QIAN SHUQING, ZHANG YIQIN, CAO HUIXIN, L ZHIcom cmult. 1986: ELECTROMAGNETIC RADIATION GENERATED BY THE ROCK RUPTURE DURING AN UNDERGROUND EXPLOSION. Acta Seismologica Sinica, 8(3): 301-308.
Citation:
QIAN SHUQING, ZHANG YIQIN, CAO HUIXIN, L ZHIcom cmult. 1986: ELECTROMAGNETIC RADIATION GENERATED BY THE ROCK RUPTURE DURING AN UNDERGROUND EXPLOSION. Acta Seismologica Sinica, 8(3): 301-308.
QIAN SHUQING, ZHANG YIQIN, CAO HUIXIN, L ZHIcom cmult. 1986: ELECTROMAGNETIC RADIATION GENERATED BY THE ROCK RUPTURE DURING AN UNDERGROUND EXPLOSION. Acta Seismologica Sinica, 8(3): 301-308.
Citation:
QIAN SHUQING, ZHANG YIQIN, CAO HUIXIN, L ZHIcom cmult. 1986: ELECTROMAGNETIC RADIATION GENERATED BY THE ROCK RUPTURE DURING AN UNDERGROUND EXPLOSION. Acta Seismologica Sinica, 8(3): 301-308.
ELECTROMAGNETIC RADIATION GENERATED BY THE ROCK RUPTURE DURING AN UNDERGROUND EXPLOSION
Thr.ee groups of electromagnetic pulses were recorded 960 m away from the point of explosion. The principal power-spectrum is about 200 Hz, which corresponds to the rupture of the surface rock of the earth. This is similar to that observed at Suixian (in Hubei province).
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