Surface waves from the Atlantic (I) ; The crust and upper mantle beneath Iceland (II)
1. Surface waves from the Atlantic It is shown that Rayleigh wave arrivals can "be used to locate small earthquakes which are not detectable using normal "body wave techniques. Using Rayleigh wave arrivals at four stations, six small earthquakes have been located on the Reykjanes Ridge, Th...
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Durham University
1969
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.585902 |