Wiese vectors

The sets of Wiese vectors calulated for different periods intervals baylike variations obtained on Regime Geophysical station "Nyzhnje Selyshche" during 1989-2000 years are analyzed For disclosure of these vectors tops distribution tliin structure there offered a special algorithms of multilinear analysis. The Oblained results approve stated earlier suppositions about existence of submeridional electroconductiv zone in vicinity of Tereblia fault in Transcarpathian trough and enabled to suppose some new peculiarities of Carpathian electroconductivity anomaly.

For explanation of anomalous Wiese vectors conduct in the Transcarpathian seismoactive trough earlier we have supposed, that in Tereblia fault zone is localized anomaly of variable conductivity. This caused problem of calculating of own Wiese vector of one of two anomalies when we have values of other anomaly own Wiese vector and theirs total value. In presented work the problem solution is given for model case of rectilinear conductors. Examples of these formulas using are given.