A three-dimensional lithospheric-scale thermal model of Germany
Denis Anikiev
CORRESPONDING AUTHOR
GFZ German Research Centre for Geosciences, Department Geosystems,
Section Basin Modelling, Potsdam, Germany
Adrian Lechel
GFZ German Research Centre for Geosciences, Department Geosystems,
Section Basin Modelling, Potsdam, Germany
Technical University of Berlin, Department Geotechnology, Berlin,
Germany
Maria Laura Gomez Dacal
GFZ German Research Centre for Geosciences, Department Geosystems,
Section Basin Modelling, Potsdam, Germany
Judith Bott
GFZ German Research Centre for Geosciences, Department Geosystems,
Section Basin Modelling, Potsdam, Germany
Mauro Cacace
GFZ German Research Centre for Geosciences, Department Geosystems,
Section Basin Modelling, Potsdam, Germany
Magdalena Scheck-Wenderoth
GFZ German Research Centre for Geosciences, Department Geosystems,
Section Basin Modelling, Potsdam, Germany
RWTH Aachen University, Faculty of Georesources and Material
Engineering, Aachen, Germany
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Knowledge about the stress state in the upper crust is of great importance for many economic and scientific questions. However, our knowledge in Germany is limited since available datasets only provide pointwise, incomplete and heterogeneous information. We present the first 3D geomechanical model that provides a continuous description of the contemporary crustal stress state for Germany. The model is calibrated by the orientation of the maximum horizontal stress and stress magnitudes.
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The Earth’s crust beneath the Caribbean Sea formed at about 90 Ma due to large magmatic activity of a mantle plume, which brought molten material up from the deep Earth. By integrating diverse geophysical datasets, we image for the first time two fossil magmatic conduits beneath the Caribbean. The location of these conduits at 90 Ma does not correspond with the present-day Galápagos plume. Either this mantle plume migrated in time or these conduits were formed above another unknown plume.
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Ershad Gholamrezaie, Magdalena Scheck-Wenderoth, Judith Sippel, and Manfred R. Strecker
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Mauro Cacace and Antoine B. Jacquey
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Judith Sippel, Christian Meeßen, Mauro Cacace, James Mechie, Stewart Fishwick, Christian Heine, Magdalena Scheck-Wenderoth, and Manfred R. Strecker
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The Kenya Rift is a zone along which the African continental plate is stretched as evidenced by strong earthquake and volcanic activity. We want to understand the controlling factors of past and future tectonic deformation; hence, we assess the structural and strength configuration of the rift system at the present-day. Data-driven 3-D numerical models show how the inherited composition of the crust and a thermal anomaly in the deep mantle interact to form localised zones of tectonic weakness.
Moritz O. Ziegler, Oliver Heidbach, John Reinecker, Anna M. Przybycin, and Magdalena Scheck-Wenderoth
Solid Earth, 7, 1365–1382, https://doi.org/10.5194/se-7-1365-2016, https://doi.org/10.5194/se-7-1365-2016, 2016
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Subsurface engineering relies on sparsely distributed data points of the stress state of the earth's crust. 3D geomechanical--numerical modelling is applied to estimate the stress state in the entire volume of a large area. We present a multi-stage approach of differently sized models which provide the stress state in an area of interest derived from few and widely scattered data records. Furthermore we demonstrate the changes in reliability of the model depending on different input parameters.
P. Klitzke, J. I. Faleide, M. Scheck-Wenderoth, and J. Sippel
Solid Earth, 6, 153–172, https://doi.org/10.5194/se-6-153-2015, https://doi.org/10.5194/se-6-153-2015, 2015
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We introduce a regional 3-D structural model of the Barents Sea and Kara Sea region which is the first to combine information on five sedimentary units and the crystalline crust as well as the configuration of the lithospheric mantle. By relating the shallow and deep structures for certain tectonic subdomains, we shed new light on possible causative basin-forming mechanisms that we discuss.
