Norwegian hydrocarbon basins

In reality, oil hydrocarbons evaporated from the surface of Arctic seas return to the Arctic Basin from precipitation. These processes are simulated in blocks APM and PSM. The maximal destruction of oil hydrocarbons is 0.0028 g m-2 da-1. The flow H7q due to bacterial decomposition averages 271 yr 1. It has unequal values for different seas (t yr-1) Bering 3.7, Greenland 11, Norwegian 2.2, Barents 3.4, Kara 2.3, White 2.3, Laptev 2.8, East Siberian 2.8, Chukchi 3.4, Beaufort 2.5, and Central Basin 0.5. 

Schneider, F., Burrus, J., Wolf, S., Doligez, B. and P. Forbes, 1991. Modelling overpressures by efFective-stress/porosity relationship mathematical artefice or physical reality. Paper presented at the Norwegian Petroleum Society International Conference on Basin modelling Advances and applications, Stavanger, Norway, March 13-15, 1991 Schowalter, T.T., 1979. Mechanics of secondary hydrocarbon migration and entrapment. 

Sverdrup, E. Bjhrlykke, K. 1997. Fault properties and development of cemented fault zones in sedimentary basins. Field examples and predictive models. In Mhller-Pedersen, P. Koestler, A. G. (eds) Hydrocarbon Seals. Importance for Exploration and Production. Norwegian Petroleum Society (NPF), Special Publication, 7, 91-106. 

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