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
Originalsprog | Engelsk |
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Antal sider | 237 |
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Status | Udgivet - 1988 |
ID: 13087776