Searched for: author:"van Wees, J.D."
(1 - 11 of 11)
document
Limberger, J. (author), Boxem, T. (author), Pluymaekers, M. (author), Bruhn, D. (author), Manzella, A. (author), Calcagno, P. (author), Beekman, F. (author), Cloetingh, S. (author), van Wees, J.D. (author)
In this paper we present results of a global resource assessment for geothermal energy within deep aquifers for direct heat utilization. Greenhouse heating, spatial heating, and spatial cooling are considered in this assessment. We derive subsurface temperatures from geophysical data and apply a volumetric heat-in-place method to improve current...
article 2018
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Limberger, J. (author), Bonte, D. (author), de Vicente, G. (author), Beekman, F. (author), Cloetingh, S. (author), van Wees, J.D. (author)
Brittle basement and sedimentary rocks, in particular if these are underlain by radiogenic crust, are considered a prime target for enhanced geothermal systems (EGS). They are marked by high geothermal gradients, caused by radiogenic heat production, and are well suited to be used for geothermal doublets after hydraulic stimulation. Critical...
article 2017
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Cloetingh, S. (author), van Wees, J.D. (author), Wesztergom, V. (author)
Geothermal energy is an important renewable energy resource, whose share is growing rapidly in the energy mix. Geosciences provide fundamental knowledge on Earth system processes and properties, required for the development of new methods to identify prospective geothermal resources suitable for exploitation. Through robust prediction and...
article 2017
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Smit, J. (author), van Wees, J.D. (author), Cloetingh, S. (author)
The crustal seismic velocity structure of northwestern Europe shows a low P-wave velocity zone (LVZ) in the lower crust along the Caledonian Thor suture zone (TSZ) that cannot be easily attributed to Avalonia or Baltica plates abutting the TSZ. The LVZ appears to correspond to a hitherto unrecognized crustal segment (accretionary complex) that...
article 2016
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Lipsey, L. (author), Pluymaekers, M. (author), Goldberg, T. (author), van Oversteeg, K. (author), Ghazaryan, L. (author), Cloetingh, S. (author), van Wees, J.D. (author)
The presence of convective fluid flow in permeable layers can create zones of anomalously high temperature which can be exploited for geothermal energy. Temperature measurements from the Luttelgeest-01 (LTG-01) well in the northern onshore region of the Netherlands indicate variations in the thermal regime that could be indicative of convection....
article 2016
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Beglinger, S.E. (author), van Wees, J.D. (author), Cloetingh, S. (author), Doust, H. (author)
The Campos Basin is a petroleum-productive, marginal sag basin along the Brazilian margin. It contains a stratigraphic sequence recording lithospheric extension and rift tectonics developing to a fully evolved postbreakup setting. We present a combined approach using subsidence analysis and basin history inversion models to make predictions on...
article 2012
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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
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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
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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
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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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