Use of 2D-seismic data and available wells to investigate the source potential of the Palaeozoic interval in the Loppa High area, SW Barents Sea
While most established plays in the Barents Sea have occurred in the Mesozoic, the Alta and Gohta discoveries prove a new carbonate play concept, with a source rock that does not stem from the Jurassic. Based on depositional environment and TOC values from the Palaeozoic interval a source rock with...
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Format: | Master Thesis |
Language: | English |
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UiT Norges arktiske universitet
2018
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Online Access: | https://hdl.handle.net/10037/12814 |