Seismoacoustic effects of the Hovsgol earthquake (Mw = 4.9) of December 5, 2014
The results of study of the Hovsgol earthquake with M w = 4.9, which occurred on December 5, 2014, in the northern part of Hovsgol Lake in Mongolia, are presented. An infrasonic signal of ~140 s long was recorded by the Tory infrasonic station for the first time for the Baikal Rift System. On the ba...
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| Veröffentlicht in: | Doklady earth sciences 2017-12, Vol.477 (2), p.1494-1497 |
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| creator | Dobrynina, A. A. Sankov, V. A. Chechelnitsky, V. V. Tcydypova, L. R. German, V. I. |
| description | The results of study of the Hovsgol earthquake with
M
w
= 4.9, which occurred on December 5, 2014, in the northern part of Hovsgol Lake in Mongolia, are presented. An infrasonic signal of ~140 s long was recorded by the Tory infrasonic station for the first time for the Baikal Rift System. On the basis of the source parameters and focal mechanism of this earthquake determined, displacements in the epicentral zone of the Hovsgol earthquake are modeled. It is shown that they could not have produced an infrasonic sound. The use of acceptable values of group velocities of infrasonic waves (0.28–0.35 km/s) demonstrates that the signal source was located approximately midway between the Tory station and the epicenter of the Hovsgol earthquake, indicating it was a secondary source. Based on the data on the azimuth and arrival time of the acoustic wave at the Tory station, the location of this secondary source is determined to have been on the northern slopes of the Khamar Daban Range. The infrasonic signal formed most likely by interaction between seismic waves from the earthquake and the mountain relief. |
| doi_str_mv | 10.1134/S1028334X17120248 |
| format | Article |
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M
w
= 4.9, which occurred on December 5, 2014, in the northern part of Hovsgol Lake in Mongolia, are presented. An infrasonic signal of ~140 s long was recorded by the Tory infrasonic station for the first time for the Baikal Rift System. On the basis of the source parameters and focal mechanism of this earthquake determined, displacements in the epicentral zone of the Hovsgol earthquake are modeled. It is shown that they could not have produced an infrasonic sound. The use of acceptable values of group velocities of infrasonic waves (0.28–0.35 km/s) demonstrates that the signal source was located approximately midway between the Tory station and the epicenter of the Hovsgol earthquake, indicating it was a secondary source. Based on the data on the azimuth and arrival time of the acoustic wave at the Tory station, the location of this secondary source is determined to have been on the northern slopes of the Khamar Daban Range. The infrasonic signal formed most likely by interaction between seismic waves from the earthquake and the mountain relief.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X17120248</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Acceptable noise levels ; Acoustic waves ; Acoustics ; Analysis ; Azimuth ; Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Geophysics ; Infrasonic waves ; Lakes ; P-waves ; Seismic activity ; Seismic waves ; Seismology ; Slope</subject><ispartof>Doklady earth sciences, 2017-12, Vol.477 (2), p.1494-1497</ispartof><rights>Pleiades Publishing, Ltd. 2017</rights><rights>COPYRIGHT 2017 Springer</rights><rights>Copyright Springer Science & Business Media Dec 2017</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c355t-f1511a4198da486832ab2e3088144c4cc33cedbb315299d9a5b09313ac51d8dc3</citedby><cites>FETCH-LOGICAL-c355t-f1511a4198da486832ab2e3088144c4cc33cedbb315299d9a5b09313ac51d8dc3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1028334X17120248$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1028334X17120248$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Dobrynina, A. A.</creatorcontrib><creatorcontrib>Sankov, V. A.</creatorcontrib><creatorcontrib>Chechelnitsky, V. V.</creatorcontrib><creatorcontrib>Tcydypova, L. R.</creatorcontrib><creatorcontrib>German, V. I.</creatorcontrib><title>Seismoacoustic effects of the Hovsgol earthquake (Mw = 4.9) of December 5, 2014</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>The results of study of the Hovsgol earthquake with
