Searched for: author:"van Wees, J.D."
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van Wees, J.D. (author), Bonte, D. (author), Nelskamp, S. (author), TNO Bouw en Ondergrond (author)
Basement heat flow is one of the most influential parameters on basin maturity. Although rapid progress has been made in the development of tectonic models capable of modelling the thermal consequences of basin formation, these models are hardly used in basin modelling. To better predict heat flows we have developed a multi-1D probabilistic...
conference paper 2009
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Doornenbal, J.C. (author), Abbink, O.A. (author), Pagnier, H.J.M. (author), van Wees, J.D. (author), TNO Bouw en Ondergrond (author)
The Southern Permian Basin (also referred to as Central European Basin) is Europe s largest sedimentary basin. It is a typical intracontinental basin that evolved from latest Carboniferous to recent times and extends from eastern England to the Belarussian-Polish border and from Denmark to South Germany. The Southern Permian Basin Atlas (SPBA)...
conference paper 2009
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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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Abadi, A.M. (author), van Wees, J.D. (author), van Dijk, P.M. (author), Cloetingh, S.A.P.L. (author)
Backstripping analysis of 225 wells located within the Sirt Basin (Fig. 1) provide new constraints on the Sirt Basin development. Four coherent tectonic phases from Late Jurassic to present. The presentation of contour maps of subsidence and crustal stretching allows to visualize spatial and temporal stretching migration. A close match is...
conference paper 2005
Searched for: author:"van Wees, J.D."
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