A three-dimensional lithospheric-scale thermal model of Germany
<p>We present a 3-D lithospheric-scale model covering the area of Germany that images the regional characteristics of the structural configuration and of the thermal field. The structural model resolves major sedimentary, crustal and lithospheric mantle units integrated from previous studies o...
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doaj-fb848bbb018646c8aead37bb78b3b78f2020-11-25T02:21:31ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592019-12-014922523410.5194/adgeo-49-225-2019A three-dimensional lithospheric-scale thermal model of GermanyD. Anikiev0A. Lechel1A. Lechel2M. L. Gomez Dacal3J. Bott4M. Cacace5M. Scheck-Wenderoth6M. Scheck-Wenderoth7GFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling, Potsdam, GermanyGFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling, Potsdam, GermanyTechnical University of Berlin, Department Geotechnology, Berlin, GermanyGFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling, Potsdam, GermanyGFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling, Potsdam, GermanyGFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling, Potsdam, GermanyGFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling, Potsdam, GermanyRWTH Aachen University, Faculty of Georesources and Material Engineering, Aachen, Germany<p>We present a 3-D lithospheric-scale model covering the area of Germany that images the regional characteristics of the structural configuration and of the thermal field. The structural model resolves major sedimentary, crustal and lithospheric mantle units integrated from previous studies of the Central European Basin System, the Upper Rhine Graben and the Molasse Basin, together with published geological and geophysical data. A combined workflow consisting of 3-D structural, gravity and thermal modelling is applied to derive the 3-D thermal configuration. The modelled temperature distribution is highly variable in response to an imposed heterogeneous distribution of thermal properties assigned to the different units. First order variations in the temperature field are mainly attributed to the thermal blanketing effect from the sedimentary cover, the variability in the amount of radiogenic heat produced within the different crystalline crust compartments and the implemented topology of the thermal Lithosphere-Asthenosphere Boundary.</p>https://www.adv-geosci.net/49/225/2019/adgeo-49-225-2019.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
D. Anikiev A. Lechel A. Lechel M. L. Gomez Dacal J. Bott M. Cacace M. Scheck-Wenderoth M. Scheck-Wenderoth |
spellingShingle |
D. Anikiev A. Lechel A. Lechel M. L. Gomez Dacal J. Bott M. Cacace M. Scheck-Wenderoth M. Scheck-Wenderoth A three-dimensional lithospheric-scale thermal model of Germany Advances in Geosciences |
author_facet |
D. Anikiev A. Lechel A. Lechel M. L. Gomez Dacal J. Bott M. Cacace M. Scheck-Wenderoth M. Scheck-Wenderoth |
author_sort |
D. Anikiev |
title |
A three-dimensional lithospheric-scale thermal model of Germany |
title_short |
A three-dimensional lithospheric-scale thermal model of Germany |
title_full |
A three-dimensional lithospheric-scale thermal model of Germany |
title_fullStr |
A three-dimensional lithospheric-scale thermal model of Germany |
title_full_unstemmed |
A three-dimensional lithospheric-scale thermal model of Germany |
title_sort |
three-dimensional lithospheric-scale thermal model of germany |
publisher |
Copernicus Publications |
series |
Advances in Geosciences |
issn |
1680-7340 1680-7359 |
publishDate |
2019-12-01 |
description |
<p>We present a 3-D lithospheric-scale model covering the
area of Germany that images the regional characteristics of the structural
configuration and of the thermal field. The structural model resolves major
sedimentary, crustal and lithospheric mantle units integrated from previous
studies of the Central European Basin System, the Upper Rhine Graben and the
Molasse Basin, together with published geological and geophysical data. A
combined workflow consisting of 3-D structural, gravity and thermal modelling
is applied to derive the 3-D thermal configuration. The modelled temperature
distribution is highly variable in response to an imposed heterogeneous
distribution of thermal properties assigned to the different units. First
order variations in the temperature field are mainly attributed to the
thermal blanketing effect from the sedimentary cover, the variability in the
amount of radiogenic heat produced within the different crystalline crust
compartments and the implemented topology of the thermal
Lithosphere-Asthenosphere Boundary.</p> |
url |
https://www.adv-geosci.net/49/225/2019/adgeo-49-225-2019.pdf |
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