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Gold deposits in northern Finland - Arkisto.gsf.fi

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Figure 22. Dark graphitic shear<br />

zone host<strong>in</strong>g the ore on right, pale<br />

grey ma<strong>fi</strong>c volcanic rock on left.<br />

Ma<strong>in</strong> open pit at the Kittilä M<strong>in</strong>e.<br />

View to the north. Photo courtesy<br />

Agnico Eagle M<strong>in</strong>es.<br />

A<br />

N<br />

B<br />

N<br />

C<br />

N<br />

N=8<br />

N=78<br />

N<br />

D<br />

N=52 N=14<br />

Figure 23. These stereoplots<br />

show the orientations of deformation<br />

features observed<br />

for Suurikuusikko (ordered<br />

from oldest to youngest).<br />

A. Bedd<strong>in</strong>g (dots), the trend of<br />

the typical regional foliation<br />

(l<strong>in</strong>es) formed prior to movements<br />

of the KiSZ related to<br />

m<strong>in</strong>eralisation, and fold axes<br />

measured <strong>in</strong> the deposit area<br />

(stars). B. C. Orientation of<br />

the ‘graphitic’ shear zones associated<br />

with the KFZ and ore<br />

zones. D. Common orientation<br />

of post-m<strong>in</strong>eralisation faults.<br />

Lower hemisphere projections<br />

on equal area nets. Plots after<br />

Patison (2001) and Patison et<br />

al. (2006).<br />

38 Pasi Eilu & Tero Niiranen (ed.)

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