Inhaltsbereich
Publications
(Co) Author: Sodoudi, F.
| Paper (ISI journals) [13] |
Conference Paper [43] |
Thesis/Habil [1] |
Miscellaneous [1] |
All [58] |
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(2013 online first): New constraints on lithospheric thickness of the Iranian plateau using converted waves. Journal of Seismology.
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(2012): Melt infiltration of the lower lithosphere beneath the Tanzania craton and the Albertine rift inferred from S receiver functions. Geochemistry Geophysics Geosystems (G3), 13, Q0AK08.
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(2011): Crustal structure of Northwest Zagros (Kermanshah) and Central Iran (Yazd and Isfahan) using teleseismic Ps converted phases. Journal of Seismology, 15, 2, 341-353.
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(2011): Receiver function images of the base of the lithosphere in the Alboran Sea region. Geophysical Journal International, 187, 2, 1019-1026.
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(2011): High-resolution image of the geometry and thickness of the subducting Nazca lithosphere beneath northern Chile. Journal of Geophysical Research, 116, B04302.
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(2010): Thickness of the central and eastern European lithosphere as seen by S receiver functions. Geophysical Journal International, 181, 2, 604-634.
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(2010): Europe from the bottom up: A statistical examination of the central and northern European lithosphere-asthenosphere boundary from comparing seismological and electromagnetic observations. Lithos, 120, 1-2, 14-29.
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(2010): Lithospheric structure of NW Iran from P and S receiver function. Journal of Seismology, 14, 4, 823-836.
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(2009): Evidence for a missing crustal root and a thin lithosphere beneath the Central Alborz by receiver function studies. Geophysical Journal International, 177, 2, 733-742.
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(2008): Crustal thickness estimation beneath the southern central Andes at 30°S and 36°S from S wave receiver function analysis. Geophysical Journal International, 174, 1, 249-254.
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(2007): An S receiver function analysis of the lithospheric structure in South America. Geophysical Research Letters, 34, L14397.
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(2006): Lithospheric structure of the Aegean obtained from P and S receiver functions. Journal of Geophysical Research, 111, B12307, 1-23.
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(2006): Lithospheric thickness beneath the Dabie Shan, central eastern China from S receiver functions. Geophysical Journal International, 166, 3, 1363-1367.
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(2013): Lithospheric structure of the Iranian Plateau using converted waves. General Assembly European Geosciences Union (Vienna, Austria 2013).| EDOC: 20507 | Abstract |
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(2013): LAB and other lithospheric discontinuities below Cratons. General Assembly European Geosciences Union (Vienna, Austria 2013).| EDOC: 20506 | Abstract |
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(2013): Imaging the LAB and other major lithospheric discontinuities beneath South Africa. General Assembly European Geosciences Union (Vienna, Austria 2013).| EDOC: 20483 | Abstract |
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(2012): The lithosphere-asthenosphere boundary observed with USArray receiver functions and comparison with other regions. General Assembly European Geosciences Union (Vienna, Austria 2012).| EDOC: 20610 | Abstract |
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(2012): Estimation of LAB depth in Zagros, Central Iran and Alborz zones using S receiver function method. General Assembly European Geosciences Union (Vienna, Austria 2012).| EDOC: 20613 | Abstract |
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(2012): Imaging the Lithosphere-Asthenosphere Boundary beneath South Africa and Madagascar using S receiver functions. General Assembly European Geosciences Union (Vienna, Austria 2012).| EDOC: 20609 | Abstract |
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(2011): Lessons learned from receiver function analysis: Variation of the seismic discontinuities along the Alboran Sea region. General Assembly European Geosciences Union (Vienna, Austria 2011).| EDOC: 17591 |
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(2011): The Lithosphere-Asthenosphere Boundary (LAB) in China observed with Receiver Functions and Comparison with Western US. AGU 2011 Fall Meeting (San Francisco 2011).| EDOC: 18070 | Abstract |
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(2011): Seismic Receiver Functions and the Lithosphere-Asthenosphere Boundary. 25th IUGG General Assembly (Melbourne 2011).| EDOC: 17588 |
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(2011): A Receiver Function Study in Kope-Dagh (Iran) Using Short Period Data. General Assembly European Geosciences Union (Vienna, Austria 2011).| EDOC: 20553 | Abstract |
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(2010): The Lithosphere-Asthenosphere Boundary (LAB) beneath the Andes seen by S-Receiver Functions.. The Meeting of the Americas (Foz do Iguassu, Brazil 2010).| EDOC: 15325 |
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(2010): Thickness of the subducting Nazca lithosphere in northern Chile as seen by S receiver functions. General Assembly European Geosciences Union (Vienna, Austria 2010).| EDOC: 20598 | Abstract |
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(2009): The crustal structure beneath the northwest of Zagros (Kermanshah region, Iran) using teleseismic receiver functions. General Assembly European Geosciences Union (Vienna, Austria 2009).| EDOC: 13894 | Abstract |
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(2009): Lithospheric structure beneath the Northwest Iran using Ps and Sp converted waves. General Assembly European Geosciences Union (Vienna, Austria 2009).| EDOC: 13895 | Abstract |
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(2009): The International Plate Boundary Observatory Chile (IPOC) in the northern Chile seismic gap. General Assembly European Geosciences Union (Vienna, Austria 2009).| EDOC: 13893 | Abstract |
