Results 11 to 20 of about 978 (214)
Deep seismic studies in the southeastern Fennoscandian Shield
Геофизический журнал, 2015 The modern concept of the deep structure of the earth crust of the Ladoga-Bothnian zone, based on analysis and summing-up of all available information obtained in the last 35 years, is presented.
N. Sharov
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8: Precambrian geodynamics and ore formation: The Fennoscandian Shield [PDF]
Ore Geology Reviews, 2005 Abstract Compared with present-day global plate tectonics, Archaean and Palaeoproterozoic plate tectonics may have involved faster moving, hotter plates that accumulated less sediment and contained a thinner section of lithospheric mantle. This scenario also fits with the complex geodynamic evolution of the Fennoscandian Shield from 2.06 to 1.78 Ga ...
Pär Weihed +7 more
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The Fennoscandian Shield within Fennoscandia [PDF]
Bulletin of the Geological Society of Finland, 1996 J. Donner
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Taxonomically and functionally diverse microbial communities in deep crystalline rocks of the Fennoscandian shield. [PDF]
ISME J, 2014 Nyyssönen M +7 more
europepmc +3 more sources
Formation mechanism of the Vaasa Batholith in the Fennoscandian shield: Petrographic and geochemical constraints [PDF]
Bulletin of the Geological Society of Finland, 2012 The ~1.88 Ga Vaasa Batholith in western Finland is a large granitoid area (8 000 km2) with gradational contacts against the garnet- and cordierite-bearing diatexite and metatexite migmatites of the Pohjanmaa Belt.
H. Mäkitie +4 more
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Graphite-bearing ore areas of the Fennoscandian Shield
Proceedings of the Karelian Research Centre of the Russian Academy of Sciences, 2022 Владимир Щипцов +1 more
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Box 8–4: Fennoscandian Shield—Rogaland Anorthosite Province
Ore Geology Reviews, 2005 Bernard Charlier
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Seismic model of the Earth's crust and upper mantle beneath the Fennoscandian Shield [PDF]
E3S Web of Conferences, 2023 Well-founded concepts of the crust and upper mantle structure of the Fennoscandian Shield were developed. Quantitative evidence for horizontal and vertical lithospheric heterogeneities was obtained.
Lebedev Artem, Sharov Nikolay
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Precambrian geodynamics and ore formation : the Fennoscandian Shield
, 2006 The complex geodynamic evolution of the Fennoscandian Shield from 2.06 to 1.78 Ga involved rapid accretion of island arcs and several microcontinent-continent collisions in a complex array of orogens. With a few exceptions, all major ore deposits formed in specific tectonic settings between 2.06 and 1.78 Ga and thus a strong geodynamic control on ore ...
Pär Weihed +7 more
openalex +2 more sources