Swedish Ordovician limestones: Problems in clarifying their directions of magnetizations

Physics

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Scientific paper

The easterly region of the Swedish Ordovician limestones (the Orthoceras Limestone) shows a fairly stable bulk magnetization of high positive (downward) inclination. A closer scrutiny reveals, however, that this magnetization is of polyphase structure, involving at least two axes of magnetization. The components have similar stability spectra, and alternating field demagnetization cannot separate them. Thermal demagnetization is more effective but no stable end-point has been reached.

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