1996
DOI: 10.1080/11035899609546323
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The Solstad Cu‐Co‐Au mineralization and its relation to post‐Svecofennian regional shear zones in southeastern Sweden

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Cited by 10 publications
(6 citation statements)
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“…Our study area is located on the southern rim of a 100,000 km 2 ore-rich geological region of central Sweden (Stephens et al 2009). Active mining from Solstad Gruva, a copper mine along the shore of Gåsfjärden, started in the 1630s and ended in 1920 (Hermansson 1966;Söderhielm and Sundblad 1996). It is possible that the copper mining started earlier, already by the end of the 15th century, concurrently with the copper mine in the nearby Gladhammar (Hermansson 1966).…”
Section: Figmentioning
confidence: 99%
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“…Our study area is located on the southern rim of a 100,000 km 2 ore-rich geological region of central Sweden (Stephens et al 2009). Active mining from Solstad Gruva, a copper mine along the shore of Gåsfjärden, started in the 1630s and ended in 1920 (Hermansson 1966;Söderhielm and Sundblad 1996). It is possible that the copper mining started earlier, already by the end of the 15th century, concurrently with the copper mine in the nearby Gladhammar (Hermansson 1966).…”
Section: Figmentioning
confidence: 99%
“…Therefore it is likely that the mine acted as a strong local point source of Cu pollution. The principal Cu ore mined at Solstad was chalcopyrite (CuFeS2) (Söderhielm and Sundblad 1996). Thus one likely mechanism of Cu transport to the study site may have been oxidation of chalcopyrite in tailings due to leaching by rainwater, followed by mobilization of Cu through complexation with dissolved organic carbon (DOC) (Lazerte et al 1989).…”
Section: Trace Metal Pollutionmentioning
confidence: 99%
“…Sampling procedure and sites description Västervik Gåsfjärden (57°34.35'N, 16°34.98'E) is a semi-enclosed inlet on the Swedish coast of the Baltic Sea. It has been exposed to varying mining activity from the Solstad copper mine from the 17 th to the early 20 th century (Söderhielm & Sundblad, 1996). We have previously documented detailed sedimentological features of Gåsfjärden and inferred past environmental changes from this data (Ning, Ghosh, et al, 2016;Ning et al, 2018;Ning, Tang, et al, 2016).…”
Section: Methodsmentioning
confidence: 99%
“…5 km 2 ) copper mining polluted inlet in the Baltic Sea, we have previously observed that strains of S. marinoi appear overly tolerant to several metals present in the mining ore (Andersson et al, 2020) and that toxic metal stress can affect interspecific competition between diatoms (Andersson et al, 2022). The mine is located on the shoreline and was active from the 17 th until the early 20 th century (Söderhielm & Sundblad, 1996). The sediment in the inlet is polluted with several metals whose concentrations across depth layers correlate negatively with the abundance of S. marinoi micro-fossils (Ning et al, 2018), suggesting that metal pollution has had an adverse effect on this species.…”
Section: Introductionmentioning
confidence: 99%
“…Individual strains of S. marinoi were germinated and isolated from sediment resting stages using standard micropipetting techniques (Härnström et al 2011). Surface sediment was collected from two semi-enclosed inlets of the brackish Baltic Sea, where one (Gåsfjärden [VG]; 57°34.35'N 16°34.98'E) has been exposed to historical copper mining (Söderhielm and Sundblad 1996) while the other (Gropviken [GP]; 58°19.92'N 16°42.35'E) has not. A total of 69 and 55 strains were isolated from VG and GP, with 88% and 94% survival, respectively.…”
Section: Strain Retrieval and Whole Genome Sequencingmentioning
confidence: 99%