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The Kiviniemi mafic intrusion, near the eastern margin of the Paleoproterozoic Central Finland Granitoid Complex, is both spatially and temporally associated with post-kinematic Fe-Ti-P-enriched Svecofennian orogenic mafic magmatism. The main rock ty
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::062db281a906216567ea9165225648a0
http://hdl.handle.net/10138/320837
http://hdl.handle.net/10138/320837
