作者: Yu.A. Kopytenko , V.S. Ismaguilov , K. Hattori , M. Hayakawa
DOI: 10.1016/J.PCE.2006.02.004
关键词: Phase velocity 、 Phase (waves) 、 Anomaly (natural sciences) 、 Earth's magnetic field 、 Geophysics 、 Epicenter 、 Position (vector) 、 Geodesy 、 Direction finding 、 Geology
摘要: Abstract Behavior of gradient and phase velocity vectors ULF ( F M > 6) 2003 = 5.8) years. The were determined using the data three high-sensitive three-component magnetic stations situated at a distance ∼5 km from each other (magnetic gradientometer). Two gradientometers installed southeast southwest Tokyo ∼150 km other. It was found that values had anomaly changes 3–4 months before strong EQs. New directions took place in same period – just to forthcoming EQ epicenter. epicenter arouse for vectors. We propose use geomagnetic disturbances as important factors short-term prediction earthquakes.