High-level landscapes along the margin of southern East Greenland鈥擜 record of tectonic uplift and incision after breakup in the NE Atlantic
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Elevated erosion surfaces in two steps characterise East Greenland passive margin.

The upper surface truncates basalts erupted near sea level during Atlantic breakup.

Erosion graded the landscape to base level (the sea) after post-basalt uplift.

The upper erosion surface reached its present elevation after two uplift phases.

Analogous surfaces on conjugate margin indicate post-breakup uplift in Norway.

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