Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5000
DC Field | Value | Language |
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dc.contributor.authorall | Gavrilov, V.; Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | en |
dc.contributor.authorall | Bogomolov, L.; Institute of Marine Geology and Geophysics Far East Branch, of the Russian Academy of Science, Yuzhno-Sakhalinsk, Russia | en |
dc.contributor.authorall | Morozova, Y.; Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | en |
dc.contributor.authorall | Storcheus, A.; Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | en |
dc.date.accessioned | 2009-04-01T10:03:48Z | en |
dc.date.available | 2009-04-01T10:03:48Z | en |
dc.date.issued | 2008-10 | en |
dc.identifier.uri | http://hdl.handle.net/2122/5000 | en |
dc.description.abstract | Continuous geoacoustic emission (GAE) measurements were acquired using a three-component geophone placed in a borehole at a depth of near 1000 m at Petropavlovsk-Kamchatsky starting in August 2000. Using geophones consisting of magneto-elastic crystal ferromagnetic sensors, and installed at such a depth allows measurement of natural geoacoustic background with signal amplitude less than 1×10-4 m/s3 in frequency band from 3 to 1500 Hz. According to the data from a 4-year survey period the characteristics of diurnal geoacoustic variations change before every earthquake with MLH≥ 5.0 that occurs at a distance of less than 300 km from the observation point or before each earthquake with MLH≥5.5 occurring at distance R≤550 km from the observation point. The changes in GAE regime correlate with the strongest earthquakes that occurred during survey period. Measurements of the natural electromagnetic field of the Earth were carried out simultaneously with the help of an underground electric antenna. The behavior of GAE in aseismic periods appears to be related to the effect of diurnal variations of the natural electromagnetic field. | en |
dc.language.iso | English | en |
dc.relation.ispartof | Annals of Geophysics | en |
dc.relation.ispartofseries | 5-6/51 (2008) | en |
dc.subject | geoacoustic emission | en |
dc.subject | deep borehole, diurnal variation | en |
dc.subject | earthquake occurrence | en |
dc.subject | natural electric field | en |
dc.title | Variations in geoacoustic emissions in a deep borehole and its correlation with seismicity | en |
dc.type | article | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 737-753 | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous | en |
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dc.description.journalType | JCR Journal | en |
dc.description.fulltext | open | en |
dc.contributor.author | Gavrilov, V. | en |
dc.contributor.author | Bogomolov, L. | en |
dc.contributor.author | Morozova, Y. | en |
dc.contributor.author | Storcheus, A. | en |
dc.contributor.department | Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | en |
dc.contributor.department | Institute of Marine Geology and Geophysics Far East Branch, of the Russian Academy of Science, Yuzhno-Sakhalinsk, Russia | en |
dc.contributor.department | Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | en |
dc.contributor.department | Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | - |
crisitem.author.dept | Scientific Station of United Institute for High Temperatures (IVTRAN), Russian Academy of Science, Bishkek, Kyrgyzstan | - |
crisitem.author.dept | Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | - |
crisitem.author.dept | Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Science, Petropavlovsk-Kamchatsky, Russia | - |
crisitem.classification.parent | 04. Solid Earth | - |
Appears in Collections: | Annals of Geophysics |
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