Orbost drilling update - Oroya Mining Limited
Orbost drilling update - Oroya Mining Limited
Orbost drilling update - Oroya Mining Limited
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ABN 16 009 146 794<br />
24 April 2013<br />
Company Announcements Office<br />
Australian Securities Exchange<br />
<strong>Orbost</strong> <strong>drilling</strong> <strong>update</strong><br />
• Three holes completed on western flank of Sunday Creek<br />
• Results indicate main copper prospectivity is on eastern and northern flank<br />
• Anomalous copper and molybdenum highlight potential of Pinnak anomaly<br />
<strong>Oroya</strong> <strong>Mining</strong> Ltd (ASX:ORO) has concluded <strong>drilling</strong> in the second phase of exploration on<br />
its <strong>Orbost</strong> porphyry copper project.<br />
Three holes, for a total of 273m, have tested the potential for shallow copper deposits at<br />
Sunday Creek, west of the original discovery holes. SC 306 was drilled to 126.3 metres<br />
toward the centre of the HeliTEM anomaly when <strong>drilling</strong> was stopped short of the target by<br />
excessive water loss.<br />
All holes intersected highly altered, pyritic granite under thin thermally metamorphosed<br />
sediments (hornfel), confirming that the HeliTEM anomaly was a response to strong<br />
mineralisation in the granites. Assaying is underway, and, as previously announced, the<br />
upper section of SC306 had low copper grades. Full results will be released when the<br />
assays are received. Holes SC307 and SC308 had sodic alteration with pyrite and hole<br />
SC306 intersected strongly pyritic sericite-chlorite alteration to the end of hole. This<br />
zonation is encouraging and potassic alteration with copper would be expected toward the<br />
centre in a classic porphyry system.<br />
Historic hole SC302, on the eastern side, intersected potassic alteration and higher copper<br />
values. Testing of the centre of the anomaly and postulated breccia pipe therefore remains<br />
a priority. It will require <strong>drilling</strong> from a location near the creek, which will entail preparation of<br />
a cultural heritage management plan. Additionally, exploration has not yet identified a<br />
breccia pipe or source for the wide spread anomalous copper in the eastern section of the<br />
Sunday Creek anomaly, although there are deep HeliTEM anomalies that might be caused<br />
by such a feature. These will be objectives for another <strong>drilling</strong> round because they correlate<br />
with high copper in the geochemical surveys. Environmental and cultural heritage surveys<br />
will need to be commissioned to fully test this prospective area.<br />
Soil and rock chip geochemical results from the area of the anomalies have been<br />
reassessed with the drill results. This indicates that copper content in the soil and rock chips<br />
is a good guide to the prospectivity for copper in the area. The findings support the<br />
extension of geochemical surveys to cover the untested HeliTEM anomalies to determine<br />
which are most prospective for copper prior to the next round of <strong>drilling</strong>. These anomalies<br />
are the major western zone of Sunday Creek and Sardine Creek.<br />
Suite 502, 140 Bourke Street, Melbourne, VIC 3000, Australia Ph: (03) 90777987<br />
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The Pinnak anomaly is now a high priority target because previous geochemical surveys<br />
have shown the Pinnak area to be highly anomalous. Rock chip sampling returned values<br />
of up to 0.2% Cu, 0.6% Pb, 0.1% Mo and 0.8 ppm gold from scattered quartz stockwork<br />
veins. Soil geochemistry found anomalous copper and molybdenum in the aureole around a<br />
granitic core (figure 1). Importantly, these results coincide with the southern part of the<br />
Pinnak HeliTEM anomaly, surveyed in 2012 (figure 2). Based on the Sunday Creek results,<br />
the HeliTEM is likely to be caused by strong pyritic mineralisation. The zonation of the<br />
geochemistry with EM results is very encouraging.<br />
The picture that is emerging from the exploration is consistent with the porphyry copper<br />
model derived from major granite intrusion. The <strong>Orbost</strong> results show zonation of<br />
mineralogy, including higher pyritic areas and potassic or chlorite-sericite alterations. It is<br />
encouraging that the HeliTEM is detecting areas of strong mineralisation, which can<br />
become the focus for geochemical follow-up to guide the next round of drill tests.<br />
Figure 1. Pinnak Prospect showing anomalous copper soil geochemistry with offset anomalous molybdenum values and<br />
a broad Pb-Zn halo across the metamorphic aureole of the Feltis Farm Granite (Tonalite). Source: McHaffie, I.W. & Radojkovic, A.,<br />
2001. Synthesis and evaluation of east Victorian soil and drainage geochemistry. Victorian Initiative for Minerals & Petroleum Report 73. Department of<br />
Natural Resources and Environment.<br />
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Figure 2. HeliTEM anomalies on <strong>Oroya</strong>'s <strong>Orbost</strong> tenements.<br />
ENDS<br />
For Further information please contact<br />
Dr Kevin Moriarty<br />
Chairman<br />
<strong>Oroya</strong> <strong>Mining</strong> <strong>Limited</strong><br />
+61 408 173 157<br />
kevinm@oroya.com.au<br />
DECLARATION OF COMPETENCY<br />
The information in this report that relates to Exploration Targets and Exploration Results is based on information compiled by Dr<br />
Kevin Moriarty, a Competent Person who is a Member of The Australasian Institute of <strong>Mining</strong> and Metallurgy. Dr Moriarty has<br />
sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity<br />
being undertaken to qualify as a Competent Person as defined in the 2004 Edition of the ‘Australasian Code for Reporting of<br />
Exploration Results, Mineral Resources and Ore Reserves’. Dr Moriarty is a consultant geologist and Chairman of <strong>Oroya</strong> <strong>Mining</strong><br />
<strong>Limited</strong>. Dr Moriarty consents to the inclusion in the report of the matters based on his information in the form and context in<br />
which it appears.<br />
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