A late Carboniferous palaeomagnetic pole recorded from a syenite still, Stabben, Central Norway

Details A late Carboniferous palaeomagnetic pole recorded from a syenite still, Stabben, Central Norway A late Carboniferous palaeomagnetic pole recorded from a syenite still, Stabben, Central Norway

Dec 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987pepi...49..350s&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 49, Issue 3-4, p. 350-359.

Physics

5

Scientific paper

High-blocking remanence components (D = 192°, I = - 12°) recorded in a syenite sill from the Island of Stabben, Central Norway, are considered to be of primary/deuteric origin and to correspond to the radiometric age (297 Ma). The upper part of the sill and the contact gneiss, however, are strongly contaminated by a younger magnetic overprint (D = 8°, I = 59°). The primary component may represent a reliable Upper Carboniferous pole determination from Western Scandinavia, whereas the secondary component most probably relates to Cretaceous or younger faulting.

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