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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00004104naa a2200349 4500
001oai:DiVA.org:ltu-7264
003SwePub
008160929s1989 | |||||||||||000 ||eng|
024a https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-72642 URI
024a https://doi.org/10.1016/0040-1951(89)90355-72 DOI
040 a (SwePub)ltu
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Pesonen, L. J.u Geological Survey of Finland4 aut
2451 0a Crustal evolution of Fennoscandia :b palaeomagnetic constraints
264 1b Elsevier BV,c 1989
338 a print2 rdacarrier
500 a Godkänd; 1989; 20070316 (ysko)
520 a Palaeomagnetic poles from Fennoscandia, ranging in age from Archaean to Tertiary, are compiled and graded using a modified Briden-Duff classification scale. An new "filtering" technique is applied to select only the most reliable poles for analysis. The filtering takes into account the following information: 1. (1) source block of rock unit,2. (2) age of rock,3. (3) age of magnetization component,4. (4) scatter of palaeomagnetic directions,5. (5) information from multicomponent analysis of natural remanent magnetization (NRM),6. (6) whether the pole considered belongs to a cluster or subcluster of poles,7. (7) magnetic polarity and8. (8) the author's original assignment of results.Data are still insufficient for the drawing of separate Apparent Polar Wander Paths (APWP) for different blocks or cratons of Fennoscandia. Treating Fennoscandia as a single plate, a new APWP from Archaean to Permian is constructed. From the five previously drawn APWP loops (or "hairpins"), only one, the Jatulian loop (2200-2000 Ma), disappears in filtering. The loops during 1925-1700 Ma and during 1100-800 Ma ago are linked to Svecofennian and Sveconorwegian orogenies, respectively. Palaeomagnetic data support the concept that these orogenies took place episodically; three distinct orogenic pulses (early, middle and late) can be distinguished in the cluster plots of palaeopoles. The drift history of Fennoscandia from Archaean to Permian is presented. During most of geological history, Fennoscandia has occupied low to moderate latitudes and undergone considerable latitudinal shifts and rotations. The Svecofennian and Sveconorwegian orogenies have different kinematic characteristics. During the Svecofennian orogeny, Fennoscandia drifted slowly while rotating a large amount in an anticlockwise sense. During the Sveconorwegian orogeny, it drifted rapidly and rotated first clockwise and then anticlockwise. The most striking feature in the drift velocity curves is, however, the pronounced maxima in the latitudinal drift and rotation rates (˜ 9 cm/yr and ˜ 0.8°/Ma, respectively) during the late Subjotnian-Jotnian anorogenic magmatism and rifting phase (˜1450-1250 Ma ago), possibly reflecting the passage of Fennoscandia across a thermal upwelling (hotspot) at equatorial latitudes. The use of palaeomagnetism in delineating and dating movements between blocks is demonstrated with three examples from the POLAR Profile area, the northernmost section of the European Geotraverse.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geofysik0 (SwePub)105052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geophysics0 (SwePub)105052 hsv//eng
653 a Applied Geophysics
653 a Tillämpad geofysik
700a Torsvik, T. H.u Department of Earth Sciences, University of Oxford4 aut
700a Elming, Sten-åkeu Luleå tekniska universitet,Geovetenskap och miljöteknik4 aut0 (Swepub:ltu)sael
700a Bylund, G.u Department of Geology, University of Lund4 aut
710a Geological Survey of Finlandb Department of Earth Sciences, University of Oxford4 org
773t Tectonophysicsd : Elsevier BVg 162:1-2, s. 27-49q 162:1-2<27-49x 0040-1951x 1879-3266
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-7264
8564 8u https://doi.org/10.1016/0040-1951(89)90355-7

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By the author/editor
Pesonen, L. J.
Torsvik, T. H.
Elming, Sten-åke
Bylund, G.
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
and Geophysics
Articles in the publication
Tectonophysics
By the university
Luleå University of Technology

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