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An attempt based on an interpretation of multichannel reflection seismic data to delineate sedimentary sequences, structures and evolution in the part of the Western Barents Sea between 72°-74°N and 10°-17°E

Publikation: Bog/antologi/afhandling/rapport › Doktordisputats

OriginalsprogEngelsk
Antal sider237
StatusUdgivet - 1988

Citationsformater