Bioarchaeological analysis illustrates the life of a 16th-century Sámi individual from Kitka, Kuusamo, northern Finland. [PDF]
Peltola S +13 more
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Metagenomic analysis of the biofilm community at the oxic-anoxic interface of a deep-underground saline spring at the Baksan Neutrino Observatory. [PDF]
Tarasov K +4 more
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Deep subsurface rock-hosted chemolithotrophic bacterial communities exhibited differential CO<sub>2</sub> assimilation and bioconversion potential under varying oxygen level. [PDF]
Saha PK +4 more
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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. [PDF]
Posarić L +5 more
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Reconstructing the historical decline of lichen cover across the reindeer fence of the Finnish-Norwegian border. [PDF]
Wallenius T +8 more
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The constant oxidation state of Earth's mantle since the Hadean. [PDF]
Zhang F +6 more
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Toxigenic Cyanobacteria and Microcystins in a Large Northern Oligotrophic Lake Onego, Russia. [PDF]
Tekanova E +6 more
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Mobility and community at Mesolithic Lake Onega, Karelia, north-west Russia: insights from strontium isotope analysis. [PDF]
Eckelmann R +10 more
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The Fennoscandian Shield encompasses roughly the northern half of Sweden, all of Finland, and the westernmost part of European Russia, ranging in northern latitudes between 60 and 70 degrees, and intersecting the Arctic Circle.
Christer Nilsson +3 more
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Related searches:
Metallogeny of gold in the Fennoscandian Shield
Mineralium Deposita, 1990Gold occurs in a number of different ore types in the Fennoscandian Shield ranging in age from Late Archean to Late Proterozoic. Until recently, the metal was exploited primarily as a byproduct in volcanogenic massive sulphide deposits but during the 1980s more gold mines have been opened than during any other episode in the mining history of northern ...
G. Gaál, K. Sundblad
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