Abstract
The northern part of the Blosseville Kyst between Kap Brewster and Kap Dalton was briefly investigated during a three week boat supported reconnaissance folIowing an aerial interpretation of the coastal structure (Watt, 1975). Most emphasis was laid on sorting out the relationship between the sediments at Kap Dalton and the structural relationship between the underlying and surrounding lava flows. Samples were collected for micropalaeontological studies both from the Kap Dalton sedimentary series and from a number of interbasaltic sediments (Soper & Costa, this report). In addition a series of traverses were made through parts of the basalt succession between Kap Dalton and Steward Ø.
Highlights
East GreenlandThe northern part of the Blosseville Kyst between Kap Brewster and Kap Dalton was briefly investigated during a three week boat supported reconnaissance folIowing an aerial interpretation of the coastal structure (Watt, 1975)
Samples wereeollected for micropalaeontological studies both from the Kap Dalton sedimentary series and from a' number of interbasaltic sediments (Soper & Costa, this report)
North-east ofKap Dalton a broad zone offauIting trends parallel to the coast separating an outer zone Df steeply dipping basalts from an inner zone ofbasalts with a shallow inland dip
Summary
The northern part of the Blosseville Kyst between Kap Brewster and Kap Dalton was briefly investigated during a three week boat supported reconnaissance folIowing an aerial interpretation of the coastal structure (Watt, 1975). Most emphasis was laid on sorting out the relationship between the sediments at Kap. Dalton and the structural relati~nship between the underlying and surrounding lava flows. Samples wereeollected for micropalaeontological studies both from the Kap Dalton sedimentary series and from a' number of interbasaltic sediments (Soper & Costa, this report). In addition a series of traverses were made through parts of the basalt succession between Kap Dalton and Steward ø
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