Analysis of the Palaeomagnetism of the Torridonian Sandstone Series of North-West Scotland. I

Physics

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Scientific paper

The permanent magnetization of the Diabaig, Applecross and Aultbea groups of the Torridonian sandstones of north-west Scotland has been measured. That of the latter two groups is along a NW negative/SE positive axis. Field evidence shows that the majority of these rocks were magnetized soon after deposition and have retained this magnetization substantially unaltered.

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