2023
DOI: 10.1016/j.lithos.2023.107389
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Trace elements in ilmenite, titanomagnetite and apatite unravel the petrogenesis of Fe-Ti-P-(+/-Zr) rich rocks and associated nelsonite from the Raftsund intrusion, Vesterålen-Lofoten AMCG suite, Northern Norway

Nolwenn Coint,
Eduardo T. Mansur,
Jakob K. Keiding
et al.
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Cited by 2 publications
(1 citation statement)
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“…In this context, the geological setting of Norway displays great potential for the discovery and subsequent exploitation of critical raw materials, especially P-REE resources [4]. Notably, significant Fe-Ti-P-REE resources have been identified in Norway that are related to layered intrusions and alkaline intrusive complexes [5,6], emphasizing the potential for discoveries in diverse settings. The Southern Oslo Rift region is renowned for hosting multiple magmatic occurrences that are rich in Fe-Ti-P-REE, with the Kodal deposit being the largest and most well-known to date [7].…”
Section: Introductionmentioning
confidence: 99%
“…In this context, the geological setting of Norway displays great potential for the discovery and subsequent exploitation of critical raw materials, especially P-REE resources [4]. Notably, significant Fe-Ti-P-REE resources have been identified in Norway that are related to layered intrusions and alkaline intrusive complexes [5,6], emphasizing the potential for discoveries in diverse settings. The Southern Oslo Rift region is renowned for hosting multiple magmatic occurrences that are rich in Fe-Ti-P-REE, with the Kodal deposit being the largest and most well-known to date [7].…”
Section: Introductionmentioning
confidence: 99%