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Автор ROBERTS, R. J.
Автор TORSVIK, T. H.
Автор ANDERSEN, T. B.
Автор REHNSTRÖM, E. F.
Дата выпуска 2003
dc.description Palaeomagnetic data from the 337 Ma Magerøy dykes (northern Norway) are of exceptionally high quality, and a positive contact test along with an existing regional result from the Silurian Honningsvåg Igneous Suite attests to a primary Early Carboniferous magnetic signature. The palaeomagnetic pole (S14.8°, E320.1°, dp/dm=4.4/8.6°) is the first Early Carboniferous pole from Baltica, and implies that northernmost Norway–Greenland, the Barents Sea and Svalbard were located at tropical to low northerly latitudes at this time. Northward drift during Carboniferous times (5–6 cm/yr) as demonstrated from palaeomagnetic data is also reflected in the sedimentary facies in the Barents Sea realm, that is, a change from tropical (Early Carboniferous) to subtropical (20–30° N) carbonates and evaporites in the Late Carboniferous. The Magerøy dykes are continental tholeiites which intruded into a set of NW–SE-trending normal faults parallel to the Trollfjorden–Komagelva Fault Zone and the Magerøysundet Fault immediately to the north and south of Magerøya, respectively. These, and many other NW–SE-trending faults (onshore and offshore), were active during Late Palaeozoic extension, and the dykes were probably contemporaneous with the earliest syn-rift sedimentation in the Barents Sea (for example, the Nordkapp Basin).
Издатель Cambridge University Press
Тема Norway
Тема palaeomagnetism
Тема Carboniferous
Тема palaeogeography
Название The Early Carboniferous Magerøy dykes, northern Norway: palaeomagnetism and palaeogeography
DOI 10.1017/S0016756803008082
Electronic ISSN 1469-5081
Print ISSN 0016-7568
Журнал Geological Magazine
Том 140
Первая страница 443
Последняя страница 451
Аффилиация ROBERTS R. J.; Wits University
Аффилиация TORSVIK T. H.; Geological Survey of Norway; Institute for Petroleum Technology and Applied Geophysics, NTNU;
Аффилиация ANDERSEN T. B.; University of Oslo
Аффилиация REHNSTRÖM E. F.; University of Oslo; Lund University
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