1887
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Abstract

The release of meltwater from the margins of the Late Quaternary Fennoscandian ice sheets resulted in complex networks of (now buried) Pleistocene tunnel-valleys that extend beneath large parts of the North Sea and the adjacent northern European lowlands.

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/content/papers/10.3997/2214-4609.201404987
2009-06-08
2021-12-04
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201404987
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