Seismic refraction experiments between Iceland and Scotland
Two reversed seismic refraction profiles, 90 and 120 km in length, located between Iceland and Faeroes, show that the crust of the Iceland-Faeroe Rise is neither typically oceanic nor typically continental. It is of the order of 18 km thick and shows layering similar to that observed on Iceland. Off...
| Main Author: | |
|---|---|
| Published: |
Durham University
1971
|
| Subjects: | |
| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.586004 |