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New subsurface temperature maps for the Tertiary Lower Rhine Basin and the adjacent Variscan Basement - Germany, The Netherlands, Belgium

Published online by Cambridge University Press:  01 April 2016

H. Karg ,
C. Bücker  and
R. Schellschmidt
H. Karg*
Affiliation:
Lehr- und Forschungsgebiet für Angewandte Geophysik, RWTH Aachen, Lochnerstrasse 4–20, 52064 Aachen, Deutschland. Now: Wintershall Energía S.A., Maipú 757, Piso 7, C1006ACI Buenos Aires, Argentina; e-mail:[email protected]
C. Bücker
Affiliation:
RWE-DEA, Hamburg, Überseering 40, 22297 Hamburg
R. Schellschmidt
Affiliation:
Institute of Joint Geoscientific Research (BGR-GGA), Stilleweg 2, 3055 Hannover
*
2corresponding author

Abstract

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The regional subsurface temperature field at the transition between the Palaeozoic Variscan Basement and the Cenozoic Lower Rhine Basin in Dutch, German and Belgium territories was mapped up to a depth of 1000 m. Temperature data from 66 wells and 11 coal mine subcrops were available. In 46 wells, temperature logs, covering a cumulative depth interval of 6600 m, were measured for this study.

Keywords

Lower Rhine BasinPalaeozoic Basementgeothermal anomaliesisothermal mapsnew temperature logs
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 83 , Issue 2 , June 2004 , pp. 135 - 146
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2004

References

Balke, K.-D., 1970. Geothermische und Hydrogeochemische Anomalien im Erftgebiet.- Fortschr. Min., Beih. 2, S. 1–3, Stuttgart.Google Scholar
Balke, K.-D., 1973. Geothermische und hydrogeologische Untersuchungen in der südlichen Niederrheinischen Bucht. Geol. Jb.C 5:5–61.Google Scholar
De Braaf, W. & Maas, W., 1952. Temperature Gradients in the South-Limburg Coal Field (The Netherlands). Geologie en Mijnbouw 14: 54–57.Google Scholar
Dornstätter, J. & Sattel, G., 1985. Thermal Measurements in the research Borehole Konzen, Hohes Venn (West Germany).-N. Jb. Geol. Paläont. Abh., 171: 117–130, Stuttgart.Google Scholar
Dürbaum, J. & Wolff, W., 1958. Das Schwerebild des südlichen Teils der Niederrheinischen Bucht. Fortschr. Geol. Rheinl. u. Westf. 2: 387–407.Google Scholar
Graulich, J.M., 1983. L’Hydrogéologie thermale de Chaudfontaine. Bull. Soc. Belge Géol. 92-3: 195–212.Google Scholar
Haenel, R., 1983. Geothermal Investigations in the Rhenish Massif. In: Fuchs, K., von Gehlen, K., Mälzer, H., Murawski, H., Semmel, H. (Eds): Plateau Uplift. Springer (Berlin, Heidelberg, New York, Tokyo).Google Scholar
Klett, M., Eichhorst, F. & Schäfer, A., 2002. Facies interpretation from well logs applied to the Tertiary Lower Rhine Basin fill. Netherlands Journal of Geosciences/Geologie en Mijnbouw 81 (2): 167–176.Google Scholar
Legrand, R., 1975. Jalons Géothermiques.-Toegelichte Verhandelingen voor de Geologische kaart en Mijnkaart van Belgie, 16, 1–46, Bruxelles.Google Scholar
Mücke, G., 1964. Die Wärmeleitfähigkeit von Karbongesteinen und ihr Einfluss auf das Grubenklima. Bergbau-Archiv (Essen) 25?: 35–58.Google Scholar
Mücke, G., 1986. Gebirgstemperaturmessung, Zeche Sophia Jacoba, Bergbauforschung GmbH Essen, unpublished.Google Scholar
Pommerening, J., 1992. Hydrogeologie, Hydrogeochemie und Genese der Aachener Thermalquellen. Diss. RWTH Aachen (Aachen): 169 pp.Google Scholar
Ramaekers, J.J.F., 1991. The Netherlands. In: Hurtig, E., Cermak, V., Haenel, R. & Zui, V. (Eds): Geothermal Atlas of Europe. Hermann Haack Verlagsgesellschaft mbH, Gotha.Google Scholar
Sadée, C.P.M., 1975. An Interpretation of South-Limburg Subsurface Temperature Data. Geologie en Mijnbouw 54: 184–194.Google Scholar
Schürmeyer, J., 1984. Bestimmung der Wärmeleitfähigkeit an Gesteinen des Salm (unteres Ordovizium) aus der Forschungsbohrung Konzen (nordöstliches Massiv von Stavelot-Venn) und ihre Korrelation mit geologischen und weiteren petrophysikalischen Parametern. Diplomarbeit RWTH Aachen, unpubl.Google Scholar
Schulz, R. & Schellschmidt, R., 1991. Das Temperaturfeld im südlichen Oberrheingraben. Geol. Jb. E48: 153–165.Google Scholar
Spelter, M., 1978. Hydrogeologie, Hydrogeochemie und Hydrothermie der südlichen Niederrheinischen Bucht, insbesondere des Südteils der Erftscholle. Diss. RWTH Aachen (Aachen): 161 pp.Google Scholar
Van Balen, R.T., Verweij, J.M., Van Wees, J.D., Simmelink, H., Van Bergen, F. & Pagnier, H., 2002. Deep subsurface temperatures in the Roer Valley Graben and the Peelblock, The Netherlands new results. Netherlands Journal of Geosciences/Geologie en Mijnbouw 81 (1): 19–26.Google Scholar
Van Dalfsen, H., 1981. Geothermal Investigation in shallow observation wells. Project G/A 9 - Contracts 073–76, The Shallow Subsurface Temperature Field in The Netherlands, Delft.Google Scholar
Vandenberghe, N. & Fock, W., 1989. Temperature data in the subsurface of Belgium. Tectonophysics 164: 237–250.Google Scholar
Visser, W.A., 1978. Early subsurface temperature measurements in The Netherlands. Geologie en Mijnbouw 57: 1–10.Google Scholar