Y. Cherubini, M. Cacace, M. Scheck-Wenderoth, and V. Noack
Geoth. Energ. Sci., 2, 1–20, https://doi.org/10.5194/gtes-2-1-2014, https://doi.org/10.5194/gtes-2-1-2014, 2014
Cited articles
Agemar, T., Schellschmidt, R., and Schulz, R.: Subsurface temperature
distribution in Germany, Geothermics, 44, 65–77, 2012.
Amante, C. and Eakins, B. W.: ETOPO1 1 Arc-Minute Global Relief Model:
Procedures, Data Sources and Analysis, NOAA Technical Memorandum NESDIS
NGDC-24, National Geophysical Data Center, NOAA, https://doi.org/10.7289/V5C8276M, 2009.
Anikiev, D., Lechel, A., Gomez, D. M. L., Bott, J., Cacace, M., and Scheck-Wenderoth, M.: 3-D-Deutschland (3-D-D): A three-dimensional lithospheric-scale thermal model of Germany, V.1., GFZ Data Services, https://doi.org/10.5880/GFZ.4.5.2019.005, 2019.
Bayrisches Staatsministerium für Wirtschaft, V. u. I.: Bayerischer
Geothermieatlas – Hydrothermale Energiegewinnung, 104 S, 2004.
Behrmann, J. H., Ziegler, P. A., Schmid, S. M., Heck, B., and Granet, M.:
The EUCOR-URGENT Project – Upper Rhine Graben: evolution and neotectonics,
Int. J. Earth Sci., 94, 505–506,
https://doi.org/10.1007/s00531-005-0513-0, 2005.
Bleibinhaus, F., Beilecke, T., Bram, K., and Gebrande, H.: A seismic
velocity model for the SW Baltic Sea derived from BASIN'96 refraction
seismic data, Tectonophysics, 314, 269–283, https://doi.org/10.1016/s0040-1951(99)00248-6,
1999.
Blundell, D. J., Freeman, R., Mueller, S., and Button, S. (Eds.): A continent revealed: The European Geotraverse, structure and dynamic evolution, Cambridge University Press, 275 p., 1992.
Boigk, H. and Schöneich, H.: The Rhinegraben: geologic history and
neotectonic activity, Approaches to Taphrogenesis, Inter-Union Commission on
Geodynamics, Sci. Rep., 8, 60–71, 1974.
Brückl, E., Bleibinhaus, F., Gosar, A., Grad, M., Guterch, A.,
Hrubcová, P., Keller, G. R., Majdański, M., Šumanovac, F.,
Tiira, T., Yliniemi, J., Hegedűs, E., and Thybo, H.: Crustal structure
due to collisional and escape tectonics in the Eastern Alps region based on
profiles Alp01 and Alp02 from the ALP 2002 seismic experiment, J.
Geophys. Res.-Solid Earth, 112, B6, https://doi.org/10.1029/2006jb004687, 2007.
Cacace, M. and Jacquey, A. B.: Flexible parallel implicit modelling of
coupled thermal–hydraulic–mechanical processes in fractured rocks, Solid
Earth, 8, 921–941, https://doi.org/10.5194/se-8-921-2017, 2017.
Cacace, M., Kaiser, B. O., Lewerenz, B., and Scheck-Wenderoth, M.:
Geothermal energy in sedimentary basins: What we can learn from regional
numerical models, Geochemistry, 70, 33–46, https://doi.org/10.1016/j.chemer.2010.05.017,
2010.
Campos-Enriquez, J. O., Hubral, P., Wenzel, F., Lüschen, E., and Meier,
L.: Gravity and magnetic constraints on deep and intermediate crustal
structure and evolution models for the Rhine Graben, Tectonophysics, 206,
113–135, https://doi.org/10.1016/0040-1951(92)90371-c, 1992.
DiPippo, R.: Geothermal power plants: principles, applications, case studies
and environmental impact, Butterworth-Heinemann, 2012.
DWD Climate Data Center (CDC): Vieljährige mittlere Raster der Lufttemperatur (2m) für Deutschland 1981–2010, Version v1.0., available at:
https://opendata.dwd.de/climate_environment/CDC/grids_germany/multi_annual/air_temperature_mean/, last access: 31 March 2019.
