Exploration
targets
Nickel deposits in southern Juva
Several nickel-bearing mafic-ultramafic intrusions occur in southern Juva and surrounding areas. One small deposit was mined during 1970, the Kitula deposit in Puumala.The bedrock is characterized by a granulite facies metamorphism postdating the mafic magmatism. Metamorphism has changed the primary mineralogy and fabric of the intrusive mafic-ultramafic rocks so that they were not identified until the late 1970s. The largest intrusion bodies, later identified and mapped are around four kilometres in length. The nickel deposits of Enonkoski, gold deposits of Rantasalmi and copper deposits of Virtasalmi are found some 40-60 km north of the southern Juva area (Fig. 1).
The NS trending, around 15 km long Pihlajasalo-Heiskalanmäki belt includes four known deposits/showings and boulder indications of additional deposits. The most potential deposits within the belt so far are Pihlajasalo and Heiskalanmäki. From all the deposits, located so far in the southern Juva area the most important one is the Niinimäki deposit, east of the Pihlajasalo-Heiskalanmäki belt (Fig. 2).
Suomen Malmitutkimus Oy has made an application for reservation notification on Pihlajasalo-Heiskalanmäki belt and Niinimäki.
More data: Niinimäki, Pihlajasalo, Heiskalanmäki.
Nickel in eastern Finland
Archaean komatiites occur in eastern Finland, in the Nurmes-Lieksa-Kuhmo region, hosting also nickel deposits like Tainiovaara in Lieksa. Some Ni-rich boulders (glacial erratics) have been found in the past, still without the known bedrock source, pointing out the nickel potential of the area. Another economically interested formation, potential for Ni-Cu-Co and PGEs + Au, is the Kuohatti layered intrusion (located in the SW part of the reservation area in Fig. 3). It was studied with bedrock mapping, lithogeochemistry, geophysics and some drilling by the Geological Survey of Finland during 2000’s and 2010’s.
Suomen Malmitutkimus Oy has made in the area in September 2021 a reservation notification, named Kuohatti-Näätä (Fig. 3).
