Electromagnetic reflections inside ice sheets

When radio echo sounding polar ice sheets weak stratified reflections are visible deep inside the ice sheets. These reflections are often called internal layers. Previously it has been suggested as a result of glacier flow models that these reflections can be treated as surfaces of equal age. In ord...

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Bibliographic Details
Main Author: Miners, William Dingle
Published: Open University 1999
Subjects:
Online Access:https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.266418