peake and Denison area
- Target 1 is a large composite magnetic pipe-like body extending to +3 km depth
- Upper surface of target pipe is approximately 350 metres below surface
- Target 1 is interpreted to be analogous to Ernest Henry style of deposit (magnetite dominant pipe-like IOCG)