1
10˚ 10˚ 12˚ 12˚ 14˚ 14˚ 16˚ 46˚ 46˚ 48˚ 48˚ 50˚ 50˚ 52˚ 54˚ 54˚ 56˚ 56˚ 52˚ 16˚ 55˚ 47˚ 49˚ 51˚ 53˚ 55˚ 47˚ 49˚ 51˚ 53˚ Kiel Copenhagen Malmö Rostock Hanover Magdeburg Leipzig Zurich Salzburg Stuttgart Nuremberg Munich Frankfurt Cologne Dresden Prague Düsseldorf Dortmund Karlsruhe Szczecin Erfurt Strasbourg Berlin Hamburg Bremen Plzeň Nancy Metz Innsbruck Bolzano Bern Geneva Linz Graz Groningen DENMARK S W E D E N P O L A N D C Z E C H R E P U B L I C A U S T R I A I T A LY SWITZERLAND F R A N C E B E L G I U M NETHERLANDS LUXEMBOURG focal mechanism borehole breakouts drilling-induced fractures overcoring borehole slotter hydraulic fractures geological indicators Method Quality Stress Regime A B C D E normal faulting strike-slip faulting thrust faulting unknown regime Stress Map Germany 2016 Citation of this map Reiter, K., Heidbach, O., Müller, B., Reinecker, J., Röckel, T., (2016): Spannungskarte Deutschland 2016, doi:10.5880/WSM.Germany2016 Key references Heidbach, O., Rajabi, M., Reiter, K., Ziegler, M. and the WSM Team, (2016): World Stress Map Database Release 2016. GFZ Data Services, doi:10.5880/WSM.2016.001. Reiter, K., Heidbach, O., Reinecker, J., Müller, B., Röckel, T., (2015): Spannungskarte Deutschland 2015, Erdöl Erdgas Kohle, 131(11), 437-42. Reinecker, J., Tingay, M. R. P., Müller, B., Heidbach, O., (2010): Present- Day Stress Orientation in the Molasse Basin, Tectonophysics, 482(1-4): 129–138, doi:10.1016/j.tecto.2009.07.021 Röckel, T., Lempp, C., (2003): Der Spannungszustand Im Norddeutschen Becken, Erdöl Erdgas Kohle 119(2):73–80. References of used data and software Heidbach, O., Höhne, J., (2008): CASMI - a tool for the visualization of the World Stress Map data base. Computers and Geosciences, 34, 783-791, doi:1016/j.cageo.2007.06.004. Wessel, P., Smith, W.H.F., (1998): New, improved version of Generic Mapping Tools released, Eos Trans., 79 (47), 579, doi:10.1029/98EO00426. Becker, J. J., D. T. Sandwell, W. H. F. Smith, J. Braud, B. Binder, J. Depner, D. Fabre, J. Factor, S. Ingalls, S-H. Kim, R. Ladner, K. Marks, S. Nelson, A. Pharaoh, R. Trimmer, J. Von Rosenberg, G. Wallace, P. Weatherall., (2009): Global Bathymetry and Elevation Data at 30 Arc Seconds Resolution: SRTM30_PLUS, Marine Geodesy, 32(4), 355-371, doi:10.1080/01490410903297766. normal faulting S V > S Hmax > S hmin S V S hmin S Hmax NF strike-slip faulting S Hmax > S V > S hmin Hmax S V S hmin S SS thrust faulting S Hmax > S hmin > S V S V S hmin S Hmax TF Under the assumption, that the vertical stress (S V ) is a principal stress, the orientation of the 3D stress tensor is defined by the orientation oft the maximum horizontal stress (S Hmax ) only. The minimum horizontal stress (S hmin ) is perpendicular to S Hmax . The orientation of S Hmax is illustrated by lines with different length in the map. The length of each line is a measure for the quality of the data, the symbol specifies the method and the colour indicates the stress regime. Data with the lowest quality (E) are illustrated without any further information as a point. Used stress data are part of the World Stress Map (WSM) data- base release 2016 and freely available. Further information about the data, criteria, data analysis and quality ranking be located on the WSM webpage: www.world-stress- map.org. Editors: Karsten Reiter 1 , Oliver Heidbach 2 , Birgit Müller 3 , John Reinecker 4 und Thomas Röckel 5 1 TU Darmstadt, Institut für Angewandte Geowissenschaften (E-Mail: [email protected]), 2 Deutsches GeoForschungsZentrum GFZ, Potsdam, 3 KIT-Institut für Angewandte Geowissenschaften, Karlsruhe, 4 GeoThermal Engineering GmbH, Karlsruhe, 5 Piewak & Partner, Ingenieurbüro für Hydrogeologie und Umweltschutz, Bayreuth 0 10 20 50 km

