Mapping of Lower Cretaceous (Knurr Sandstone) turbidite lobes using Seismic Stratigraphy and prospectivity along the southern Loppa High Margin, Hammerfest Basin, Barents Sea, Norway
The Hammerfest Basin was formed through downfaulting in Late Jurassic-Early Cretaceous times, allowing the deposition and preservation of Jurassic sediments which later were covered by thick Cretaceous sequences filling in the basin. This study has been conducted along the southern margin of the Lop...
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Format: | Others |
Language: | English |
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Uppsala universitet, Geofysik
2008
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Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-183699 |