1. Unlocking the Cretaceous Petroleum Systems of the Norwegian Sea
- Author
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M. Erdmann, S.A. Clark, E. Rein, S.A. Bullimore, B.J. Schmidt, R. Kyrkjebø, L.M. Johansen, M. Roudot, O. Thießen, M. Dörner, E. Stavrou, J. O. Hansen, A. Wenke, C. Vandré, J. Zweigel, A. Orlovs, J.H. van Koverden, A.E. Ryseth, O.S. Kløvjan, B. Rafaelsen, U. Mann, G. Boonen Ferreira, P. Embry, and M. Inthorn
- Subjects
Natural gas field ,chemistry.chemical_compound ,Source rock ,chemistry ,Geochemistry ,Petroleum ,Structural basin ,Cenomanian ,Petroleum play ,Geology ,Cretaceous ,Deposition (geology) - Abstract
Summary The Mid-Norwegian segment of the Norwegian Continental Shelf, between 62° and 67° N, includes a Berriasian to Paleocene basin fill of >12.5 km thickness. The area of deposition covers several major basins and sub-basins, including the More and Voring basins and adjacent terraces. Although the area contains the large Ormen Lange and Aasta Hansteen gas fields, the discovery density in post-Jurassic strata is not comparable with the Jurassic petroleum play on the Halten-/Donna terraces. To fully re-assess the Cretaceous petroleum system of the Norwegian Sea, an integrated petroleum system analysis study was performed including i) source rock evaluation, ii) top-down petroleum systems analysis, iii) petroleum systems modeling and iv) migration and charge analysis. Three rich source rock formations have been proven, indications for five additional source rock formations related to Cretaceous OAE collected. Regional petroleum-source correlations identified the presence of oils and condensates of pre-Albian, Cenomanian/Turonian and post-Turonian origin. The study shows that the volumes of expelled hydrocarbons and thus the YTF oil volumes are underestimated in the area. The Cretaceous petroleum systems study results were finally implemented in recent exploration strategies and proven by new discoveries on the Norwegian Continetal Shelf.
- Published
- 2021
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