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Colorado School of Mines. Arthur Lakes Library

Characterization of the mineralized albitite bodies at Biggejavri, Kautokeino Greenstone Belt, Finnmark, Northern Norway

Abstract

dc:description.abstract

The Kautokeino Greenstone Belt in Finnmark, Northern Norway is host to the Biggejavri U-REE occurrence and the Bidjovagge Cu-Au deposit. The Biggejavri U-REE occurrence is hosted in albitite lenses within the amphibolite unit of the Suoluvuopmi Formation whereas the Bidjovagge Cu-Au deposit is hosted in shear structures crosscutting albitite lenses in the amphibolite of the Časkejas Formation in the west. Both Biggejavri and Bidjovagge occur in the same stratigraphic sequence, comprised of amphibolites, mica and graphitic schists, metadolerites and albitite lenses, with the high Mg amphibolite only occurring at Biggejavri. The Biggejavri U-REE occurrence is unique in its mineralogy with the predominant ore mineral being davidite-loveringite ((La,Ce,Ca)(Y,U)(Ti,Fe3+)20O38-(Ca,Ce)(Ti,Fe3+,Cr,Mg)21O38). The aim of this study is to better understand the formation of the complex mineralogy observed in the Biggejavri area. Amphibole from all units of the Biggejavri U-REE occurrence as well as the Bidjovagge Cu-Au deposit were analyzed using FE-SEM, automated mineralogy, EPMA, and LA-ICP-MS. Trace elements such as Ni and Cr are highest in amphibole in the high Mg amphibolite from the Biggejavri U-REE occurrence, whereas trace elements such as Ti and V are highest in amphibole from the albitite lenses. Biggejavri displays a unique co-location of mafic high Mg rocks and highly evolved felsic rocks. While trace element analysis of amphibole indicates that the high Mg amphibolite, formerly a komatiite, is highly enriched in elements such as Ni and Cr, the felsic albitite lenses within the high Mg amphibolite show enrichment in elements such as Ti, V, and REEs. During metamorphism, the aforementioned elements were released into the metamorphic fluid and formed rare minerals of the davidite-lovingerite solid solution series ((La,Ce,Ca)(Y,U)(Ti,Fe3+)20O38-(Ca,Ce)(Ti,Fe3+,Cr,Mg)21O38).

Degree

thesis:*
Name thesis:degree_name
Master of Science (M.S.)
Level thesis:degree_level
Masters
Discipline thesis:degree_discipline
Geology and Geological Engineering
Grantor dc:publisher
Colorado School of Mines. Arthur Lakes Library
Year dc:date.issued
2019

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Fisher, Lyndsey N.
Advisor dc:contributor.advisor
  • Pfaff, Katharina
Committee members dc:contributor.committeemember
  • Wendlandt, Richard F.
  • Gysi, Alexander

Subjects

dc:subject × 6

Rights

dc:rights
Statement dc:rights
  • Copyright of the original work is retained by the author.
Language dc:language.iso
eng, English

Identifiers

dc:identifier.*
Identifier
T 8835
OAI identifier oai:identifier
oai:repository.mines.edu:11124/173977

Chain of custody

source
Harvested from
Colorado School of Mines
Base URL
repository.mines.edu/server/oai/request
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
citation

Fisher, Lyndsey N.. Characterization of the mineralized albitite bodies at Biggejavri, Kautokeino Greenstone Belt, Finnmark, Northern Norway. Masters thesis, Colorado School of Mines. Arthur Lakes Library, 2019. https://hdl.handle.net/11124/173977