Journal Title
Title of Journal: Int J Earth Sci Geol Rundsch
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Abbravation: International Journal of Earth Sciences
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Publisher
Springer-Verlag
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Authors: Jacek Majorowicz Stanislaw Wybraniec
Publish Date: 2010/03/07
Volume: 100, Issue: 4, Pages: 881-887
Abstract
Heat flow variations with depth in Europe can be explained by a model of surface temperature changes 10°C New heat flow map of Europe is based on updated database of uncorrected heat flow values to which paleoclimatic correction is applied across the continent Correction is depth dependent due to a diffusive thermal transfer of the surface temperature forcing of which glacial–interglacial history has the largest impact It is obvious that large part of the uncorrected heat flow values in the existing heat flow databases from wells as shallow as few hundreds of meters is underestimated This explains some very low uncorrected heat flow values 20–30 mW/m2 in the shields and shallow basin areas of the craton Also heat flow values in other areas including orogenic belts are likely underestimated Based on the uncorrected and corrected heat flow maps using 5 km × 5 km grid we have calculated average heat flow values uncorrected heat flow 560 mW/m2 SD 203 mW/m2 vs corrected heat flow 632 mW/m2 SD 196 m/Wm2 and heat loss for the continental part Total heat loss is 928 E09 W for the uncorrected values versus corrected 1050 E09 WFirst author JM would like to thank Prof Will Gosnold of the University of North Dakota Dr Jan Safanda Czech Academy of Science and Dr Volker Rath of the Dpt of Earth Sciences Astronomy and Astrophysics Faculty of Physical Sciences Universidad Complutense de Madrid for stimulating discussions We would like to thank Dr M Fernandez for help with the Iberian peninsula data Dr Vladimir Cermak is acknowledged for his comments and having me JM started on the European heat flow mapping team in early 70th V Cermak editorial comments and helpful comments of anonymous reviewers led to improvement of the manuscript
Keywords:
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- Sedimentary development and correlation of Late Quaternary terraces in the Kyrenia Range, northern Cyprus, using a combination of sedimentology and optical luminescence data
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- The strong diachronous Muschelkalk/Keuper facies shift in the Central European Basin: implications from the type-section of the Erfurt Formation (Lower Keuper, Triassic) and basin-wide correlations
- Cenozoic tectonic evolution in the Central Andes in northern Chile and west central Bolivia: implications for paleogeographic, magmatic and mountain building evolution
- Abundances and isotopic compositions of rhenium and osmium in pyrite samples from the Huaibei coalfield, Anhui, China
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- Early Cretaceous highly positive ε Nd felsic volcanic rocks from the Hinggan Mountains, NE China: origin and implications for Phanerozoic crustal growth
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- Mineralogy and mineral chemistry of detrital heavy minerals from the Rhine River in Germany as evidence to their provenance, sedimentary and depositional history: focus on platinum-group minerals and remarks on cassiterite, columbite-group minerals and uraninite
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- Sedimentary evolution of Lake Van (Eastern Turkey) reconstructed from high-resolution seismic investigations
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