Abstract
Small outliers of sedimentary rocks overlying the Tertiary basalts of the northern Blosseville Kyst are preserved in down-faulted areas at Kap Dalton and Savoia Halvø (Kap Brewster) (Watt et al., this report). They are of particular interest in that their age establishes a younger limit for the period of effusive vulcanity on this sector of the East Greenland continental margin.

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