1887

Abstract

Palaeomagnetic data from the c. 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.

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/content/papers/10.3997/2214-4609-pdb.144.20
2003-10-07
2025-01-24
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