Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1510
AuthorsDrakatos, G.* 
Karantonis, G.* 
Stavrakakis, G. N.* 
TitleP-wave crustal tomography of Greece with use of an accurate two-point ray tracer
Issue DateJan-1997
Series/Report no.40/1
URIhttp://hdl.handle.net/2122/1510
KeywordsGreece
Aegean
tomography
structure
velocity
Subject Classification04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous 
04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy 
AbstractThe three-dimensional velocity structure of the crust in the Aegean sea and the surrounding regions (34.0º-42.OºN, 19.0ºE-29.0ºE) is investigated by inversion of about 10000 residuals of arrival times of P-wave from local events. The resulting velocity structure shows strong horizontal variations due to the complicated crustal structure and the variations of crustal thickness. The northern part of the region generally shows high velocities. In the inner part of the volcanic arc (Southern Aegean area), relatively low velocities are observed, suggesting a large-scale absorption of seismic energy as confirmed by the low seismicity of the region. A low velocity zone was observed along the subduction zone of the region, up to a depth of 4 km. The existence of such a zone could be due to granitic or other intrusions in the crust during the uplift of the region during Alpidic orogenesis.
Appears in Collections:Annals of Geophysics

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