Searched for: author:"van Wees, J.D."
(1 - 6 of 6)
document
Cloetingh, S. (author), van Wees, J.D. (author), Ziegler, P.A. (author), Lenkey, L. (author), Beekman, F. (author), Tesauro, M. (author), Förster, A. (author), Norden, B. (author), Kaban, M. (author), Hardebol, N. (author), Bonté, D. (author), Genter, A. (author), Guillou-Frottier, L. (author), ter Voorde, M. (author), Sokoutis, D. (author), Willingshofer, E. (author), Cornu, T. (author), Worum, G. (author), TNO Bouw en Ondergrond (author)
Knowledge of temperature at drillable depth is a prerequisite in site selection for geothermal exploration and development of enhanced geothermal systems (EGS). Equally important, the thermo-mechanical signature of the lithosphere and crust provides critical constraints for the crustal stress field and basement temperatures where borehole...
article 2010
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), Cloetingh, S. (author), Ziegler, P.A. (author), Lenkey, L. (author), Beekman, F. (author), Tesauro, M. (author), Förster, A. (author), Norden, B. (author), Kaban, M. (author), Hardebol, N. (author), Voorde, M.T. (author), Willingshofer, E. (author), Cornu, T. (author), Bonté, D. (author), TNO Bouw en ondergrond (author)
For geothermal exploration and the development of enhanced geothermal systems (EGS) knowlegde of temperature at drillable depth is a prerequisite for site selection. Equally important is the thermo-mechanical signature of the lithosphere and crust which allow to obtain critical constraints for the crustal stress field and basement temperatures...
conference paper 2009
document
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
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
document
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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