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Magnetic anomalies and rock magnetism of basalts from Reykjanes (SW-Iceland)
Authors:Frank Dietze  Agnes Kontny  Ingo Heyde  Carsten Vahle
Institution:1.Institut für Angewandte Geowissenschaften,Karlsruher Institut für Technologie (KIT),Karlsruhe,Germany;2.Bundesanstalt für Geowissenschaften und Rohstoffe,Hannover,Germany;3.Eriksfiord AS, Kunnskapsparken,Stavanger,Norway
Abstract:This study presents rock magnetic properties along with magnetic field measurements of different stratigraphic and lithologic basalt units from Reykjanes, the southwestern promontory of the Reykjanes peninsula, where the submarine Reykjanes Ridge passes over into the rift zone of southwestern Iceland. The basaltic fissure eruptions and shield lava of tholeiitic composition (less than 11500 a old) show a high natural remanent magnetization (NRM, Jr) up to 33.6 A/m and high Koenigsberger ratio (Q) up to 52.2 indicating a clear dominance of the NRM compared to the induced part of the magnetization. Pillow basalts and picritic shield lava show distinctly lower Jr values below 10 A/m. Magnetic susceptibility (κ) ranges for all lithologies from 2.5 to 26×10−3 SI.
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