Pockmarks, gas flares, carbonate crusts and their relation to tectonic and stratigraphic evolution of southwestern Barents Sea

The project's aim is to achieve a better understanding of shallow geological/seabed conditions and processes to support technical and environmental aspects of exploration and production along the southwestern margin of the Barents Sea, including the Hammerfest Basin, the Loppa High, the Polheim Subplatform, the Tromsø Basin/lngøydjupet area and along the Finnmark Platform.

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Available:
NGU-biblioteket
Series:
NGU-rapport
Series nr:
2013.025
Page number:
60
ISSN:
0800-3416
Document type:
Rapport
Project:
Neotectonics and Fluid Flow Processes in the Southwestern Barents Sea
Project nr:
341300