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(2009): High resolution receiver function Images of the lithosphere beneath the Central Andes between 19°and 24° S using data of Integrated Plate boundary Observatory Chile (IPOC). AGU 2009 Fall Meeting (San Francisco 2009).| EDOC: 14442 | Abstract |
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(2009): Preliminary results of the receiver functions from the EGELADOS network. General Assembly European Geosciences Union (Vienna, Austria 2009).| EDOC: 13896 | Abstract |
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(2008): Moho depth and Vp/Vs ratio beneath the Isfahan network of Iran from analyis of teleseismic P receiver functions.. General Assembly European Geosciences Union (Vienna, Austria 2008).| EDOC: 20537 |
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(2008): Broadband Seismometers are good tsunameter. General Assembly European Geosciences Union (Vienna, Austria 2008).| EDOC: 11365 |
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(2008): The 14 November, 2007 Mw 7,8 Tocopilla, northern Chile earthquake within the lquique seismic gap. AGU 2008 Joint Assembly (Fort Lauderdale, Florida 2008), 68-68.| EDOC: 11353 |
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(2008): The thickness of the European Lithosphere as seen by S receiver functions. General Assembly European Geosciences Union (Vienna, Austria 2008).| EDOC: 20538 |
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(2007): The thickness of European Lithosphere as seen by S receiver functions. General Assembly European Geoscience Union (EGU) (Vienna, Austria 2007).| EDOC: 10694 |
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(2007): Structures of the crust and mantle lithosphere in South America: trying to find the lithosphere-asthenosphere boundary. General Assembly European Geosciences Union (EGU) (Vienna, Austria 2007).| EDOC: 10695 |
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(2007): The crust and lithophere thickness of South America: trying to find the lithosphere-asthenosphere boundary. AGU 2007 Joint Assembly (Acapulco, Mexico 2007).| EDOC: 10696 |
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(2007): High resolution images of the Lithophere-Astenosphere Boundary obtained from S receiver. General Assembly European Geosciences Union (EGU) (Vienna, Austria 2007).| EDOC: 10778 |
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(2007): A study of the tsunami induced seismic signal recorded at broadband stations. General Assembly European Geosciences Union (EGU) (Vienna, Austria 2007).| EDOC: 10983 |
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(2007): A study of the tsunami induced seismic signal recorded at broadband stations. General Assembly European Geosciences Union (EGU) (Vienna, Austria 2007).| EDOC: 11781 |
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(2007): High resolution images of the tsunami induced seismic signal recorded at broadband stations.. 5. International Conference on Seismolgy and Earthquake Engineering (Tehran, Iran 2007).| EDOC: 11780 |
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(2006): Lithospheric thickness beneath the Dabie Shan, central eastern China from S receiver functions. 3rd General Assembly European Geosciences Union (Vienna, Austria 2006).| EDOC: 11266 |
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(2005): Lithospheric structure in the Aegean area and Greece obtainded from P and S receiver function methods. 2nd General Assembly European Geosciences Union (Vienna, Austria 2005).| EDOC: 7290 | Abstract |
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(2004): A receiver function study in Greece and the Hellenic subduction zone. 1st General Assembly European Geosciences Union (Nice, France 2004).| EDOC: 11345 |
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(2004): A receiver function study in Greece and the Hellenic subduction zone. 64. Jahrestagung der Deutschen Geophysikalischen Gesellschaft (Berlin 2004).| EDOC: 11344 |
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(2004): Crustal structure of Central Alborz.. 2nd Franco-Iranian Workshop on Earth Sciences and Seismic Hazard in Iran (Grenoble 2004).| EDOC: 11782 |
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(2004): Structure of the crust and upper mantle in central Alborz using teleseismic receiver functions.. 1st General Assembly European Geosciences Union (Nice, France 2004).| EDOC: 11783 |
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(2004): The crustal and upper mantle structure of the Central Alborz (Iran) using teleseismic receiver functions. 1st General Assembly European Geosciences Union (Nice, France 2004).| EDOC: 11346 |
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(2003): Receiver Function Study of the Hellenic Subduction Zone. AGU 2003 Fall Meeting (San Francisco 2003).| EDOC: 11786 |
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(2003): Structure of the crust in Greece using receiver functions.. EGS-AGU-EUG Joint Assembly (Nice, France 2003).| EDOC: 11788 |
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(2003): Structure of Greece and the Hellenic subduction zone using Receiver Functions.. AGU 2003 Fall Meeting (San Francisco 2003).| EDOC: 11785 |
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(2003): Structure of the crust and upper mantle in central Alborz using teleseismic receiver functions.. The 11th Iranian Geophysical Conference (Tehran, Iran 2003).| EDOC: 11784 |
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(2002): Receiver Function probing of the crust in northern Iran.. AGU 2002 Fall Meeting (San Francisco 2002).| EDOC: 11807 |
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(2002): Struktur der Erdkruste in Griechenland aus Receiver funktionen.. 28. Treffen der AG Seismologie (Potsdam 2002).| EDOC: 11808 |
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(2000): The model of the crust in Central Alborz using dispersed Reyleigh waves.. The Third Meeting of the Asian Seismological Commission and Symposium on 'Seismology Earthquake Hazard Assessment and Earth’s Interior Related Topics' - ASC2000 (Tehran, Iran 2000).| EDOC: 11809 |
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(1999): The sensitivity of the phase and group velocity of Rayleigh waves in respect with the various parameters.. 10th Geophysical Conference of Iran (Tehran, Iran 1999).| EDOC: 11810 |
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(2005): Lithospheric structure of the Aegean obtained from P and S receiver functions.. Scientific Technical Report ; STR 05/15, GeoForschungsZentrum, 167.
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(2003): Structure of the Hellenic Subduction Zone.| EDOC: 11787 |