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A research project proposes to recalibrate the Palaeocene-Eocene boundary using Ar-Ar and U-Pb dating methods. The study, led by the British Geological Survey, aims to resolve discrepancies between magmatic event ages and accepted magnetostratigraphy time ranges. It involves dating sanidine from ash layers in northern Jutland and zircon/sphene from Danish and Hebridean ashes.
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