Interference amplitude-phase structure of the narrow-band vector-scalar signals in shallow sea

In shallow water is made the comparative analysis of amplitude and phase of low-frequency narrowband vector-scalar signals in areas of interference maxima and minima (IMA and IMI). The essential difference between the interference structure of sound pressure and the horizontal projections of the vector of the vibrational acceleration (speed) from the characteristics of vertical projections are installed. The stability gradients of the phase in the bands of IMA and the rapid phase change in the bands of IMI, presumably related to the dislocation zones are shows.