EUGENO-S Working Group: Crustal structure and tectonic evolution european of
the transition between the Baltic Shield and the North German Caledonides
(the EUGENO-S Project), Tectonophysics, 150, 253–348,
https://doi.org/10.1016/0040-1951(88)90073-x, 1988.
Förste, C., Bruinsma, S., Abrikosov, O., Flechtner, F., Marty, J.-C.,
Lemoine, J.-M., Dahle, C., Neumayer, H., Barthelmes, F., and König, R.:
EIGEN-6C4-The latest combined global gravity field model including GOCE data
up to degree and order 1949 of GFZ Potsdam and GRGS Toulouse, EGU general
assembly conference abstracts, 2014.
Freymark, J., Sippel, J., Scheck-Wenderoth, M., Bär, K., Stiller, M.,
Fritsche, J.-G., and Kracht, M.: The deep thermal field of the Upper Rhine
Graben, Tectonophysics, 694, 114–129, https://doi.org/10.1016/j.tecto.2016.11.013, 2017.
Fuchs, S. and Balling, N.: Improving the temperature predictions of
subsurface thermal models by using high-quality input data, Part 2: A case
study from the Danish-German border region, Geothermics, 64, 1–14,
https://doi.org/10.1016/j.geothermics.2016.04.004, 2016.
Gebrande, H.: TRANSALP: concept and main results on the project,
Geologisch-Paläontologischen Mitteilungen, 25, 7–8, 2001.
Geissler, W. H., Sodoudi, F., and Kind, R.: Thickness of the central and
eastern European lithosphere as seen bySreceiver functions, Geophys.
J. Int., 181, 604–634, https://doi.org/10.1111/j.1365-246X.2010.04548.x, 2010.
GeORG-Projektteam: Geopotenziale des tieferen Untergrundes im
Oberrheingraben, Fachlich-Technischer Abschlussbericht des INTERREG-Projekts
GeORG, Teil 1: Ziele und Ergebnisse des Projekts, 103, 2013.
Götze, H. J. and Lahmeyer, B.: Application of three-dimensional
interactive modeling in gravity and magnetics, Geophysics, 53, 1096–1108,
https://doi.org/10.1190/1.1442546, 1988.
Hetényi, G., Plomerová, J., Bianchi, I., Kampfová Exnerová,
H., Bokelmann, G., Handy, M. R., and Babuška, V.: From mountain summits
to roots: Crustal structure of the Eastern Alps and Bohemian Massif along
longitude 13.3∘ E, Tectonophysics, 744, 239–255,
https://doi.org/10.1016/j.tecto.2018.07.001, 2018.
Ince, E. S., Barthelmes, F., Reißland, S., Elger, K., Förste, C., Flechtner, F., and Schuh, H.: ICGEM – 15 years of successful collection and distribution of global gravitational models, associated services, and future plans, Earth Syst. Sci. Data, 11, 647–674, https://doi.org/10.5194/essd-11-647-2019, 2019.
Jacquey, A. and Cacace, M.: GOLEM, a MOOSE-based application, Zenodo,
https://doi.org/10.5281/zenodo.999400, 2017.
Lechel, A.: A geological, three-dimensional, lithospheric scale, structural
model of Germany, Bachelor, Technical University Berlin, Berlin, 53 pp.,
2017.
Lüschen, E., Wenzel, F., Sandmeier, K.-J., Menges, D., Rühl, T.,
Stiller, M., Janoth, W., Keller, F., Söllner, W., and Thomas, R.:
Near-vertical and wide-angle seismic surveys in the Schwarzwald, in: The
German Continental Deep Drilling Program (KTB), Springer, 297–362, 1989.
Majorowicz, J. and Wybraniec, S.: New terrestrial heat flow map of Europe
after regional paleoclimatic correction application, Int. J. Earth Sci., 100, 881–887, https://doi.org/10.1007/s00531-010-0526-1, 2011.
Maystrenko, Y. P. and Scheck-Wenderoth, M.: 3-D lithosphere-scale density
model of the Central European Basin System and adjacent areas,
Tectonophysics, 601, 53–77, https://doi.org/10.1016/j.tecto.2013.04.023, 2013.
