Modified: 14.08.2009
Roninlampi - Gold Database
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| Name | Roninlampi | DATA UPDATED | 24.5.2007 | |||
| Alternative names | Pahasuo 2 | |||||
| Deposit summary | RONINLAMPI, in the southern part of the Kuhmo greenstone belt, is an Archaean orogenic gold occurrence with no resource estimate available. It comprises auriferous quartz and quartz-carbonate veins in mafic volcanic rock. The controlling structure may be a NW-trending branch of the main shear zone of the greenstone belt. | |||||
| LOCATION | ||||||
| Geological domain | Archaean | Belt | Kuhmo | |||
| Site photo | Regional map |
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| Map sheet | 441301 | |||||
| Northing (kkj) | 7109500 | Easting (kkj) | 4466800 | |||
| Latitude | 64.08381N | Longitude | 29.31613E | |||
| Municipality | Kuhmo | |||||
| Nearest town, roads | 17 km W from Kuhmo. Three km to a sealed road, gravel road to the area. | |||||
| MINING | ||||||
| Exploration licence no | 7468/2 | Mining concession no | ||||
| Present holder | Geological Survey of Finland (GTK) (2001–) | |||||
| Previous holders | ||||||
| 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 @ 3.62 ppm, 2 m @ 1.35 ppm, 1 m @ 1.88 ppm Au [1,3]. | |||||
| EXPLORATION | ||||||
| Discovery year | 2001 | |||||
| Discovery | By GTK [1,3]: First indication were Au-anomalies in till detected in regional geochemical exploration campaign in 1990's: Auriferous glacial erratics and outrcops were detected during regional exploration in 2001–2002. | |||||
| Exploration history | GTK (1990's, 2001–2003) [1,2,3]: bedrock mapping, low-altitude airborne magnetic, electric and radiometric survey, regional and local till geochemical survey, diamond drilling. | |||||
| Section figure 1 |
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Plan figure 1 | ||||
| Section figure 2 |
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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 | GTK (2003): seven diamond-drill holes, total 495 m [1,3]. | |||||
| Elements analysed | ICP–AES and GFAAS analyses [3]. | |||||
| Primary dispersion | ||||||
| Secondary dispersion | ||||||
| Primary anomaly fig 1 |
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Secondary anomaly fig 1 |
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| Primary anomaly fig 2 |
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Secondary anomaly fig 2 |
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| 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: Aimo Hartikainen | |||||
| ORE | ||||||
| Siting of gold | ||||||
| Fineness | ||||||
| Major opaques | Pyrrhotite, arsenopyrite [1]. | |||||
| Minor opaques | Stibnite, chalcopyrite galena, sphalerite, gold [1]. | |||||
| Gangue | Quartz, tourmaline, scheelite, carbonate [1]. | |||||
| 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 | ||||||
| Ore composition table 1 | Click here | Ore composition table 2 | ||||
| Enriched elements | As, Au, B, CO2, Pb, S, Sb, Te, W, Zn [3]. | |||||
| Ore fluid | ||||||
| Stable isotopes | ||||||
| Pb isotope data | ||||||
| GEOLOGY | ||||||
| Geological setting | The local bedrock is dominated by mica schist and metavolcanic rocks. These are in the southern part of the Late-Archaean Kuhmo Greenstone Belt, in a sequence dominated by mica schists, phyllites, chert, BIF and mafic tholeiitic metavolcanic rocks, in the Ontojärvi synform [1,2,3]. | |||||
| Major host rocks | Mafic metavolcanic rock [1]. | |||||
| Minor host rocks | Mica schist [1]. | |||||
| Intrusives | The hosting sequence is intruded by Palaeoproterozoic, 2.2-2.1 Ga wehritic dykes [1]. | |||||
| Regional geol map 1 |
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Outcrop photo 1 |
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| Regional geol map 2 | Outcrop photo 2 |
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| Local geology map 1 |
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Outcrop photo 3 | ||||
| Local geology map 2 | ||||||
| METAMORPHISM | ||||||
| Metamorphic history | ||||||
| Metamorphic grade | ||||||
| Metamorphic mineral assemblage | Mica schist: quartz-K feldspar-plagioclase-biotite-±garnet
[1].
Mafic metavolcanic rock: plagioclase-hornblende ± garnet [1]. |
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| Metamorph photo 1 | Metamorph photo 2 | |||||
| STRUCTURE | ||||||
| Structural style | ||||||
| Closest major shear | ||||||
| Controlling structure | ||||||
| Deformation history | At least, six deformation stages during the late Archaean and two deformation stages during the Palaeoproterozoic detected in the area; gold mineralisation is related to the Archaean late D3 and/or D4 stages; D2: 2850–2837 Ma, D3: 2701–2697 Ma, D4: peaked at 2657±32 Ma; age of D2 is probably 2820±15 Ma [2] or 2843±18 Ma [4]. | |||||
| Ore fabric | ||||||
| Veins | Auriferous quartz and quartz-carbonate veins 0.5 cm to 2 m thick, and post-mineralisation white quartz veins [1,3]. | |||||
| Structure photo 1 | Vein photo 1 | |||||
| Structure photo 2 | 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 | ||||||
| GENETIC TYPE | Orogenic | References | [1] | |||
| Alternative genetic type 1 | References | |||||
| Alternative genetic type 2 | References | |||||
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References 1. Hartikainen, A. & Pietikäinen, K. & Niskanen, M. 2004. Tutkimustyöselostus Kuhmon kaupungin länsipuolella sijaitsevien valtausten Pahasuo 1 ja 2 (kaivosrekisterinumerot 7468/1 ja 7486/1) alueilla tehdyistä kultatutkimuksista. English summary: A research report of studies concerning the claims Pahasuo 1 and 2 (register numbers of the claims 7468/1 and 7486/1), located 15 km west of Kuhmo, eastern Finland. Geol. Surv. Finland, Report M06/4413/2004/1/10. 16 p. (1.8 MB)2. Luukkonen, E., Halkoaho, T., Hartikainen, A., Heino, T., Niskanen, M., Pietikäinen, K. & Tenhola, M. 2002. Itä-Suomen arkeeiset alueet –hankkeen (12201 ja 210 5000) toiminta vuosina 1992–2001 Suomussalmen, Hyrynsalmen, Kuhmon, Nurmeksen, Rautavaaran, Valtimon, Lieksan, Ilomantsin, Kiihtelysvaaran, Enon, Kontiolahden, Tohmajärven ja Tuupovaaran alueella. Geol. Surv. Finland, Report M19/4513/2002/1. 265 p. (in Finnish, 130 MB) 3. Pietikäinen, K., Halkoaho, T., Hartikainen, A., Niskanen, M. & Tenhola, M. 2005. Itä-Suomen arkeeiset alueet II-hankkeen (2105000) toiminta vuosina 2001–2004 Kuhmon, Nurmeksen, Lieksan ja Hyrynsalmen alueilla. Geol. Surv. Finland, Report M 19/4411/2005/1. 84 p. (in Finnish, 23 MB) 4. Sorjonen-Ward, P. & Luukkonen, E.J. 2005. Archean rocks. In: Precambrian Geology of Finland - Key to the Evolution of The Fennoscandian Shield. Elsevier Science B.V., Amsterdam, 19-99. |
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