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Anomalous seismo-electromagnetic emission related with seismic waves been associated with passage of seismic waves through the place of electromagnetic field observations

System Mathematical Models for the Formation of Signals and Synchronous Interference with the Use of Pulsed Non-explosive Seismic Sources registered by seismic sensors. An algorithm is proposed to reduce the effect of the inhomogeneous upper

Development of a non-explosive water source of seismic acoustic waves with an electromagnetic drive to automate the work in transit zones and in shallow waterThe paper examines the theoretical aspects of the excitation of seismic waves in the aquatic

Surface electromagnetic wave microscopy of opaque samples surface electromagnetic waves (SEW) for the cases when the light signal is detected in the near

Investigation of EM responses under shock impact on rock samples. II. Field experiments are the inclusions of a crystalline piezoelectric excited by seismic wave. The existence of low and high

Physical Basis of Quasi-optimal Seismoacoustic Pulse Generating for Geophysical Prospecting in Shallow Water and Transit Zones. Part 2. The Layout of Aqueous Seismic Source and the Results of ExperimentsThe article discusses theoretical aspects of seismic wave excitation of in the aquatic environ

Lightning triggering related with seismic waves-millisecond electromagnetic pulses associated with passage of seismic waves from earthquakes. The Malaysian LDN data have been

On experimental observations of seismoelectric effect at gas condensate deposit in earth's electromagnetic and seismic noises based on a recording of seismoelectric effect in natural Earth's seismic and electromagnetic fields

Study of the EM responses under shock impacts on rock samples. II. Field experiments are the inclusions of a crystalline piezoelectric excited by seismic wave. The existence of low and high

Features of application of versions of the VSP method for the study of the near-well space [Особенности применения модификаций метода ВСП для изучения околоскважинного пространства] to the presence of permafrost. Consideration of this heterogeneity is important for predicting seismic velocities

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