A palaeomagnetic study of Tertiary and Devonian igneous rocks from Britain
Theoretical angular dispersion curves were produced from a model of the geomagnetic field in which parameters such as dipole wobble, dipole moment, and secular variation could vary independently of each other. Comparison with palaeomagnetic data suggested that the average geomagnetic field could be...
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Imperial College London
1968
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.526303 |