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Sökning: onr:"swepub:oai:DiVA.org:ltu-101624" > New palaeoproterozo...

New palaeoproterozoic palaeomagnetic data from Central and Northern Finland indicate a long-lived stable position for Fennoscandia

Luoto, T. (författare)
Department of Geosciences and Geography, P.O. Box 64, 00014 University of Helsinki, Finland; Geological Survey of Finland, P.O. Box 96, 02151 Espoo, Finland
Salminen, J. (författare)
Department of Geosciences and Geography, P.O. Box 64, 00014 University of Helsinki, Finland; Geological Survey of Finland, P.O. Box 96, 02151 Espoo, Finland
Mertanen, S. (författare)
Geological Survey of Finland, P.O. Box 96, 02151 Espoo, Finland
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Elming, Sten-Åke (författare)
Luleå tekniska universitet,Geovetenskap och miljöteknik
Pesonen, L. J. (författare)
Department of Physics, University of Helsinki, P.O. Box 64, 00014, Finland
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Department of Geosciences and Geography, PO. Box 64, 00014 University of Helsinki, Finland; Geological Survey of Finland, P.O. Box 96, 02151 Espoo, Finland Geological Survey of Finland, P.O. Box 96, 02151 Espoo, Finland (creator_code:org_t)
Oxford Univ Press, 2023
2023
Engelska.
Ingår i: Geophysical Journal International. - : Oxford Univ Press. - 0956-540X .- 1365-246X. ; 235:2, s. 1810-1831
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • The Svecofennian gabbro intrusions coincide temporally with the global 2100-1800 Ma orogens related to the amalgamation of the Mesoproterozoic supercontinent Nuna. We provide a new reliable 1891-1875 Ma palaeomagnetic pole for Fennoscandia based on rock magnetic and palaeomagnetic studies on the Svecofennian intrusions in central Finland to fill gaps in the Palaeoproterozoic palaeomagnetic record. By using the new pole together with other global high-quality data, we propose a new palaeogeographic reconstruction at 1885 Ma. This, together with previous data, supports a long-lived relatively stable position of Fennoscandia at low to moderate latitudes at 1890-1790 Ma. Similar stable pole positions have also been obtained for Kalahari at 1880-1830 Ma, Siberia at 1880-1850 Ma, and possibly India at 1980-1775 Ma. A new reconstruction at the beginning of this period indicates the convergence of several cratons at 1885 Ma in the initial stages of the amalgamation of the Nuna supercontinent at low to moderate latitudes. The close proximity of cratons at low to moderate latitudes is further supported by global and regional palaeoclimatic indicators. Stable position of several cratons could indicate a global period of minimal apparent drift at ca. 1880-1830 Ma. Before this period, the global palaeomagnetic record indicates large back-and-forth swings, most prominently seen in the high-resolution 2020-1870 Ma Coronation loops of the Slave craton. These large back-and-forth movements have been explained as resulting from an unstable geomagnetic field or basin- or local-scale vertical-axis rotations. However, the most likely explanation is inertial interchange true polar wander (IITPW) events, which is in line with the suggestion of large amplitude true polar wander events during the formation of the supercontinent.

Ämnesord

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

Nyckelord

Europe
Palaeomagnetism
Rock and mineral magnetism
Tectonics and landscape evolution
Tillämpad geofysik
Applied Geophysics

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