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Upper mantle structure of the Aegean derived from two-station phase velocities of fundamental mode Rayleigh waves

I. Kassaras 1 K. Makropoulos 1 E. Bourova 2 Helle Pedersen 2 Denis Hatzfeld 2 
1 Department of Geophysics and Geothermics
2 LGIT - Laboratoire de Géophysique Interne et Tectonophysique
Abstract : The tectonic- geodynamic setting and the present upper mantle structure of the Aegean area are discussed. It includes an interesting interpretation of data on the spatial distribution of intermediate focal depth earthquakes, fault plane solutions and deep velocity structures, to further investigate active tectonics related to the deep structure of the southern Aegean volcanic arc.
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https://hal-insu.archives-ouvertes.fr/insu-00372759
Contributor : Pascale Talour Connect in order to contact the contributor
Submitted on : Thursday, April 2, 2009 - 12:37:10 PM
Last modification on : Tuesday, October 19, 2021 - 6:58:04 PM

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  • HAL Id : insu-00372759, version 1

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I. Kassaras, K. Makropoulos, E. Bourova, Helle Pedersen, Denis Hatzfeld. Upper mantle structure of the Aegean derived from two-station phase velocities of fundamental mode Rayleigh waves. M. Fytikas ; G. Vougioukalakis. The South Aegean Active Volcanic Arc, Elsevier, pp.19 à 45, 2005, Developments in Volcanology, n°7. ⟨insu-00372759⟩

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