Upper mantle structure of the Aegean derived from two-station phase velocities of fundamental mode Rayleigh waves - Archive ouverte HAL Access content directly
Book Sections Year : 2005

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

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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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Dates and versions

insu-00372759 , version 1 (02-04-2009)

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  • HAL Id : insu-00372759 , version 1

Cite

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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