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TRF_2D for Windows - Field Example.
2D inversion results for the VES field data obtained near Sevastoplol (the
Ukraine) with the
Amn + mnB half-Schlumberger combined array (the current electrode spasings
1/3 - 100 m, the distanse between sounding points - 10 m).
The objective of the survey was to study the lambstone massif (the
right-hand part of the cross-section) embedded in the litified clays (the
central and the left-hand part of the cross-section). It is obvious from
the inversion results that the lambstones, being underlayed by the litified
clays, are not the bedrock. According to the geological data, it is likely
that the lambstone block forms the landslide body slipping over the water-saturated
litified clays. The independent interactive 1D interpretation (using the
IPI program by MSU - see the page) results are close to those of 2D inversion.
Alexei A. Bobachev
Dept. of Geophysics, Geological Faculty, MSU
Vorobievy Gory 119899, Moscow, Russia
Phone /fax: (+7-095) 939 49 63
Please feel free to send us