Issue: 10
, Volume: 49
, Уear of publication: 2008
Serial edition: Russian Geology and Geophysics
Pages: 790-802
Abstract
We suggest new inversion techniques for IP-affected TDEM data. The method implies joint inversion of inductive and galvanic measurements, the galvanic array being configured in a way to separate the polarization and induction components of transient responses from a layered polarizable earth. The IP effects turned out to be reducible at a certain receiver configuration, which was predicted theoretically and proved valid in field tests.
