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Delineation and character of the Archaean-Proterozoic boundary in northern Sweden

Öhlander, Björn (author)
Luleå tekniska universitet,Geovetenskap och miljöteknik
Skiöld, T. (author)
Laboratory for Isotope Geology, Swedish Museum of Natural History, Stockholm, Sweden
Elming, Sten-Åke (author)
Luleå tekniska universitet,Geovetenskap och miljöteknik
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Claesson, S. (author)
Laboratory for Isotope Geology, Swedish Museum of Natural History, Stockholm, Sweden
Jensen, T. D. (author)
Greenland Geological Survey, Copenhagen, Denmark
Hobbs, R. W. (author)
Department of Geophysics, Stanford University, California, USA
Klemperer, S. L. (author)
Department of Geophysics, Stanford University, California, USA
Matthews, D. H. (author)
British Institutions' Reflection Profiling Syndicate (BIRPS), Bullard Laboratories, Cambridge University, Cambridge, UK
Snyder, D. B. (author)
British Institutions' Reflection Profiling Syndicate (BIRPS), Bullard Laboratories, Cambridge University, Cambridge, UK
Long, R. (author)
Department of Geological Sciences, Durham University, Durham, UK
Matthews, T. (author)
Department of Geological Sciences, Durham University, Durham, UK
Blundell, D. J. (author)
Department of Geology, RHB New College, Egham, UK
Lund, C-E (author)
Department of Solid Earth Geophysics, University of Uppsala, Uppsala, Sweden
Palm, H. (author)
Department of Solid Earth Geophysics, University of Uppsala, Uppsala, Sweden
Pedersen, L. B. (author)
Department of Solid Earth Geophysics, University of Uppsala, Uppsala, Sweden
Roberts, R. G. (author)
Department of Solid Earth Geophysics, University of Uppsala, Uppsala, Sweden
Heikinen, P. (author)
Institute of Seismology, Helsinki University, Helsinki, Finland
Korhonen, H. (author)
Institute of Seismology, Helsinki University, Helsinki, Finland
Luosto, U. (author)
Institute of Seismology, Helsinki University, Helsinki, Finland
Hjelt, S-E (author)
Department of Geophysics, Oulu University, Oulu, Finland
Komminaho, K. (author)
Department of Geophysics, Oulu University, Oulu, Finland
Yliniemi, J. (author)
Geophysical Observatory, Oulu University, Oulu, Finland
Meissner, R. (author)
Institute for Geophysics, Kiel, Germany
Sadowiak, P. (author)
Institute for Geophysics, Kiel, Germany
Wever, Th. (author)
Institute for Geophysics, Kiel, Germany
Dickmann, T. (author)
GEOMAR Institute, Germany
Flueh, E. R. (author)
GEOMAR Institute, Germany
Berthelsen, A. (author)
Institut for Almen Geologi, Copenhagen, Denmark
Tybo, H. (author)
Institut for Almen Geologi, Copenhagen, Denmark
Balling, N. (author)
Department of Earth Sciences, Aarhus University, Aarhus, Denmark
Normark, E. (author)
Department of Earth Sciences, Aarhus University, Aarhus, Denmark
Nisca, D.H. (author)
Luleå tekniska universitet
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 (creator_code:org_t)
1993
1993
English.
In: Precambrian Research. - 0301-9268 .- 1872-7433. ; 64:1-4, s. 67-84
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Before the deposition of a Proterozoic cover and the repeated Proterozoic reworking of the older rocks, the presently exposed Archaean areas in northern Sweden formed part of a coherent craton. In the present study, we have used Sm---Nd isotopic analyses of Proterozoic granitoids and metavolcanics to delineate the Archaean palaeoboundary. In a regional context, the transition from strongly negative εNd(t) values in the northeast to positive values in the southwest is distinct, and approximately defines the border of the old craton. The Archaean palaeoboundary extends in a WNW direction, and is subparallel to the longitudinal axis of the Skellefte sulphide ore district but it is situated ≈ 100 km farther to the north. The ≈ 1.9 Ga old granitoids on the two sides of the palaeoboundary were all formed in compressional environments, but those situated to the north have higher contents of LILE and LREE at similar contents of Si. This indicates that they were generated in an area with thicker crust and supports the location of the Archaean-Proterozoic palaeoboundary. There is no simple correlation between the Archaean palaeoboundary, as defined by the isotopic results, and any of the major fracture systems as interpreted from regional geophysical measurements. Reflection seismic work indicates that juvenile volcanic-arc terrains to the south have been thrust onto the Archaean craton. Possible thrust faults have been identified from aeromagnetic measurements. Rifting of the Archaean craton created a passive margin ≈ 2.0 Ga ago. Spreading shifted to convergence with subduction beneath the Archaean continent ≈ 1.9 Ga ago. Subsequently, the resulting juvenile volcanic arc collided with the old continent, and the Archaean palaeoboundary as existing today was formed by a collision characterized by overthrusting. The boundary then was disturbed by later deformation predominantly along NNE-trending fracture systems.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geofysik (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geophysics (hsv//eng)

Keyword

Applied Geology
Tillämpad geologi
Applied Geophysics
Tillämpad geofysik

Publication and Content Type

ref (subject category)
art (subject category)

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