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Exploration Update
Conquistador Exploration Update
26 May 2008
Exploration Update - Conquistador & Earaheedy Projects
Exploration update reporting on follow up drilling and ground EM surveys at the Conquistador zinc project and the completion of a detailed aeromagnetic survey at the key Earaheedy project.
18 September 2007
Conquistador Project - High Grade Zinc Intersection
A new zone of zinc mineralisation intersected 140m grid south from previous drilling.
14 August 2007

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21 April 2008
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11 March 2008

Earaheedy

Zinc Co's 100% owned Earaheedy zinc project covers much of the southwestern margin of the mid Proterozoic Earaheedy Basin in Western Australia, and includes most of the known zones of carbonate-hosted lead-zinc mineralisation in the area. Broadly spaced drilling has defined several prospects containing oxidised and primary Zn-Pb mineralisation (zinc dominant), most of which are confined to a single, laterally continuous dolomite horizon over 30 kilometres strike.  These discoveries, together with the discovery of dolomite-hosted lead oxide reserves at the operating Magellan mine in outliers of the Earaheedy Basin near Wiluna, suggest a  potential major new base metals district.

The Earaheedy Basin has, on its southern and western margins, a recently recognised platform carbonate succession of approximately 500 metres total thickness (Yelma Formation).  Zinc dominant base metals mineralisation, dominantly sphalerite with some galena, is hosted by the laminar stromatolitic Navajoh Dolomite sub-unit.  In some drill-hole intersections the entire width (up to 98m) of this sub-unit is mineralised.  The basin is cut by a number of major long-lived fault zones, particularly the Mt Lockeridge Fault, that are spatially related to the carbonate hosted base metals mineralisation, and may also be prospective 'feeder' structures for sedex style mineralisation within the shale-dominated upper stratigraphic units.

Location and Geology of the Earaheedy Project Area

Location and Geology of the Earaheedy Project Area

                         First pass reverse circulation drilling has been completed at 5-10km spacing and infill diamond and RC drilling of a few established prospects has been completed down to an approximate 1km x 1km pattern (about one third of these drill-holes have failed to test the Navajoh Dolomite adequately due to poor siting or drilling difficulties).  The established prospects held by Zinc Co at 'Navajoh', 'Magazine' and 'Chinook' typically have drill-hole intersections of the order of >50m @ >0.5% Zn+Pb, with higher grade intervals including ‘Navajoh’, an intersection of 7.3m @ 6.12%Zn, 0.77%Pb  (including 3.3 metres @ 11.2% zinc, and 0.93% lead) is untested for 500 metres to 1 kilometre in all directions.  A step out hole located 1.1 kilometres to the north-east returned 6m @ 3.9%Zn, 0.39%Pb, 2.5ppmAg, and a further 16m @ 1.0%Zn, 0.12%Pb.  At ‘Magazine’ there are no follow up holes within a 1 kilometre radius of a discovery intersection of 11m @ 2.66%Zn, 0.84%Pb, 4.4 ppm Ag  (including 2 metres @ 8.2% zinc and 2.8% lead). At ‘Chinook’  intersections including 6 metres @ 3.63% lead +zinc, and 1metre @ 6.18% zinc+lead have been returned.

                              

                              Earaheedy Project Drill Section


Better drill intersections from the three established prospects are shown below;
 Hole  Prospect  East  North  From (m)  To (m)  Intersection
 TDH4  Navajoh
 264466
 7158215
 150.2
 157.5
 7.3m@6.12%Zn, 0.77%Pb
       incl.
 150.2
 153.5
 3.3m@11.2%Zn, 0.93%Pb
 TDH14
 Chinook
 252886
 7166840
 222.5
 231.5
 9m@3.54%Zn, 0.58%Pb,
 2.3ppm Ag
 TRC47
 Magazine
 262263
 71589796
 103
 114
 11m@2.66%Zn, 0.84%Pb,
 4.4ppm Ag
       incl.
 103
 105
 2m@8.23%Zn, 2.77%Pb,
 6ppm Ag
 TRC70  Chinook
 253471
 7164813  126
 131
 5m@2.52%Zn, 1.02%Pb,
 6.8ppm Ag
 TDH20
 Navajoh
 265616
 7158831
 210.5
 216.5
 6m@3.9%Zn, 0.39%Pb,
 2.5ppm Ag
       and
 225
 241
 16m@1.0%Zn, 0.12%Pb

Significant further drilling is required to define resources at each prospect. Drilling between prospects is sparse and there is potential for significant further discoveries, particularly considering that structural controls on mineralisation are not well established.