Abstract
During span of a satellite over zones of deep faults of a lithosphere, the variations of intensity of low-frequency emissions and also bursts (splashes) of low energy electron flows (50 eV and 120 eV) and increase of ambient plasma temperature are observed. On the basis of such stable anomalous measurements on different orbits above the same tectonic frames, the method of a detection of lithospheric areas with various geodynamic activity is revealed.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
