Wordmark GFZ Potsdam

Publications

 
(Co) Author: Stromeyer, D.
(since 2003) [ All ]































  • Grünthal, G.; Stromeyer, D. (2003): Direction of recent maximal stress and epicentre map of tectonic earthquakes (maps 5 and 6) : Results of IGCP project 346. Verhandlungen des Naturwissenschaftlichen Vereins in Hamburg, 40, 97-104.


  • Ballani, L.; Wardinski, I.; Stromeyer, D.; Greiner-Mai, H. (2005): Time structure of the 1991 magnetic jerk in the core-mantle boundary zone by inverting global magnetic data supported by satellite measurements. - In: Reigber, C.; Lühr, H.; Schwintzer, P.; Wickert, J. (Eds.), Earth Observation with CHAMP : Results from Three Years in Orbit, Springer, 311-316.






















  • Sørensen, M.; Stromeyer, D.; Grünthal, G. (2008): Attenuation of Macroseismic Intensity - New Attenuation Relations for Active Regions in Europe. 31st General Assembly of the European Seismological Commission - ESC2008 (Crete, Hersonissos 2008).

  • Sørensen, M.; Stromeyer, D.; Grünthal, G. (2008): Estimation of macroseismic intensity - new attenuation and intensity vs. ground motion relations for different parts of Europe. 14th World Conference on Earthquake Engineering (Beijing, China 2008).















  • Ballani, L.; Wardinski, I.; Stromeyer, D.; Greiner-Mai, H. (2004): CMB fluid flow between 1980 and 2000 due to a conductive mantle and for different degrees of the input model data (Gauss coefficients). 9th Symposium on the Study of the Earth's Deep Interior (SEDI) (Garmisch-Partenkirchen, Germany 2004), 27.




  • Stromeyer, D.; Grünthal, G. (2004): Intensity attenuation for seismic zones in Germany considering uncertainties. 29th General Assembly European Seismological Commission (Potsdam 2004), 155.







  • Förster, A.; Förster, H.-J.; Stromeyer, D. (2003): An internally consistent present-day thermo-petrological model of the Erzgebirge crust. Geology Without Frontiers: Magmatic and Metamorphic Evolution of the Central European Variscides (Blansko 2003), 49-50.














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