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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Main Authors: D. Anikiev, A. Lechel, M. L. Gomez Dacal, J. Bott, M. Cacace, M. Scheck-Wenderoth
Format: Article
Language:English
Published: Copernicus Publications 2019-12-01
Series:Advances in Geosciences
Online Access:https://www.adv-geosci.net/49/225/2019/adgeo-49-225-2019.pdf
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spelling 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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