Seismic reflection and gravity investigations of the 'Widmerpool Gulf' in the East Midlands, with a study of linear seismic sources and data processing techniques involving computer graphics
The gravity anomalies in the vicinity of the Widmerpool Gulf display a strong negative trend, which is best fitted by a third degree surface. This trend is attributed to the development of thick conglomeratic and quartzitic materials, probably of O.R.S and/or Lower Palaeozoic age. The "residual...
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University of Leicester
1972
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.674066 |