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Thermal history of impact melt rocks in the Fennoscandian shield

Contributions to Mineralogy and Petrology, 1975
Shock-melted rocks from the Fennoscandian shield commonly contain fragments of quartz which appear to represent paramorphs of quartz after lechatelierite and, therefore indicate very high melt temperatures, at or above 1700 °C.
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The origin of the Paleoproterozoic belt (northeastern Fennoscandian Shield). Reply

Canadian Journal of Earth Sciences, 1998
I thank Dr. V. Melezhik and Dr. B. Sturt for their comments on my paper published in the Canadian Journal of Earth Sciences (Smolkin 1997). I am ready to continue constructive discussion on the questions of the genesis of Paleoproterozoic magmatic complexes of the Kola region (northwestern Russia) that host sulfide, chromite, and titanomagnetite ore ...
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Proterozoic Processes in the Fennoscandian Shield

GFF, 2005
Olav Eklund   +2 more
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The Fennoscandian Shield

2009
Christer Nilsson   +3 more
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Past and Present Biofilm Formation in Deep Fennoscandian Shield Groundwater

2003
Intra-terrestrial life has been found at kilometre depths in deep subseafloor sediments and in the basement crust beneath the sediments, up to 2800 m deep in continental sedimentary rocks, in igneous rock aquifers down to 3500 m and in fluid inclusions in ancient salt deposits from salt mines (Pedersen 2000). The biomass of these organisms may be equal
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A flexible electron-blocking interfacial shield for dendrite-free solid lithium metal batteries

Nature Communications, 2021
Hanyu Huo, Ning Zhao, Dongxing Zhang
exaly  

Fennoscandian Shield

1984
S. Rudberg, A. A. Aseev
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Metagenomics studies of deep terrestrial biosphere of Fennoscandian Shield

2014
Molecular microbial studies of several deep boreholes ranging from 300 to 2500 m reveal considerable diversity of bacteria, archaea, fungi and viruses in the Fennoscandian Shield. The cell counts decrease with depth even if the temperatures at 2.5 km are only around 40 oC.
Itävaara, Merja   +12 more
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