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• W2023173856 abstract "Several reversed polarity magnetozones occur within deep-sea sediment core CH57-8 from the Greater Antilles Outer Ridge, within sediment of latest Pleistocene/Late Brunhes age. The uppermost reversed interval spanning 31 data points coincides with the X faunal zone of the Last Interglacial Period. Radiochemical dating of cores CH57-8 and KN25-4 has shown that all the reversed polarity magnetozones are significantly younger than the Brunhes/Matuyama boundary at 0.7 m.y. B.P. A variation of the excess230Th method was used, in which210Po and238U were the actual radionuclides measured. In a third core from the Mid-Atlantic Ridge, our210Po results were similar to those which others obtained earlier by direct230Th measurements." @default.
• W2023173856 created "2016-06-24" @default.
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• W2023173856 date "1977-07-01" @default.
• W2023173856 modified "2023-09-27" @default.
• W2023173856 title "Paleomagnetism and radiochemical age estimates for Late Brunhes polarity episodes" @default.
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• W2023173856 doi "https://doi.org/10.1016/0012-821x(77)90072-3" @default.
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