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Abstract

The continental break-up between Norway and Greenland occurred in late Paleocene / early Eocene, and was associated with an intensive volcanisim along the margin. At a passive continental margin the whole process of crustal evolution is generally retained in the crustal structure from the continent to the ocean.

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/content/papers/10.3997/2214-4609.201409544
1995-05-29
2024-04-25
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