T. IOSIF and SIEGLINDE IOSIF
Institute of Applied Geophysics, Bucharest
(Abstract)
In the present paper the crustal and mantle structure is studied, by using
the P wave travel times of shallow earthquakes with epicentres in the Romanian
territory.
For Conrad and Mohorovicic discontinuities, in the south-east part of Europe
there were obtained the average values 24.5 km and 36 km, respectively.
The travel times T = f(
)
from = 13° to 92° can be represented by
six straight line segments indicating abrupt velocity changes around 23°,
35°, 50°, 65° and 79°.