par LIVIU CONSTANTINESCU 1, I. CORNEA 2,
D. ENESCU 2
1Chaire de Géophysique, I.P.G.G.,
Bucarest, Romania
2 Institut de Géophysique Appliqué,
Bucarest, Romania
Researches carried out in Romania on the basis of seismological, deep seismic
sounding and gravity data, with a view to determining the structure of the
Earth's crust for the national territory, have led to results, which are to
a great extent contradictory. A comparative analysis of the three categories
of data and a critical study of the methods having provided them have allowed
to identify the causes responsible for their discrepancies and have made it
possible to correct some of the results considered as erroneous. This paper
contours the present state of the problem and summarizes the recent results
of the integration of the geophysical data available at this moment, among
which the most relevant for a quantitative characterization of the structure
of the Earth's crust are those provided by the deep seismic soundings.