Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3868
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dc.contributor.authorallFirstov, P. P.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russiaen
dc.contributor.authorallYakovleva, V. S.; Tomsk Polytechnic University, Tomsk, Russiaen
dc.contributor.authorallShirokov, V. A.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russiaen
dc.contributor.authorallMalysheva, O. P.; Institute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russiaen
dc.date.accessioned2008-05-19T15:04:25Zen
dc.date.available2008-05-19T15:04:25Zen
dc.date.issued2007-08en
dc.identifier.urihttp://hdl.handle.net/2122/3868en
dc.description.abstractThe comparison of kinematics and dynamic parameters of radon and molecular hydrogen concentration in subsoil air on the stations network at the Petropavlovsk-Kamchatsky geodynamic proving ground with seismicity of the northern flank of the Kuril-Kamchatka subduction zone was fulfilled in the period from July till August 2004. On the basis of correlation analysis of the regional seismicity and variations of radon flux density calculated using the data of gas-discharge counters of STS-6 type and SSNTDs it was shown that the radon mass transfer abnormal variations are conditioned by both regional seismicity in total and the subduction zone of proving ground. The azimuths of «geodeformation waves» coming to the registration points are calculated during clearly expressed anomaly beginnings, which coincide with directions to earthquake epicenters taking place at the same time. The geochemical anomalies recorded are presumptively deformative by nature and can be conditioned by processes of «quasi-viscous» flow of the lithosphere during rearrangement of tectonic stress fields of the subduction zone. The short-term (predicted time Τ <14 days) precursor of the earthquakes swarm was revealed in hydrogen dynamics on August, 4-5 (four earthquakes had M≥5.3 and epicentral distance about 130 km from the Paratunka base station).en
dc.language.isoEnglishen
dc.relation.ispartofAnnals of Geophysicsen
dc.relation.ispartofseries4/50 (2007)en
dc.subjectradonen
dc.subjecthydrogenen
dc.subjectseismicityen
dc.subjectgeodeformation waveen
dc.subjectearthquakeen
dc.titleThe nexus of soil radon and hydrogen dynamics and seismicity of the northern flank of the Kuril-Kamchatka subduction zoneen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoringen
dc.relation.referencesDUBINCHUK, V.T. (1991): Radon as a precursor of earthquakes, in Isotopic Geochemical Precursors of Earthquakes and Volcanic Eruption, Vienna, 37-42. FIRSTOV, P.P. (1999): Monitoring of subsoil radon volumetric activity on Paratunka geothermal system in 1997 - 1998 with the purpose to search for the precursors of strong earthquakes of Kamchatka, Volcanol. Seismol., 6, 1-11 (in Russian). FIRSTOV, P.P. and V.P. RUDAKOV (2003): Results of subsoil radon registration in 1997-2000 on the Petropavlovsk - Kamchatsky geodynamic polygon, Volcanol. Seismol., 1, 26-41 (in Russian). KIM, I.S., A. AHHLEBY and G.H. SIGEL JR. (1997): Observation of the trapping of radioactive inert gas radon on oxide glass surfaces: macroporous scintillating-glassfiber bundle alpha detector, Nucl. Instrum. Methods Phys. Res., A390, 419-422. KING, C.-Y. (1991): Gas-geochemical approaches to earthquake prediction, in Isotopic Geochemical Precursors of Earthquakes and Volcanic Eruption, Vienna, 22-36. LJUBUSHIN, A.A. JR. (1993): The multivariate analysis of time series of systems of geophysical monitoring, Phys. Earth, 1, 103-108 (in Russian). LJUBUSHIN, A.A. JR. (1998): The aggregated signal of systems of low-frequency geophysical monitoring, Izvestiya (Physics of the Solid Earth), 1, 69-74 (in Russian). MORGUNOV, V.A. (2001): The creep of the rocks at a finishing stage of preparation of earthquakes, Izvestiya (Physics of the Solid Earth), 4, 3-11 (in Russian). NIKOLAEV, V.A. and R. ILIÇ (1999): Etched track radiometers in radon measurements: a review, Radiat. Meas., 30, 1-13. NIKOLAEV, V.A., M.G. BUZYNNIY, I.B.VOROBYEV, A.V. GROMOV, A.S. KRIVOKHATSKIY, I.P. LOS, A.V. ZELENSKIY and YU.A. TOMILIN (1993): Application of the track method for radon measurements in Ukraine, Nucl. Tracks Radiat. Meas., 21 (3), 433-436. NOVIKOV, G.F. (1989): The Radiometric Exploration, Lenin grad, pp. 406 (in Russian). RIZNICHENKO, YU.V. (1977): Calculation of speed of deformations at seismic current of mountain weights, Izvestiya (Physics of the Solid Earth), 54-65 (in Russian). RUDAKOV, V.P. (2003): The seismoemanation effects of geological structures, in Problems of Geophysics of XXI Century. The Book 2 (Znanije Publ., Moscow), 95-113 (in Russian). SEREZHNIKOV, A.I. and V.M. ZIMIN (1976): Geological structure of Paratunka geothermal area, influence of separate geological factors on modern geothermal activity, in Hydrothermal Systems and Thermal Fields on Kamchatka, Vladivostok, 115-142 (in Russian). STEINITZ, G., U. VULKAN and B. LANG (1999): Radon flux at the northwestern segment of the Dead Sea (Dead Sea rift) and its relation to earthquakes, Isr. J. Earth Sci., 48, 283-299. STEINITZ, G., Z.B. BEGIN and N. GAZIT-YAARI (2003): Statistically significant relation between radon flux and weak earthquakes in the Dead Sea rift valley, Geology, 6, 505-508. UTKIN, V.I. (2000): Radon and problem of tectonic earthquakes, SOZh, 6 (12), 64-70 (in Russian). YAKOVLEVA, V.S. (2005): A theoretical method for estimating the characteristics of radon transport in homogeneous soil, Ann. Geophysics, 48 (1), 195-198.en
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorFirstov, P. P.en
dc.contributor.authorYakovleva, V. S.en
dc.contributor.authorShirokov, V. A.en
dc.contributor.authorMalysheva, O. P.en
dc.contributor.departmentInstitute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russiaen
dc.contributor.departmentTomsk Polytechnic University, Tomsk, Russiaen
dc.contributor.departmentInstitute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russiaen
dc.contributor.departmentInstitute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russiaen
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
item.fulltextWith Fulltext-
item.openairetypearticle-
item.grantfulltextopen-
crisitem.author.deptInstitute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia-
crisitem.author.deptTomsk Polytechnic University, Tomsk, Russia-
crisitem.author.deptInstitute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia-
crisitem.author.deptInstitute of Volcanology and Seismology FEB RAS, Petropavlovsk-Kamchatsky, Russia-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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