By M. Fytikas,G. Vougioukalakis
This publication is a suite of twenty-two chosen papers from the homonymous convention held in September 2003 Milos, Greece. the purpose of the convention used to be to function a discussion board for the presentation and confident dialogue of the cutting-edge and rising matters at the South Aegean Volcanic Arc.
In the 1st a part of the booklet the tectonic- geodynamic surroundings and the current higher mantle constitution of the Aegean sector are mentioned. It comprises a fascinating interpretation of knowledge at the spatial distribution of intermediate focal intensity earthquakes, fault aircraft recommendations and deep pace constructions, to additional examine lively tectonics with regards to the deep constitution of the southern Aegean volcanic arc.
The moment half offers with common volcanological, petrological and tectonic features of the SAAVA proposing an in depth evaluation of volcanological, chemical, isotope and tectonic information, utilizing a large number of new box and laboratory facts. fascinating conclusions are awarded concerning the current volcanic institutions, the volcanic fields position and form in appreciate to the massive tectonic lineaments and the plate motions, the resource of the SAAVA parental magmas.
Presented within the 3rd half is an intensive assessment at the volcanic probability review and the tracking kingdom of the SAAVA facilities. Seismic and geodetic tracking of the Santorini volcano and the new (1995-1998) difficulty of Nisyros volcano are provided and discussed.
The final half bargains with hydrothermal deposits and approaches within the SAAVA, in addition to items and strategies in adjoining components with a selected curiosity and importance that hyperlink them to the SAAVA processes.
*Systematic second look at the geodynamic and tectonic environment of the Aegean energetic volcanic facilities
*Thorough assessment with new info and ideas at the magma resource area, the magma differentiation approaches in either the deep and shallow degrees, and the volcanological approaches similar either to the magma composition and garage intensity in addition to to the tectonic regime of the volcano progress area
*Up thus far estimation of the volcanic threat within the Aegean region, and a close presentation of the current kingdom and the tracking efforts of the South Aegean energetic centers