Some peculiarities of Wiese vectors in Transcarpathiam trough and their interpretation
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.