Management Team

Gold, Silver and Base Metals

Historic Mines

SMA – Historic Mines Legend

Historic Mining in the Upper Mosquito Creek Silver-Lead-Zinc Province

Numerous old mines lie within a province known as Upper Mosquito Creek silver province. The map above shows the broad distribution of old mines in this province. For Silver-Lead-Zinc these mines may be grouped into three main clusters from west to east: New Moon group, Argent King group and Southern Cross group. The Southern Cross group mines have been mapped and sampled in detail and are now “drill ready for resource definition”.

Silver production appears to have commenced in 1906 at the Orion mine and extended until approximately 1930 with a second period of mining around 1947 – 52. The target mineral was galena (lead) in high grade veins. Silver values were presented in terms of ounces/ton of lead. Old records indicate that the converted grades for silver ranged from 6.8Kg/tonne lead produced for the New Moon group, 0.83Kg/t for the Argent King group, 2.5 – 3.95 Kg/t for the Orion – Southern Cross group. One estimate (CR 17255) suggests over 19 tonnes of silver has been recovered from small mines in this Province.

Recorded production from Leowalds shaft includes ¬16,500oz silver and 317 tonnes lead during the period 1912 – 1919; sporadic re-processing of surface 2nd and 3rd grade waste stockpiles produced a further 2,200Oz silver and 37tonnes lead during the period 1920 – 1949.

In the period prior to World War I ore was handpicked and carted a long distance to Chillagoe for treatment. This smelter closed at the start of the war so many mines in the Georgetown area were then closed. Little attention was paid to the extent of mineralization; either at depth or laterally to known veins. Detailed field mapping and core drilling is almost non-existent in the region. The deepest shaft appears to be 56 metres (Leowalds) with most mines terminated at the water table around 25 metres depth. Subsequent exploration has been cursory in nature.

 

Southern Cross mine (EPM 25726 – 100% SMA)

The table below shows assays of gossan samples taken earlier from the Southern Cross silver-lead-zinc mine dumps. As expected from historical production these gossans record a mineral lode that is rich in silver, lead and zinc. Assays show enrichment in tantalum also. This was unexpected. Minor gold is also reported in several samples. It is noted for both tables that samples are “seconds” taken from dumps. All high-grade ore was hand sorted and despatched by the miners for processing so these assays are indicative only.

The very unusual association of silver and tantalum is found in the Southern Cross and Orion mines. Petrological studies have revealed three periods of mineralisation have occurred. First was sphalerite (zinc) mineralisation, followed and partially replaced by galena (lead), silver and tantalum. The final phase of mineralisation saw gold-bearing pyrite with minor copper introduced. It is important to note that the zinc and lead credits are significant for this mine.

 

Southern Cross Mine Gossan Assays.

Sample # Nb2O5 (ppm) Ta2O5    (ppm) Ag         (ppm) Au           (ppm) CuO       (ppm) ZnO      (%) As2O3   (ppm) PbO      (%)
1285 320 790 913 0.482 5450 9.6240 0 27.9510
810 160 710 36 0.090 330 16.5290 470 0.8860
1664 620 520 622 0.121 2450 46.3160 <10 28.7500
1385 180 480 168 0.15 540 10.2010 0 11.3060
100 240 320 307 0.205 920 6.8200 4020 11.1250
1667 640 270 442 0.57 1930 13.8470 1310 25.2220
1384 0 230 10 0.02 290 10.4970 120 0.4060
1666 470 170 619 2.731 930 5.4080 40210 23.6770
Average 329 436

390

= 12.6 oz/tonne

0.546 1605 14.905 5766 16.164

 SMA has identified the Southern Cross – Leowalds line of lode as a priority target for evaluation. The line of lode is shown on the satellite image below. Note the main road passes close by in the southeast corner of the figure. A powerline follows this road.

Micro-XRF Geochemistry and Mineralogy Report

 

Portable Spectral Services Pty Ltd in Perth analysed 3 gossan samples from the Southern Cross dump. The principal mineralogy identified consisted of galena (lead), quartz, sphalerite (zinc), manganese oxide and zinc oxide. Minor minerals included chalcopyrite (copper), pyrite (usually carries gold) and ankerite (a carbonate associated with mineralising systems). 

An important finding from this study was that silver occurs as a separate mineral phase hosted within the quartz rather than the galena. As the early miners focussed on extracting the highly visible galena lead ore the implication is that silver mineralisation may be more extensive and of higher grade than in the ore mined. 

 

Orion Mine (EPM 18490 – 95% SMA Mining)

 SMA also sampled gossans from the Orion mine that lies ~ 1.5 km due west of the Southern Cross – Leowalds line of load and appears to be on the same regional structure. This structure extends an estimated 10 kms further to the east of Leowalds. SMA now has this ground under application (EPM 27551).

The results below are from gossans taken on the old dumps around the Orion mine shaft. The Orion mine was reported as averaging ~ 46 ozs Ag/tonne in lead ore. Again, it is important to note that the zinc and lead credits are significant for this mine.

 

Table 2.4: Orion Mine Gossan Assays.

Sample # Nb2O5 (ppm) Ta2O5    (ppm) Ag         (ppm) Au           (ppm) CuO       (ppm) ZnO      (%) As2O3   (ppm) PbO      (%)
RC1795 <10 90 8 0.031 300 11.275 70 0.255
RC1796 160 120 137 0.048 410 12.129 2050 10.488
RC1797 30 230 20 0.056 700 21.477 780 1.245
RC1798 <10 120 176 0.050 3700 9.489 470 1.240
RC1799 30 80 452 0.156 2690 5.178 1090 2.057
Average 44 128 159 0.068 1560 11.91 892 3.057

 

Silver Resource Evaluation

Southern Cross Lode (EPM 25726)

 SMA has completed detailed mapping and geochemical sub soil sampling on the Southern Cross/Leowalds and Orion mines found on EPM’s 18490 and 25726. These mines are formed along linear structures in metasediment host rocks formed by shearing against harder amphibolites. The map below shows the geology of the immediate mine area, geochemical contours for both lead and zinc that outline the surface area of the mineralisation, and the planned drill grid. All sites have been ground proofed.

Orion Lode (EPM 18490)

Surface mapping of the Orion mine area followed the main line of lode further to both the east and west than indicated by surface pitting. The geochemical contouring from 120 sub soil samples showed the zinc anomaly to be widespread and to cover a broader area than previously thought. The area of anomaly for lead is more confined but does highlight the presence of a potential second line of lode along the contact with a unit of slates to the south of the main shaft. Drilling is planned to evaluate the east-west extension of the main lode.