Abstract
The Lower Eleonore Bay Group outcropping on the eastern flank of the 'central metamorphic complex' and in the Alpefjord region comprises a sedimentary sequence more than 8000 m thick. It is overlain concordantly by the Upper Eleonore Bay Group, Tillite Group (Eocambrian) and Cambro-Ordovician sediments.
Highlights
Investigations on the Lower Eleonore Bay Group in the Alpefjord region, central East Greenland
The Lower Eleonore Bay Group outcropping on the eastern flank of the 'central metamorphic complex' and in the Alpefjord region comprises a sedimentary sequence more than 8000 m thick
Layers are rich in mud cracks and small-scale channeis, both types are filled up by sandy material, and similar to those recorded in Canning Land (Caby, 1972). These small-scale channels,which occur throughout the Lower Eleonore Bay Group, resemble on bedding surfaces branching and meandering rill marks with accumulation tongues formed in tidal fl~t~
Summary
Investigations on the Lower Eleonore Bay Group in the Alpefjord region, central East Greenland The Lower Eleonore Bay Group outcropping on the eastern flank of the 'central metamorphic complex' and in the Alpefjord region comprises a sedimentary sequence more than 8000 m thick.
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