Gold deposits in northern Finland - Arkisto.gsf.fi
Gold deposits in northern Finland - Arkisto.gsf.fi
Gold deposits in northern Finland - Arkisto.gsf.fi
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A<br />
B<br />
C<br />
Figure 27. Two back-scattered electron microprobe<br />
images and one reflected light image of ore samples<br />
<strong>in</strong> ma<strong>fi</strong>c host rocks. A. Nucleation (or recrystallisation)<br />
of arsenopyrite <strong>in</strong> graphitic (black phase) milled zones<br />
relat<strong>in</strong>g to shear<strong>in</strong>g. B. A fractured competent rock<br />
fragment with arsenopyrite associated with fracture<br />
<strong>in</strong><strong>fi</strong>ll. A penetrative shear boundary is seen at the edge<br />
of this m<strong>in</strong>eralised fragment (center of photograph).<br />
C. The host with abundant f<strong>in</strong>e-gra<strong>in</strong>ed auriferous<br />
arsenopyrite-pyrite dissem<strong>in</strong>ation and a late, crosscutt<strong>in</strong>g<br />
quartz-carbonate ve<strong>in</strong>. Field of view <strong>in</strong> A and B<br />
is 1.5 mm, but 4 cm <strong>in</strong> C.<br />
alloys with Ag and Hg (Chernet et al. 2000).<br />
Rare stibnite ve<strong>in</strong>s and amorphous gra<strong>in</strong>s conta<strong>in</strong><br />
extremely high gold grades and overpr<strong>in</strong>t<br />
the ma<strong>in</strong> ore-bear<strong>in</strong>g sulphides.<br />
Acknowledgements<br />
Agnico Eagle is gratefully acknowledged for the<br />
permission to publish the data and all the images.<br />
The <strong>in</strong>formation <strong>in</strong> this summary reflects<br />
the op<strong>in</strong>ions of the authors only, unless otherwise<br />
referenced. The majority of <strong>in</strong>formation is<br />
based on data collected prior to 2005 (dur<strong>in</strong>g<br />
the exploration phase of the deposit preced<strong>in</strong>g<br />
m<strong>in</strong>e development).<br />
Rompas-Rajapalot gold-uranium<br />
project, Peräpohja Schist Belt<br />
Mawson Exploration Team and co-workers<br />
The Rompas-Rajapalot gold-uranium project is<br />
located <strong>in</strong> the Ylitornio municipality of <strong>northern</strong><br />
F<strong>in</strong>land at 66.45 °N and 24.75 °E, approximately<br />
50 km west of the Rovaniemi town. The<br />
<strong>in</strong>itial discovery area, Rompas, was discovered<br />
by AREVA Resources F<strong>in</strong>land Oy <strong>in</strong> September<br />
2008 as part of regional uranium exploration.<br />
Limited exploration was undertaken until<br />
Mawson Resources purchased the exploration<br />
assets of Areva <strong>in</strong> 2010. Mawson subsequently<br />
def<strong>in</strong>ed more than 300 bonanza grade gold<br />
occurrences of ve<strong>in</strong> style m<strong>in</strong>eralisation over a<br />
6 km strike length. Diamond drill<strong>in</strong>g <strong>in</strong> 2012<br />
and early 2013 produced numerous Au-U <strong>in</strong>tersections,<br />
of which 6 metres at 617 g/t Au rema<strong>in</strong>s<br />
the highlight. Rajapalot is a new grassroots discovery<br />
made by Mawson, 8 km east of Rompas,<br />
where a total of 52 outcrop grab samples to date<br />
average 152.8 g/t gold and range from 0.001 g/t<br />
to 2 817 g/t gold.<br />
Mawson holds 833 claims and claim applications<br />
for 75 340 hectares at the Rompas Project.<br />
A total of 110 exploration claims that cover a<br />
surface area of 10 580 hectares and form the core<br />
claims at Rompas came <strong>in</strong>to legal force on Oc<br />
42 Pasi Eilu & Tero Niiranen (ed.)