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/rapportDoktordisputats

OriginalsprogEngelsk
Antal sider237
StatusUdgivet - 1988

ID: 13087776