Inhaltsbereich
Publications
(Co) Author: Sodoudi, F.
(since 2005) [ All ]
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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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(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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(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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(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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(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): 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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(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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(2005): Lithospheric structure of the Aegean obtained from P and S receiver functions.. Scientific Technical Report ; STR 05/15, GeoForschungsZentrum, 167.