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Page 1: stress map germany 2016-10-12-ANull-EN - KIT

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Munich

Frankfurt

CologneDresden

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Karlsruhe

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Hamburg

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Linz

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D E N M A R K

S W E D E N

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C Z E C H R E P U B L I C

A U S T R I A

I T A L Y

S W I T Z E R L A N D

F R A N C E

B E L G I U M

N E T H E R L A N D S

LUXEMBOURG

focal mechanismborehole breakoutsdrilling-induced fracturesovercoringborehole slotterhydraulic fracturesgeological indicators

Method Quality Stress RegimeABCDE

normal faulting

strike-slip faulting

thrust faulting

unknown regime

Stress Map Germany 2016

Citation of this mapReiter, K., Heidbach, O., Müller, B., Reinecker, J., Röckel, T., (2016):

Spannungskarte Deutschland 2016, doi:10.5880/WSM.Germany2016

Key referencesHeidbach, O., Rajabi, M., Reiter, K., Ziegler, M. and the WSM Team, (2016):

World Stress Map Database Release 2016. GFZ Data Services, doi:10.5880/WSM.2016.001.

Reiter, K., Heidbach, O., Reinecker, J., Müller, B., Röckel, T., (2015): Spannungskarte Deutschland 2015, Erdöl Erdgas Kohle, 131(11), 437-42.

Reinecker, J., Tingay, M. R. P., Müller, B., Heidbach, O., (2010): Present-Day Stress Orientation in the Molasse Basin, Tectonophysics, 482(1-4): 129–138, doi:10.1016/j.tecto.2009.07.021

Röckel, T., Lempp, C., (2003): Der Spannungszustand Im Norddeutschen Becken, Erdöl Erdgas Kohle 119(2):73–80.

References of used data and softwareHeidbach, O., Höhne, J., (2008): CASMI - a tool for the visualization of the

World Stress Map data base. Computers and Geosciences, 34, 783-791, doi:1016/j.cageo.2007.06.004.

Wessel, P., Smith, W.H.F., (1998): New, improved version of Generic Mapping Tools released, Eos Trans., 79 (47), 579, doi:10.1029/98EO00426.

Becker, J. J., D. T. Sandwell, W. H. F. Smith, J. Braud, B. Binder, J. Depner, D. Fabre, J. Factor, S. Ingalls, S-H. Kim, R. Ladner, K. Marks, S. Nelson, A. Pharaoh, R. Trimmer, J. Von Rosenberg, G. Wallace, P. Weatherall., (2009): Global Bathymetry and Elevation Data at 30 Arc Seconds Resolution: SRTM30_PLUS, Marine Geodesy, 32(4), 355-371, doi:10.1080/01490410903297766.

normal faultingSV > SHmax > Shmin

SV

ShminSHmax

NF

strike-slip faulting SHmax > SV > Shmin

Hmax

SV

ShminS

SS

thrust faulting SHmax > Shmin > SV

SV

ShminSHmax

TF

Under the assumption, that the vertical stress (SV) is a principal stress, the orientation of the 3D stress tensor is defined by the orientation oft the maximum horizontal stress (SHmax) only. The minimum horizontal stress (Shmin) is perpendicular to SHmax. The orientation of SHmax is illustrated by lines with different length in the map. The length of each line is a measure for the quality of the data, the symbol specifies the method and the colour indicates

the stress regime. Data with the lowest quality (E) are illustrated without any further information as a point. Used stress data are part of the World Stress Map (WSM) data- base release 2016 and freely available. Further information about the data, criteria, data analysis and quality ranking be located on the WSM webpage: www.world-stress-map.org.

Editors:Karsten Reiter1, Oliver Heidbach2, Birgit Müller3, John Reinecker4 und Thomas Röckel5

1 TU Darmstadt, Institut für Angewandte Geowissenschaften (E-Mail: [email protected]),2 Deutsches GeoForschungsZentrum GFZ, Potsdam, 3 KIT-Institut für Angewandte Geowissenschaften, Karlsruhe,

4 GeoThermal Engineering GmbH, Karlsruhe, 5 Piewak & Partner, Ingenieurbüro für Hydrogeologie und Umweltschutz, Bayreuth

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