A receiver function study of the crust and mantle beneath the British Isles
A seismic experiment across the British Isles was undertaken to probe the structure of both the crust and mantle in order to constrain the causes of Cenozoic uplift. Seismic data were processed using an iterative deconvolution method to produce receiver functions showing P-to-S conversions from velo...
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University of Cambridge
2010
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.598396 |