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Mongolia - General Mining

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54<br />

5 - Independent Geological Report - Australia<br />

interest were black chlorite schists, limestones and<br />

dolomites. Several quartz-reefs were also noted and<br />

sampled.<br />

Targeted during this visit were the ‘black calcite’<br />

outcrops, which earlier prospecting has found to be<br />

highly anomalous in silver; in particular the ‘black<br />

calcite’ range, which was noted during RW’s 2006<br />

helicopter reconnaissance to persist for over six<br />

kilometres strike length.<br />

The independent geologist was able to follow this<br />

feature on the ground and to sample it over 1,500<br />

m length. He found that it was indeed open in both<br />

the north and the south. He has formed the opinion<br />

that this be the Halls Creek Fault or an associated<br />

structure. Over half the samples were collected<br />

from this 30-50m wide zone which swells up to<br />

over 100m. The NNE-SSW striking feature typically<br />

consists of dark green (‘black’) chlorite schist forming<br />

dark ridges. While the schist consists of large slatelike<br />

plates, it is often tightly folded. Within and to<br />

the west of this prominent schist are a number of<br />

calcite and dolomite lenses and layers. These are of<br />

a few cm to nearly a metre thick. There are many of<br />

these lenses and layers, comprising 10-30% of the<br />

30-50m wide target-zone. They consist of calcite and<br />

dolomite of light to dark (gray) colour, often with<br />

blobs and irregular veins of milky quartz. Malachite<br />

was frequently observed in the carbonate lenses.<br />

Galena was found in one outcrop. Sampling by the<br />

2.5.5 Black Hill Proposed Exploration<br />

and Budget<br />

It is recommended that detailed prospecting,<br />

geological mapping and geochemical sampling<br />

comprise the initial exploration phase. The target zones<br />

can be traced on satellite images and air-photographs,<br />

due to the dark ridges and the specific vegetation<br />

cover as well as the lighter colours of limestone,<br />

dolomite, ankerite and calcrete in the slopes and flats.<br />

independent geologist could not confirm the earlier<br />

silver values obtained from within the ELA area. He<br />

found, however, several copper occurrences, with of<br />

up to 1.3% Cu in rock chip samples. The majority of<br />

samples had also elevated Mn values.<br />

2.5.4 Potential<br />

The stated exploration targets of this project are<br />

silver-bearing carbonate-rich zones and locations of<br />

black calcite.<br />

Black calcite is a common associate of silver/<br />

manganese ores found in the southwestern silver<br />

fields of the USA. This association is reported, among<br />

others, from the Silver District in Arizona (S.B. Keith<br />

1978), from the Western <strong>Mining</strong> Districts of the USA<br />

(Hewett & Radtke 1967), as well as from Sonora,<br />

Mexico (Silvermex 2007).<br />

The Halls Creek Fault Zone hosts a number of<br />

hydrothermal vein type copper occurrences in mafic<br />

Tickalara Metamorphics, immediately to the north of<br />

the ELA, and the hosting structures extend into the<br />

GMM tenement area.<br />

Gold occurrences have been described from the<br />

Eastern Zone of the Lamboo Group (Report 74 of<br />

the GSWA). Since the ELA straddles this zone, its<br />

gold potential should be examined as well.<br />

Proposed Work Yr 1 Yr 2 Total<br />

Road cutting, prospecting, sampling $25,000 $50,000 $75,000<br />

Geophysics $50,000 $50,000<br />

Drilling ten RC holes $90,000 $90,000<br />

Assaying $10,000 $25,000 $35,000<br />

Planning, supervising, reporting $20,000 $50,000 $70,000<br />

Total $105,000 + $215,000 = $ 320,000

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