Piippumäki graphite occurrence, Pertunmaa, South Savo, Finlandi
Regional Level Types | |
---|---|
Piippumäki graphite occurrence | Occurrence |
Pertunmaa | Municipality |
South Savo | Region |
Finland | Country |
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Latitude & Longitude (WGS84):
61° 27' 56'' North , 26° 25' 54'' East
Latitude & Longitude (decimal):
Locality type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Pertunmaa | 2,089 (2014) | 4.7km |
Mäntyharju | 6,871 (2014) | 24.6km |
Hartola | 3,676 (2014) | 25.6km |
Hirvensalmi | 2,517 (2014) | 27.0km |
Joutsa | 4,060 (2014) | 34.1km |
High-quality graphite occurrence that was indicated by an airborne electromagnetic anomaly (approx. 0.5 × 1 km in size), and subsequently was located during fieldwork by electromagnetic measurements.
The flake graphite is hosted by Paleoproterozoic quartz-feldspar gneiss and amphibolite that have been subjected to retrograde metamorphism (granulite facies regressing to greenschist facies). Equilibration conditions are calculated at ca 5 kbar and 740 °C.
Located about 50 km from Mikkeli.
Note: coordinates fairly approximate.
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Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
ⓘ Graphite Formula: C Reference: Palosaari, J., Latonen, RM., Smått, JH., Raunio, S., Eklund, O. (2020): The flake graphite prospect of Piippumäki—an example of a high-quality graphite occurrence in a retrograde metamorphic terrain in Finland. Mineralium Deposita 55, 1647-1660. https://doi.org/10.1007/s00126-020-00971-z |
Gallery:
References
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Year (asc) Year (desc) Author (A-Z) Author (Z-A)Palosaari, J., Latonen, RM., Smått, JH., Raunio, S., Eklund, O. (2020): The flake graphite prospect of Piippumäki—an example of a high-quality graphite occurrence in a retrograde metamorphic terrain in Finland. Mineralium Deposita 55, 1647-1660. https://doi.org/10.1007/s00126-020-00971-z
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