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Modelling the hydrocarbon generation and migration in the West Netherlands Basin, the Netherlands

Published online by Cambridge University Press:  01 April 2016

R.T. van Balen*
Affiliation:
Netherlands Institute of Applied Geoscience TNO - National Geological Survey, Department of Geo-Energy, P.O. Box 80015, 3508 TA Utrecht.
F. van Bergen
Affiliation:
Netherlands Institute of Applied Geoscience TNO - National Geological Survey, Department of Geo-Energy, P.O. Box 80015, 3508 TA Utrecht.
C. de Leeuw
Affiliation:
Netherlands Institute of Applied Geoscience TNO - National Geological Survey, Department of Geo-Energy, P.O. Box 80015, 3508 TA Utrecht.
H. Pagnier
Affiliation:
Netherlands Institute of Applied Geoscience TNO - National Geological Survey, Department of Geo-Energy, P.O. Box 80015, 3508 TA Utrecht.
H. Simmelink
Affiliation:
Netherlands Institute of Applied Geoscience TNO - National Geological Survey, Department of Geo-Energy, P.O. Box 80015, 3508 TA Utrecht.
J.D. van Wees
Affiliation:
Netherlands Institute of Applied Geoscience TNO - National Geological Survey, Department of Geo-Energy, P.O. Box 80015, 3508 TA Utrecht.
J.M. Verweij
Affiliation:
Netherlands Institute of Applied Geoscience TNO - National Geological Survey, Department of Geo-Energy, P.O. Box 80015, 3508 TA Utrecht.
*
2corresponding author; e-mail: [email protected]; http://www.nitg.tno.nl/basin-modelling
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Abstract

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The hydrocarbon systems of the Mesozoic, inverted West Netherlands Basin have been analyzed using 2-D forward modelling. Three source rocks are considered in the modelling: Lower Jurassic oil-prone shales, Westphalian gas-prone coal deposits, and Lower Namurian oil-prone shales. The Lower Namurian hydrocarbon system of the basin is discussed for the first time.

According to the modelling results of the Early Jurassic oil system, the oil accumulations were filled just after the main inversion event. Their predicted locations are in agreement with exploration results. Modelling results of the Westphalian gas system, however, show smaller and larger sized accumulations at unexplored locations. The gas reservoirs were filled during the Late Jurassic-Early Cretaceous rifting phase. Results of modelling of the Lower Namurian oil system indicate that gas formed by secondary cracking of the oils can have mixed with the Westphalian coal-derived gas. Such a mixing is inferred from geochemical analyses. The existence of a Lower Namurian hydrocarbon system in the West Netherlands Basin implies that hydrocarbons are possibly trapped in the Westphalian and Namurian successions. These potential traps in the basin have not yet been explored.

Type
Research Article
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2000

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