Tereblia fault zone

Mathematical relationships for Wiese vectors depending on rectilinear anomalies of conductivity

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.