Anisotropy of the P-wave velocity in the area of Central and External Dinarides (CROSBI ID 467251)
Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | međunarodna recenzija
Podaci o odgovornosti
Herak, Marijan ; Lokmer, Ivan
engleski
Anisotropy of the P-wave velocity in the area of Central and External Dinarides
The anisotropy of the P-wave velocity in the crust and upper mantle of Central and Southern External Dinarides was determined by considering travel-times of Pg and Pn phases recorded on local and regional seismic stations. A total of 4965 Pg and 6833 Pn arrival times from 1027 well-located earthquakes in that area were selected for analysis. The velocity representative for a given azimuth interval was determined by considering differences of travel-times and of ray-paths for all events as reported by stations within this azimuth window. The obtained azimuthal distribution showa pronounced anisotropy both in the upper crust and in upper mantle. The crustal velocities range between 5.8 and 6.3 km/s.
Seismic anisotropy; Dinarides; Croatia
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
Podaci o prilogu
C155-x.
1998.
objavljeno
Podaci o matičnoj publikaciji
Annales Geophysicae Suppl., Part I
EGS
Aberystwyth: Cambrian Printers
Podaci o skupu
23rd General Assembly of EGS
poster
20.04.1998-24.04.1998
Nica, Francuska