M
w
= 4.9, which occurred on December 5, 2014, in the northern part of Hovsgol Lake in Mongolia, are presented. An infrasonic signal of ~140 s long was recorded by the Tory infrasonic station for the first time for the Baikal Rift System. On the basis of the source parameters and focal mechanism of this earthquake determined, displacements in the epicentral zone of the Hovsgol earthquake are modeled. It is shown that they could not have produced an infrasonic sound. The use of acceptable values of group velocities of infrasonic waves (0.28–0.35 km/s) demonstrates that the signal source was located approximately midway between the Tory station and the epicenter of the Hovsgol earthquake, indicating it was a secondary source. Based on the data on the azimuth and arrival time of the acoustic wave at the Tory station, the location of this secondary source is determined to have been on the northern slopes of the Khamar Daban Range. The infrasonic signal formed most likely by interaction between seismic waves from the earthquake and the mountain relief.</description><subject>Acceptable noise levels</subject><subject>Acoustic waves</subject><subject>Acoustics</subject><subject>Analysis</subject><subject>Azimuth</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Geophysics</subject><subject>Infrasonic waves</subject><subject>Lakes</subject><subject>P-waves</subject><subject>Seismic activity</subject><subject>Seismic waves</subject><subject>Seismology</subject><subject>Slope</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kE1LAzEQhhdRsFZ_gLeAFwW3ZjJJmz14KPWjQqWHKnhbstnZdmvbtMlW8d-bUg-CyBxmmHmfd4ZJknPgHQCUNxPgQiPKN-iB4ELqg6QFCiHVqORhrOM43c2Pk5MQ5pxLKVXWSsYTqsPSGeu2oakto6oi2wTmKtbMiA3dR5i6BSPjm9lma96JXT5_slsmO9nVTnRHlpYFeaaumeAgT5OjyiwCnf3kdvL6cP8yGKaj8ePToD9KLSrVpBUoACMh06WRuqtRmEIQcq1BSiutRbRUFgWCEllWZkYVPENAYxWUurTYTi72vmvvNlsKTT53W7-KK_Noil0BqHpR1dmrpmZBeb2qXOONjVHSsrZuRVUd-30lsNftIe4A2APWuxA8Vfna10vjv3Lg-e7R-Z9HR0bsmRC1qyn5X6f8C30D4VF7bg</recordid><startdate>20171201</startdate><enddate>20171201</enddate><creator>Dobrynina, A. 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A.</au><au>Sankov, V. A.</au><au>Chechelnitsky, V. V.</au><au>Tcydypova, L. R.</au><au>German, V. I.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seismoacoustic effects of the Hovsgol earthquake (Mw = 4.9) of December 5, 2014</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2017-12-01</date><risdate>2017</risdate><volume>477</volume><issue>2</issue><spage>1494</spage><epage>1497</epage><pages>1494-1497</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>The results of study of the Hovsgol earthquake with
M
w
= 4.9, which occurred on December 5, 2014, in the northern part of Hovsgol Lake in Mongolia, are presented. An infrasonic signal of ~140 s long was recorded by the Tory infrasonic station for the first time for the Baikal Rift System. On the basis of the source parameters and focal mechanism of this earthquake determined, displacements in the epicentral zone of the Hovsgol earthquake are modeled. It is shown that they could not have produced an infrasonic sound. The use of acceptable values of group velocities of infrasonic waves (0.28–0.35 km/s) demonstrates that the signal source was located approximately midway between the Tory station and the epicenter of the Hovsgol earthquake, indicating it was a secondary source. Based on the data on the azimuth and arrival time of the acoustic wave at the Tory station, the location of this secondary source is determined to have been on the northern slopes of the Khamar Daban Range. The infrasonic signal formed most likely by interaction between seismic waves from the earthquake and the mountain relief.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1028334X17120248</doi><tpages>4</tpages></addata></record> |
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| subjects | Acceptable noise levels Acoustic waves Acoustics Analysis Azimuth Earth and Environmental Science Earth Sciences Earthquakes Geophysics Infrasonic waves Lakes P-waves Seismic activity Seismic waves Seismology Slope |
| title | Seismoacoustic effects of the Hovsgol earthquake (Mw = 4.9) of December 5, 2014 |
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