Searched for: author:"Cloetingh, S."
(1 - 13 of 13)
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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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Vargas, H. (author), Gaspar-Escribano, J.M. (author), López-Gómez, J. (author), van Wees, J.-D. (author), Cloetingh, S. (author), de la Horra, R. (author), Arche, A. (author)
The Permian-Triassic sediments of the Iberian Plate are a well studied case of classical Buntsandstein-Muschelkalk-Keuper facies, with good sedimentological interpretations and precise datings based on pollen and spore assemblages, ammonoids and foraminifera. Synrift-postrift cycles are recorded in these facies, but there are only a few studies...
article 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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Cloetingh, S. (author), Cornu, T. (author), Ziegler, P.A. (author), Beekman, F. (author), Ustaszewski, K. (author), Schmid, S.M. (author), Dèzes, P. (author), Hinsch, R. (author), Decker, K. (author), Lopes Gardozo, G. (author), Granet, M. (author), Bertrand, G. (author), Behrmann, J. (author), van Balen, R. (author), Michon, L. (author), Pagnier, H. (author), Rozsa, S. (author), Heck, B. (author), Tesauro, M. (author), Kahle, H.G. (author), Dewez, T. (author), Carretier, S. (author), Winter, T. (author), Hardebol, N. (author), Bada, G. (author), Dost, B. (author), van Eck, T. (author), TNO Bouw en Ondergrond (author)
Research on neotectonics and related seismicity has hitherto been mostly focused on active plate boundaries that are characterized by generally high levels of earthquake activity. Current seismic hazard estimates for intraplate domains are mainly based on probabilistic analyses of historical and instrumental earthquake catalogues. The accuracy...
article 2006
document
Worum, G. (author), van Wees, G.D. (author), Bada, G. (author), van Balen, R.T. (author), Cloetingh, S. (author), Pagnier, H. (author)
We describe a new numerical approach to constrain the three‐dimensional (3‐D) pattern of fault reactivation. Taking advantage of the knowledge of the tectonic stress field, the ratio of the resolved shear and normal stresses (slip tendency) as well as the direction of the shear stress is calculated at every location on the faults modelled by...
article 2004
Searched for: author:"Cloetingh, S."
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