The obtained models of simulated rock types of the post-orogenic Taadikvere and anorogenic Abja and Sigula-like lithologies produced the best-matched models for the Luusika potential field anomaly as their density and magnetic susceptibility are comparable to those of the Luusika source body.
The LH and its metal complexes have been synthesized and characterized by Infrared, proton-NMR, carbon-NMR spectra, elemental analyses, electronic spectra, magnetic susceptibility measurements, thermo gravimetric analyses, scanning electron microscope and cyclic voltammetry.
Thus, the interaction of electromagnetic waves with single-phase multiferroic materials the electric susceptibility ([[chi].sub.e]) and magnetic susceptibility ([[chi].sub.m]) are densities of their dipoles related to the interaction with each other through their magnetic (M) and electric (P) fields, respectively.
(1) To study the magnetization and magnetic susceptibility, we obtain that the critical temperature of the system is [T.sub.c] = 2.3075, [+ or -] 0.00852 and the critical length of the correlation length is v = 1.
Two groups of rocks were used in the modeling, the first composed by igneous rocks taken from the basement of the basin, with an average magnetic susceptibility of 13x[10.sup.-3] SI, while the second group includes the sedimentary rocks taken from the basin presented an average magnetic susceptibility of 0 SI.