J. P. Konnunaho
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
J. P. Konnunaho has a total of 16 co-authors. Here are the top co-authors by number of shared publications:
- Andrey Bekker
Department of Earth and Planetary Sciences, University of California, Riverside, USA
1 shared publication Anne Tuomela
1 shared publication- Anssi Rauhala
University of Oulu
1 shared publication B. A. Wing
Department of Earth and Planetary Sciences and GEOTOP, McGill University, Montréal, Canada
1 shared publicationE. Hanski
University of Oulu
1 shared publicationE. J. Hanski
Department of Geosciences, University of Oulu, Oulu, Finland
1 shared publication
Latest Publications
- Open Access
- 13 March 2026
- Published by Copernicus GmbH
Assessment of Graphite Potential in the Siikalatva Area, Central Finland
Critical and strategic raw materials have emerged as a focal point of global interest and are increasingly embedded in geopolitical competition among major powers. The European Union (EU) has been identified as reliant on external suppliers for these minerals and has undertaken a range of measures to mitigate this dependency.As part of this initiative, Siikalatva graphite as a raw material for the green transition project has been launched in Central-Finland by the municipality of Siikalatva, the University of Oulu, and the Geological Survey of Finland (GTK). The project is funded by the EU’s Just Transition Fund (JTF) for 2024–2026, with the objective of mitigating the adverse impacts associated with the transition to a low-carbon economy. The project aims to achieve this goal by supporting the regions and employees most affected by the transition and by promoting a balanced socioeconomic transformation.The main goal of this project is to investigate the flake graphite potential in a small municipality (Siikalatva) in Central Finland. Flake graphite is, after all, a critical raw material e.g., in battery production. Flake graphite occurs in a Paleoproterozoic metasedimentary environment that has undergone high-grade metamorphism, which increases the size of the graphite flakes. Graphite exhibits strong geophysical conductivity and is frequently associated with iron sulfides, including pyrrhotite and pyrite.In this presentation, we will examine the geophysical research opportunities offered by the GTK’s geophysical and geological data sets for assessing graphite potential in the municipality of Siikalatva. This also serves as a good example of the possibilities and long-term usefulness of geodata for various purposes.By processing geophysical data from a high-grade metamorphic area, we can delineate graphite-rich zones and further classify them into sulfide-poor and sulfide-rich types. These zones can then be presented as potential areas and integrated with other land-use planning, existing infrastructure, settlements, and tourism. Similarly, integrating this information with, for example, groundwater resource data provides valuable insights for the potential utilization of flake graphite.This study provides the municipality of Siikalatva an opportunity to assess the perspectives and potential that the graphite in its area may offer. At the same time, it supports land-use planning and decision-making. The results of the project will be published in the final report in 2026.
- 13 March 2026
- Published by Copernicus GmbH
Open AccessAssessment of Graphite Potential in the Siikalatva Area, Central Finland
Critical and strategic raw materials have emerged as a focal point of global interest and are increasingly embedded in geopolitical competition among major powers. The European Union (EU) has been identified as reliant on external suppliers for these minerals and has undertaken a range of measures to mitigate this dependency.As part of this initiative, Siikalatva graphite as a raw material for the green transition project has been launched in Central-Finland by the municipality of Siikalatva, the University of Oulu, and the Geological Survey of Finland (GTK). The project is funded by the EU’s Just Transition Fund (JTF) for 2024–2026, with the objective of mitigating the adverse impacts associated with the transition to a low-carbon economy. The project aims to achieve this goal by supporting the regions and employees most affected by the transition and by promoting a balanced socioeconomic transformation.The main goal of this project is to investigate the flake graphite potential in a small municipality (Siikalatva) in Central Finland. Flake graphite is, after all, a critical raw material e.g., in battery production. Flake graphite occurs in a Paleoproterozoic metasedimentary environment that has undergone high-grade metamorphism, which increases the size of the graphite flakes. Graphite exhibits strong geophysical conductivity and is frequently associated with iron sulfides, including pyrrhotite and pyrite.In this presentation, we will examine the geophysical research opportunities offered by the GTK’s geophysical and geological data sets for assessing graphite potential in the municipality of Siikalatva. This also serves as a good example of the possibilities and long-term usefulness of geodata for various purposes.By processing geophysical data from a high-grade metamorphic area, we can delineate graphite-rich zones and further classify them into sulfide-poor and sulfide-rich types. These zones can then be presented as potential areas and integrated with other land-use planning, existing infrastructure, settlements, and tourism. Similarly, integrating this information with, for example, groundwater resource data provides valuable insights for the potential utilization of flake graphite.This study provides the municipality of Siikalatva an opportunity to assess the perspectives and potential that the graphite in its area may offer. At the same time, it supports land-use planning and decision-making. The results of the project will be published in the final report in 2026.
- Open Access
- 1 June 2018
- Published by The Geological Society of Finland in Bulletin of the Geological Society of Finland
- Vol. 90 (1) , 109-136
The petrology and genesis of the Paleoproterozoic mafic intrusion-hosted Co-Cu-Ni deposit at Hietakero, NW Finnish Lapland
- 1 June 2018
- Published by The Geological Society of Finland in Bulletin of the Geological Society of Finland
- Vol. 90 (1) , 109-136
Open AccessThe petrology and genesis of the Paleoproterozoic mafic intrusion-hosted Co-Cu-Ni deposit at Hietakero, NW Finnish Lapland
- 1 October 2015
- Published by Springer Nature in Mineralium Deposita
- Vol. 51 (3) , 411-430
The Paleoproterozoic komatiite-hosted PGE mineralization at Lomalampi, Central Lapland Greenstone Belt, northern Finland
- 1 October 2015
- Published by Springer Nature in Mineralium Deposita
- Vol. 51 (3) , 411-430
The Paleoproterozoic komatiite-hosted PGE mineralization at Lomalampi, Central Lapland Greenstone Belt, northern Finland
- 24 April 2013
- Published by Springer Nature in Mineralium Deposita
- Vol. 48 (8) , 967-989
The Archean komatiite-hosted, PGE-bearing Ni–Cu sulfide deposit at Vaara, eastern Finland: evidence for assimilation of external sulfur and post-depositional desulfurization
- 24 April 2013
- Published by Springer Nature in Mineralium Deposita
- Vol. 48 (8) , 967-989
The Archean komatiite-hosted, PGE-bearing Ni–Cu sulfide deposit at Vaara, eastern Finland: evidence for assimilation of external sulfur and post-depositional desulfurization