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Numerical Methods for Seismic Wave Propagation on Regional and GlobalScalesHomepage of Gunnar Jahnke, Finite Difference, (FD) Methods for Global Seismic Wave Propagation
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Homepage of Gunnar Jahnke, Finite Difference, (FD) Methods for Global Seismic Wave Propagation
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Numerical Methods for Seismic Wave Propagation on Regional and GlobalScales | terraemotus.org Reviews
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Homepage of Gunnar Jahnke, Finite Difference, (FD) Methods for Global Seismic Wave Propagation
terraemotus.org
Numerical Methods for Seismic Wave Propagation on Regional and GlobalScales
http://www.terraemotus.org/index.html
For Seismic Wave Propagation. On Regional and Global Scales. Department of Earth and Environmental Sciences,. Geophysics Section, LMU Munich. Last update: 22. June 2013. Numerical Methods for Seismic Wave Propagation on Regional and Global Scales. 3D models is done for fault zones, especially to investigate so called. Which are very sensible on fault structure at depth (for example seismograms see here. The used method is a 3D high-order staggered-grid finite-difference scheme. In contrast to 2D cylindri...
Hitachi Project - Seismic Wave Propagation
http://www.terraemotus.org/HLRB/HLRB_Project.html
3-D Seismic Wave Propagation on a Global and Regional Scale:. Earthquakes, Fault Zones, Volcanoes. Project Leader: Prof. Dr. Heiner Igel, Institute of Geophysics, Ludwig-Maximilians-University, Munich. Involved scientists: Gunnar Jahnke, Michael Ewald, Johannes Ripperger, Tarje Nissen-Meyer, Max Strasser,. Melanie Reichardt, Markus Treml, Guoquan Wang, Gilbert Brietzke, Miko Fohrmann, Falko Bethmann. Wave Propagation in Volcanoes. Simulations of ground motion for likely earthquake scenarios.
FZPaper Jahnke/Igel/Ben-Zion Download
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Gunnar Jahnke, Heiner Igel and Yehuda. Ben-Zion,. Three-dimensional calculations of fault zone guided waves in. Various irregular structures,. Geophys. J. Int. Supplementary material to the paper is available at www.blackwell-publishing.com. Not at blackwell-science.com as referenced in the journal! Http:/ www.blackwell-publishing.co.uk/GJI.
Diplom thesis
http://www.terraemotus.org/dipl_abstr/dipl_eng.html
In my Diplom thesis I am investigating the. Mantle structure beneath the Tonga-Fiji subduction zone. The dataset consists of 306 deep earthquakes from the Tonga-Fiji region from 1978 till 1984 which were registered at the Warramunga Array in North Australia. Most of the events are clearly deeper than 300 km up to a maximum depth of about 650 km. The time windows of the seismograms have a maximum length of 600 seconds. 3) Interpretation and comparison with regional and global models. Raypaths of the phase...
LRZ: Bundeshöchstleistungsrechner 'Hitachi SR8000-F1'
http://www.terraemotus.org/HitachiSR8000descr.html
Quelle: Leibniz-Rechenzentrum (LRZ), Stand: 2005-01-17. LRZ) hatte im ersten Quartal des Jahres 2000 als. Installiert, das Anfang 2002 noch einmal um mehr als die Hälfte weiter ausgebaut wurde. Damit war am LRZ zeitweise der schnellste Rechner Europas verfügbar. Die Entscheidung für diesen Rechner fiel im Sommer 1999 auf der Basis von aktuellen Benchmark-Programmen der Hochleistungsrechner-Benutzer; die Auswahl sollte nämlich zu einem Rechner mit dem besten Kosten-/Nutzenverhältnis für. Gemeinsamer Speic...
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Numerical Methods for Seismic Wave Propagation on Regional and GlobalScales
For Seismic Wave Propagation. On Regional and Global Scales. Department of Earth and Environmental Sciences,. Geophysics Section, LMU Munich. Last update: 22. June 2013. Numerical Methods for Seismic Wave Propagation on Regional and Global Scales. 3D models is done for fault zones, especially to investigate so called. Which are very sensible on fault structure at depth (for example seismograms see here. The used method is a 3D high-order staggered-grid finite-difference scheme. In contrast to 2D cylindri...
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