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A three-dimensional lithospheric-scale thermal model of Germany

Abstract. 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.