Modified: 14.08.2009

Sudenkylä - Gold Database

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Name Sudenkylä DATA UPDATED 12.1.2007
Alternative names Haudankylä
Deposit summary SUDENKYLÄ (HAUDANKYLÄ), in Southern Ostrobothnia, is a Palaeoproterozoic orogenic gold occurrence with no resource estimate available. It is hosted by mica gneiss, and located between two major NW-trending shear zones.
LOCATION
Geological domain Svecofennian Belt Southern Ostrobothnia
Site photo   Regional map  
Map sheet 222204
Northing (kkj) 6950500 Easting (kkj) 2437100
Latitude 62.65344N Longitude 22.76967E
Municipality Ilmajoki
Nearest town, roads 15 km SW from Seinäjoki. A sealed road 7 km from the mineralisation, a gravel road adjacent to the area.
MINING
Exploration licence no 6136/1 Mining concession no  
Present holder OPEN FOR ACQUISITION
Previous holders Geological Survey of Finland (GTK) (1981–86),
Malmikaivos Oy (1986–), Outokumpu Oyj
Mine photo 1   Mine photo 2  
Mine photo 3   Mine photo 4  
Status of development Prospect
When mined  
Resources  
Deposit size (Mt)   Reference (size)  
Total in-situ gold (kg)   Reference (in-situ Au)  
Total gold production (kg)   Reference (gold prod)  
Production of other metals  
Extent of mineralisation  
Lodes  
Best sections 1 m @ 3.5 ppm Au [3].
EXPLORATION
Discovery year 1986
Discovery By Malmikaivos Oy; the first indication was an aurideforus glacial erratic found by an amateur prospector; the occurrence was found by a follow-up exploration on an Au anomaly in till detected during regional till geochemical survey [3].
Exploration history GTK (1981–86) [2,3]: Regional and localised till geochemical survey, till stratigraphy and bedrock mapping.
Malmikaivos (1986–) [4]: Bedrock mapping, diamond drilling?.
Section figure 1   Plan figure 1  
Section figure 2   Plan figure 2  
Section figure 3   Plan figure 3  
Trench fig 1   Trench fig 4  
Trench fig 2   Trench fig 5  
Trench fig 3   Trench fig 6  
Explor site photo 1   Explor site photo 2  
Geophysical response  
Drilling  
Elements analysed  
Primary dispersion  
Secondary dispersion An Au anomaly 600x600 m in size in till; the regional Sb and As anomalies in till are, apparently, unrelated to gold mineralisation [2,3].
Primary anomaly fig 1   Secondary anomaly fig 1 kalliosalo9_thumb
Primary anomaly fig 2   Secondary anomaly fig 2  
Primary anomaly fig 3   Secondary anomaly fig 3  
Primary anomaly fig 4   Secondary anomaly fig 4  
Primary anomaly fig 5   Secondary anomaly fig 5  
Economic evaluations  
Exploration geologist in charge GTK: Pekka Lestinen; Malmikaivos: Pertti Huopaniemi.
ORE
Siting of gold  
Fineness  
Major opaques Arsenopyrite, pyrrhotite, pyrite(?) [3].
Minor opaques  
Gangue  
Ore miner. photo 1   Ore miner. photo 5  
Ore miner. photo 2   Ore miner. photo 6  
Ore miner. photo 3   Ore outcrop photo 1  
Ore miner. photo 4   Ore outcrop photo 2  
Ore composition Diamond-drill core [1]: 10.80 ppm Au, 0.70 ppm Ag, 30000 ppm As, 3.0 ppm B, 475 ppm Ba, 19.2 ppm Bi, 999 ppm Co, 632 ppm Cu, 210 ppb Hg, <1 ppm Mo, 775 ppm Ni, 5 ppm Pb, 91 ppm Rb, 104000 ppm S, 2.3 ppm Sb, 7.9 ppm Se, 82 ppm Sr, 5.600 ppm Te, 1.8 ppm Th, 1.6 ppm U, 120 ppm V, <0.5 ppm W, 70 ppm Zn; 46.2% SiO2, 0.49% TiO2, 5.56% Al2O3, 31.5% Fe2O3, 2.66% MgO, 2.28% CaO, 1.60% Na2O, 2.76% K2O, 0.039% P2O5, 9.00% LOI.
Enriched elements Au, Ag, As, Bi, Co, Cu, Hg, K, Rb, S, Sb, Se, Te [1].
Ore fluid  
Stable isotopes  
Pb isotope data  
GEOLOGY
Geological setting A sequence of palaeoproterozoic metapelites and metagreywackes intruded by the intermediate plagioclase and plagioclase-uralite porphyry sills(?) [2,3,5].
Major host rocks Mafic metavolcanic rock [1]; mica gneiss [3].
Minor host rocks  
Intrusives  
Regional geol map 1   Outcrop photo 1  
Regional geol map 2   Outcrop photo 2  
Local geology map 1   Outcrop photo 3  
Local geology map 2  
METAMORPHISM
Metamorphic history  
Metamorphic grade  
Metamorphic mineral assemblage  
Metamorph photo 1   Metamorph photo 2  
STRUCTURE
Structural style  
Closest major shear The mineralisation is between two NW-NNW trending, major shear zones [2,3,5].
Controlling structure  
Deformation history  
Ore fabric  
Veins  
Structure photo 1   Vein photo 1  
Structure photo 2   Vein photo 2  
Structure photo 3   Vein photo 3  
ALTERATION
General alteration  
Proximal alteration  
Intermediate alteration  
Distal alteration  
Zonation figure   Prox alteration photo 1  
Alteration photo 1   Prox alteration photo 2  
Alteration photo 2   Intermed alteration photo  
Alteration photo 3   Distal alteration photo 1  
Post-mineralisation modifications  
TIMING  
GENETIC MODEL Orogenic "mesothermal" deposit.
GENETIC TYPE Orogenic, Au-Sb subtype References  
Alternative genetic type 1   References  
Alternative genetic type 2   References  

References

1. Nurmi, P. A., Lestinen, P. & Niskavaara, H. 1991. Geochemical characteristics of mesothermal gold deposits in the Fennoscandian Shield, and a comparison with selected Canadian and Australian deposits. Geol. Surv. Finland, Bull. 351. 101 p.
2. Lestinen, P. 1988. Seinäjoen alueen geokemialliset tutkimukset vuosina 1983–1986. Geol. Surv. Finland, Report S/41/2222/1/1988. 40 p. (in Finnish, 1.4 MB)
3. Lestinen, P., Kontas, E., Niskavaara, H. & Virtasalo, J. 1991. Till geochemistry of gold, arsenic and antimony in the Seinäjoki district, western Finland. Journal of Geochemical Exploration 39, 343–361.
4. Tyni, M. 1983. Lausunto Kalliosalon antimoniesiintymän hyväksikäyttömahdollisuuksista. A letter by Malmikaivos Oy to the Ministry of Trade and Industry. 3 p. (in Finnish)
5. Korsman, K., Koistinen, T., Kohonen, J., Wennerström, M., Ekdahl, E., Honkamo, M., Idman, H. & Pekkala, Y. (eds.) 1997. Suomen Kallioperäkartta = Berggrundskarta över Finland = Bedrock map of Finland 1:1 000 000. Geol. Surv. Finland.
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