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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:harald.karg@wintershall.com.ar
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
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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

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