Evidence map›Paper›PMID 40035910›Full record

ArticleEnvironmental geochemistry and health2025

Lithology as a factor for the distribution of metals in stream sediments associated with sediment-hosted Cu deposits: a case study from the Alta-Kvænangen tectonic window, northern Norway.

Laura Posarić, Sabina Strmić Palinkaš, Johan Hilmo, Željka Fiket, Andrea Čobić, Hana Fajković

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Article in Environmental geochemistry and health, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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4 · The record

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5 · Who and what money

Authors and funding

6 authors.

Laura PosarićDepartment of Geology, University of Zagreb Faculty of Science, Horvatovac 102B, 10000, Zagreb, Croatia.ORCID https://orcid.org/0000-0002-9652-5850
Sabina Strmić PalinkašDepartment of Geosciences, UiT-The Arctic University of Norway, Dramsvegen 201, 9037, Tromsø, Norway. sabina.s.palinkas@uit.no.ORCID https://orcid.org/0000-0002-8468-6569
Johan HilmoDepartment of Geosciences, UiT-The Arctic University of Norway, Dramsvegen 201, 9037, Tromsø, Norway.
Željka FiketDivision for Marine and Environmental Research, Ruđer Bošković Institute, Bijenička Cesta 54, 10000, Zagreb, Croatia.ORCID https://orcid.org/0000-0002-7628-9045
Andrea ČobićDepartment of Geology, University of Zagreb Faculty of Science, Horvatovac 102B, 10000, Zagreb, Croatia.ORCID https://orcid.org/0000-0002-3805-0594
Hana FajkovićDepartment of Geology, University of Zagreb Faculty of Science, Horvatovac 102B, 10000, Zagreb, Croatia. hana.fajkovic@geol.pmf.unizg.hr.ORCID https://orcid.org/0000-0003-3901-228X

Funding

Sveučilište u Zagrebu 20286481
6 · The paper itself

Abstract

The Kåfjord area in northern Norway hosts numerous Cu deposits that were subjected to mining activities back in the nineteenth century. Relicts of the historical mining activity are still visible at several abandoned mines and associated mine waste disposal sites that may represent an environmental threat. The area was subjected to mining activities during the nineteenth century and abandoned mines and associated mine waste disposal sites still may represent a significant environmental threat. The Cu mineralization, found within the Paleoproterozoic Alta-Kvænangen Tectonic Window, primarily occurs as epigenetic sulfide-quartz-carbonate hydrothermal veins that crosscut the Kvenvik volcano-sedimentary complex and the overlying Storviknes sedimentary sequence. This study aims to determine the geochemical composition of stream sediments associated with the sediment-hosted Cu deposits and examine the role of host lithologies in the dispersion of elements associated with the deposits. Sediments from two streams and a river in the Kåfjord area were analyzed using phase and element analyses (aqua regia chemistry), complemented by a seven-step sequential extraction procedure. Results from Annaselva stream, draining Cu occurrences in the carbonate sediments of the Storviknes sequence, showed a significant positive correlation of Cu with mobile chalcophile elements (Pb, Zn, Ni, Tl, Hg, Ag, Sb, Bi) and lithophile elements (Sr, Ca, Ba, Al, K). In contrast, Brakkelva stream, draining the mafic volcanics of the Kvenvik complex, exhibited no statistically significant correlations between Cu and any of the analyzed elements. Møllneselva River, draining both lithologies, showed a strong Cu-Sc correlation, with principal component analysis indicating limited distinction between lithology-derived elements. These results did not completely align with statistical analysis outcomes highlighting the challenges of statistical data interpretation using a limited number of samples.

Indexed as

CopperGeologic SedimentsRiversWater Pollutants, ChemicalEnvironmental MonitoringMiningNorwayCopperWater Pollutants, ChemicalPrincipal component analysis (PCA)Sediment-hosted Cu depositsSeven-step sequential extraction analysisSpatial analysisStream and river sedimentsX-ray powder diffraction (XRPD)

Identifiers

PMID40035910
PMCPMC11880057

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