10.5880/GFZ.4.5.2019.005 eng dataset GFZ German Research Centre for Geosciences datapub@gfz-potsdam.de http://www.gfz-potsdam.de Helmholtz-Centre Potsdam - GFZ German Research Centre for Geosciences Helmholtz-Centre Potsdam - GFZ German Research Centre for Geosciences pointOfContact 2019-12-20 urn:ogc:def:crs:EPSG:4326 3-D-Deutschland (3-D-D): A three-dimensional lithospheric-scale thermal model of Germany 2019-12-20 revision 2019-11-14 creation doi:10.5880/GFZ.4.5.2019.005 Anikiev, Denis GFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling author Lechel, Adrian GFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling; Technical University of Berlin, Department Geotechnology, Berlin, Germany; GEO-data, Hannover, Germany author Gomez Dacal, Maria Laura GFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling author Bott, Judith GFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling author Cacace, Mauro GFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling author Scheck-Wenderoth, Magdalena GFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling author GFZ Data Services publisher We present a 3-D lithospheric-scale model covering the area of Germany that images the regional structural configuration. The model comprises 31 lithostratigraphic units: seawater, 14 sedimentary units, 14 crystalline crustal units and 2 lithospheric mantle units. The corresponding surfaces are 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. The model is a result of a combined workflow consisting of 3-D structural, gravity and thermal modelling applied to derive the 3-D thermal configuration. The top surface elevations and thicknesses of corresponding layers of the 3-D-D model are provided as ASCII files, one for each individual layer of the model. The columns in each file are identical: the Easting is given in the “X COORD (UTM Zone 32N)”, the Northing is in the “Y COORD (UTM Zone 32N)”, the top surface elevation of each layer is given as "TOP (m.a.s.l)", the thickness of each layer is given as "THICKNESS (m)". Complete Anikiev, Denis GFZ German Research Centre for Geosciences, Department Geosystems, Section Basin Modelling Scientist denis.anikiev@gfz-potsdam.de www.gfz-potsdam.de/staff/denis.anikiev informtion pointOfContact Germany Upper Rhine Graben Molasse Basin Central European Basin System Sediment Thickness Crustal Thickness Mantle Variscan Domains Baltic Shield Tauern Body North German Basin Rhenish Massif Netherlands Denmark Czech Republic Alps Vosges Massif Black Forest Massif Bohemian Massif Hesse Depression Ore Mountains Mohorovičić Discontinuity Lithosphere-Asthenosphere Boundary Saar–Nahe Basin Austria Switzerland France EARTH SCIENCE EARTH SCIENCE > LAND SURFACE EARTH SCIENCE > SOLID EARTH EARTH SCIENCE > SOLID EARTH > GEOTHERMAL DYNAMICS > GEOTHERMAL ENERGY EARTH SCIENCE > SOLID EARTH > GEOTHERMAL DYNAMICS > GEOTHERMAL TEMPERATURE EARTH SCIENCE > SOLID EARTH > GRAVITY/GRAVITATIONAL FIELD EARTH SCIENCE > SOLID EARTH > TECTONICS EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > STRATIGRAPHIC SEQUENCE EARTH SCIENCE SERVICES > MODELS EARTH SCIENCE SERVICES > MODELS > GEOLOGIC/TECTONIC/PALEOCLIMATE MODELS EARTH SCIENCE SERVICES > MODELS > LAND SURFACE MODELS NASA/GCMD Earth Science Keywords publication environment > geophysical environment geological process lithosphere GEMET - INSPIRE themes, version 1.0 publication CC BY 4.0 CC BY 4.0 10.1016/j.tecto.2013.04.023 DOI IsDerivedFrom 10.1007/s00531-014-1132-4 DOI IsDerivedFrom 10.1016/j.tecto.2016.11.013 DOI IsDerivedFrom 10.7289/V5C8276M DOI IsDerivedFrom 10.1016/j.tecto.2018.07.001 DOI IsDerivedFrom 10.1007/s00531-005-0513-0 DOI References 10.1016/s0040-1951(99)00248-6 DOI References 10.1029/2006jb004687 DOI References 10.5194/se-8-921-2017 DOI References 10.1016/j.chemer.2010.05.017 DOI References 10.1016/0040-1951(88)90073-x DOI References 10.1016/0040-1951(92)90371-c DOI References 10.1111/j.1365-246X.2010.04548.x DOI References 10.1190/1.1442546 DOI References 10.5194/essd-11-647-2019 DOI References 10.1007/s00531-010-0526-1 DOI References 10.1016/j.tecto.2012.06.030 DOI References 10.1016/j.tecto.2011.07.001 DOI References 10.1016/s0040-1951(99)00235-8 DOI References 10.1186/s40517-015-0038-0 DOI References 10.1016/j.marpetgeo.2014.03.009 DOI References 10.1007/s12665-013-2679-2 DOI References 10.1016/j.tecto.2010.05.003 DOI References 10.5281/zenodo.999400 DOI References 10.5194/adgeo-49-225-2019 DOI IsSupplementTo eng geoscientificInformation The model area covers the whole territory of Germany, it spans 1000 km in North-South and 643 km in East-West direction. Coordinates are given in UTM zone 32 coordinate system (in meters). 5.7 15.2 46.8 55.9 http://doi.org/10.5880/GFZ.4.5.2019.005 WWW:LINK-1.0-http--link Data Access - DOI Data Access - DOI information The applied morel creation workflow comprises (1) structural modelling to correlate the lithostratigraphic units derived from the different input models, followed by (2) a validation of the derived configuration with 3-D gravity modelling and, lastly, (3) the calculation of the conductive thermal field. The main challenge in joining the three existing models was to identify layers of corresponding lithostratigraphy and to merge these for the whole 3-D-D model area. Therefore, we revisited published seismological data to overcome inconsistencies across the boundaries of the input models.