@article{oai:nipr.repo.nii.ac.jp:00001637,
 author = {Ueki, Sadato and Kaminuma, Katsutada and Baba, Megumi and Koyama, Etsuro and Kienle, Juergen},
 journal = {Memoirs of National Institute of Polar Research. Special issue},
 month = {Sep},
 note = {P(論文), Mount Erebus is an active volcano with a persistent convecting lava lake at the summit crater, located on Ross Island, Antarctica. Since December 1980 the seismic activity of Mount Erebus has been continuously monitored using a radio-telemetered network of six seismic stations. A 50-day temporary seismic observation was also carried out in the 1982-1983 Antarctic field season. The following seismic activities were observed during this field season : 1) Explosion earthquakes accompanied with Strombolian eruptions from the lava lake occurred at a rate of 0-4 times per day which is slightly lower than the rate in the previous season; 2) an intense earthquake swarm, which is possibly related to the underground movement of magma, occurred in October 1982 near Abbott Peak, 10km northwest of the summit; 3) there were other source regions of seismicity in Ross Island, fairly distant from Mount Erebus to the east.},
 pages = {29--40},
 title = {Seismic activity of Mount Erebus, Antarctica in 1982-1983},
 volume = {33},
 year = {1984}
}