Searched for: author:"van Wees, J.D."
(1 - 4 of 4)
document
van Wees, J.D. (author), van Bergen, F. (author), David, P. (author), Nepveu, M. (author), Beekman, F. (author), Cloetingh, S. (author), Bonté, D. (author), TNO Bouw en Ondergrond (author)
Tectonic modeling is often neglected in the basin modeling workflow and heat flow is most times considered a user input. Such heat flows can, therefore, result in erroneous basin modeling outcomes, resulting in false overoptimistic identification of prospective areas or failure to identify prospects. This is particularly true for areas with...
article 2009
document
van Wees, J.D. (author), Bertotti, G. (author), David, P. (author), van Bergen, F. (author), Cloetingh, S. (author), TNO Bouw en Ondergrond (author)
Basin modelling results can be very sensitive to (paleo-)temperature uncertainties. For frontier basins, in particular for deep water settings, the thermal signature of the basin is poorly constrained, as data from wells are lacking. This may lead to wrong heat flow assumptions if these are extrapolated from the shallow offshore or onshore....
conference paper 2007
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van Balen, R.T. (author), van Bergen, F. (author), de Leeuw, C. (author), Pagnier, H. (author), Simmelink, H. (author), van Wees, J.D. (author), Verweij, J.M. (author), Nederlands Instituut voor Toegepaste Geowetenschappen TNO (author)
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...
article 2000
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Nederlands Instituut voor Toegepaste Geowetenschappen TNO (author), van Balen, R.T. (author), van Bergen, F. (author), de Leeuw, C. (author), Pagnier, H. (author), Simmelink, E. (author), van Wees, J.D. (author), Verweij, H. (author)
The hydrocarbon systems of the West Netherlands Basin are analysed using the two-dimensional forward modelling. Three source rock intervals are considered in the modelling. The history of heatflow is calculated from the forward modelling of tectonic subsidence. Modelling results show that the oil accumulations were filled just after the Sub...
conference paper 2000
Searched for: author:"van Wees, J.D."
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