Palaeolatitudinal controls of Phanerozoic sediment-hosted mineral deposits
The distribution of Phanerozoic sediment-hosted mineral deposits appears to be influenced by latitudinal zoning. The palaeolatitudes of the host rocks were determined using standard palaeomagnetic procedures - the most reliable results being for the Mesozoic and Cenozoic with early Palaeozoic palaeo...
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University of Newcastle Upon Tyne
1987
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.380211 |