Maystrenko, Y. P., Bayer, U., and Scheck-Wenderoth, M.: Salt as a 3-D element
in structural modeling – Example from the Central European Basin System,
Tectonophysics, 591, 62–82, https://doi.org/10.1016/j.tecto.2012.06.030, 2013.
Meissner, R. and Bortfeld, R. K.: DEKORP-Atlas: results of deutsches
kontinentales reflexionsseismisches Programm, Springer, 2014.
Mitterbauer, U., Behm, M., Brückl, E., Lippitsch, R., Guterch, A.,
Keller, G. R., Koslovskaya, E., Rumpfhuber, E.-M., and Šumanovac, F.:
Shape and origin of the East-Alpine slab constrained by the ALPASS
teleseismic model, Tectonophysics, 510, 195–206,
https://doi.org/10.1016/j.tecto.2011.07.001, 2011.
Norden, B., Förster, A., and Balling, N.: Heat flow and lithospheric thermal regime in the Northeast German Basin, Tectonophysics, 460, 215–229, https://doi.org/10.1016/j.tecto.2008.08.022, 2008.
Pharaoh, T. C.: Palaeozoic terranes and their lithospheric boundaries within
the Trans-European Suture Zone (TESZ): a review, Tectonophysics, 314, 17–41,
https://doi.org/10.1016/s0040-1951(99)00235-8, 1999.
Przybycin, A. M., Scheck-Wenderoth, M., and Schneider, M.: Assessment of the
isostatic state and the load distribution of the European Molasse basin by
means of lithospheric-scale 3-D structural and 3-D gravity modelling,
Int. J. Earth Sci., 104, 1405–1424,
https://doi.org/10.1007/s00531-014-1132-4, 2014.
Przybycin, A. M., Scheck-Wenderoth, M., and Schneider, M.: The 3-D conductive
thermal field of the North Alpine Foreland Basin: influence of the deep
structure and the adjacent European Alps, Geotherm. Energy, 3, 17,
https://doi.org/10.1186/s40517-015-0038-0, 2015.
Scheck-Wenderoth, M., Cacace, M., Maystrenko, Y. P., Cherubini, Y., Noack,
V., Kaiser, B. O., Sippel, J., and Björn, L.: Models of heat transport
in the Central European Basin System: Effective mechanisms at different
scales, Mar. Petrol. Geol., 55, 315–331,
https://doi.org/10.1016/j.marpetgeo.2014.03.009, 2014.
Schmidt, S., Götze, H.-J., Fichler, C., and Alvers, M.: IGMAS+ – a new
3-D gravity, FTG and magnetic modeling software, GEO-INFORMATIK Die Welt im
Netz, edited by: Zipf, A., Behncke, K., Hillen, F., and Scheffermeyer, J.,
Akademische Verlagsgesellschaft AKA GmbH, Heidelberg, Germany, 57–63, 2010.
Sippel, J., Fuchs, S., Cacace, M., Braatz, A., Kastner, O., Huenges, E., and
Scheck-Wenderoth, M.: Deep 3-D thermal modelling for the city of Berlin
(Germany), Environ. Earth Sci., 70, 3545–3566,
https://doi.org/10.1007/s12665-013-2679-2, 2013.
Turcotte, D. and Shubert, G.: Geodynamics (2nd ed.), Cambridge University
Press, 2002.
Vilà, M., Fernández, M., and Jiménez-Munt, I.: Radiogenic heat
production variability of some common lithological groups and its
significance to lithospheric thermal modeling, Tectonophysics, 490, 152–164,
https://doi.org/10.1016/j.tecto.2010.05.003, 2010.
Short summary
We have developed a first Germany-wide 3D data-based density and temperature model integrating geoscientific observations and physical processes. The model can serve as a reference for local detailed studies dealing with temperature, pressure, stress, subsidence and sedimentation. Our results help to improve subsurface utilization concepts, reveal current geomechanical conditions crucial for hazard assessment and gather information on viable resources such groundwater and deep geothermal energy.
We have developed a first Germany-wide 3D data-based density and temperature model integrating...