The style of mineralisation at the historic Razorback Mine is essentially the same as at Renison Mine, located 7km along strike to the north.
The geology of the Razorback Mine is dominated by the Razorback Fault where the Cambrian serpentinite is in faulted contact with the younger Dundas Group Red Lead Conglomerate and Hodge Slate. The Serpentinite has been strongly dolomitized and talc altered within 20-30m of the fault contact. The sequence strikes north-northwest and is near vertically dipping with the fault dip steep east near surface to steep west dipping below 100m depth.
Tin mineralisation is hosted within the talc-carbonate altered serpentinite and the Red Lead Conglomerate where they are adjacent to the Razorback Fault. The mineralised lodes are semi continuous and plunge steeply south within the plane of the fault. Mineralisation consists of semi-massive pyrrhotite with cassiterite, pyrite, arsenopyrite, chalcopyrite, sphalerite and galena.
The lode is wedge shaped with a width of 10-15m at the top (base of pit floor), narrowing to widths of 2-3m at a depth of approximately 100m below the pit floor. The average length of the significant intersections listed in Appendix 1 is 6.4m. The Razorback lode strikes over [200m] and possibly plunges steeply south to over 400m in depth.
Razorback Mine Typical Cross Section 5,363,850mN
Exploration and Mining History
Initial exploration over the Razorback Tin Mine was undertaken from 1958 to 1969 by the Bureau of Mineral Resources and the Tasmanian Mines Department who completed 7 surface diamond drillholes for 528m.
Extensive underground exploration development, 22 underground diamond drillholes (1,009m) and underground bulk sampling was completed over the Razorback Mine by Placer Prospecting Ltd between 1964 and 1966. Placer also completed 16 surface diamond drillholes over the Razorback Mine during this period.
The Razorback Mine was operated as an open pit mine by Minops Pty Ltd from 1975 to 1978 during which time an estimated 180,000 tonnes of ore at ~0.6% Sn was mined and processed by an on-site processing plant and tailings facility.
In 1978 Minops completed a further 7 surface diamond drillholes aimed at locating extensions of the ore to the south of the open cut.
In 1979 a Joint Venture was signed between Minops and CRA Exploration who proceeded to drill 5 deeper surface diamond drillholes over the next few years. In 1982, CRA Exploration decided not to procced further with the project.
In total 35 historic surface diamond drillholes (6,054m) and 22 underground diamond drillholes (1,009m) have been completed over the Razorback Mine between 1958 and 1984.
In 2018, Stellar dug and sampled 3 costeans in the pit floor.
Razorback Mine Long Projection
Razorback Mine Exploration Target
An Exploration Target of 180,000 – 220,000 tonnes @ 0.8 – 1.0% Sn at a cut-off grade of 0.3% Sn has been defined to a depth of 100m below the previously mined Razorback pit floor in accordance with the JORC Code 2012 by technical consultant, Resource and Exploration Geology, in July 2019. There has been no material change to assumptions since the estimate was completed in 2019.
Razorback Mine Exploration Target
It should be noted that this Exploration Target estimate is conceptual in nature. There has been insufficient exploration to define a Mineral Resource in this volume and it is uncertain if further exploration will result in the determination of a Mineral Resource.
Most of the historic drilling, which forms the basis of the Razorback Mine Exploration Target, has only tested mineralisation to a depth of ~150m below the current pit floor. Possible extensions to the Razorback Mine orebody were further identified by CRA Exploration in 1979 after drilling 5 deeper holes. Further drilling of deeper extension targets, such as those identified by CRA Exploration in 1979, have the potential to substantially increase the Razorback Mine Exploration Target.
Razorback Fault and Grand Prize Exploration Potential
There is potential for discovery of further mineralisation along the Razorback Fault over the 7km of strike length between Razorback and Rension and including the Grand Prize Tin deposit, also within Stellar’s Exploration Licence (EL11/201).
The Grand Prize-Razorback Fault structure is a large mineralizing system. Its proximity to the Pine Hill Granite and the Renison Bell Tin Mine make it highly prospective for structural and replacement style tin-copper deposits.
Broad spaced historic exploration of the Grand Prize Fault suggests it is a large mineralizing system, although possibly sub ore grade at this stage. There are ore grade intercepts within the larger low-grade intercepts suggesting there may be some scope for targeting and modelling of higher-grade zones. There is also the possibility of recovering a copper concentrate adding value to the mineralisation. To put it into perspective, the known mineralizing system covers an area twice that of the Severn deposit at Zeehan and remains open down dip.
Razorback – Grand Prize Fault Structure Geological Plan