Use of Waveform Cross Correlation to Reconstruct the Aftershock Sequence of the August 14, 2016, Sakhalin Earthquake
The waveform cross correlation technique is used to detect signals from aftershocks of the ML = 6.1, August 14, 2016, Sakhalin earthquake using regional seismic network data. Regular P - and S -wave phase arrivals are associated with seismic sources; the resulting cross correlation bulletin is compa...
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| Veröffentlicht in: | Seismic instruments 2019-09, Vol.55 (5), p.544-558 |
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| container_title | Seismic instruments |
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| creator | Kitov, I. O. Turuntaev, S. B. Konovalov, A. V. Stepnov, A. A. Pupatenko, V. V. |
| description | The waveform cross correlation technique is used to detect signals from aftershocks of the ML = 6.1, August 14, 2016, Sakhalin earthquake using regional seismic network data. Regular
P
- and
S
-wave phase arrivals are associated with seismic sources; the resulting cross correlation bulletin is compared with a standard seismic bulletin for the same aftershock sequence. An advantage of the cross correlation bulletin is that it has more detected seismic events tied to three or more stations and a lower catalog completeness threshold; even the epicenters of the weakest aftershocks are located with greater accuracy. The exact aftershock locations tend to cluster along a narrow zone related to the Central Sakhalin Fault. |
| doi_str_mv | 10.3103/S0747923919050074 |
| format | Article |
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P
- and
S
-wave phase arrivals are associated with seismic sources; the resulting cross correlation bulletin is compared with a standard seismic bulletin for the same aftershock sequence. An advantage of the cross correlation bulletin is that it has more detected seismic events tied to three or more stations and a lower catalog completeness threshold; even the epicenters of the weakest aftershocks are located with greater accuracy. The exact aftershock locations tend to cluster along a narrow zone related to the Central Sakhalin Fault.</description><identifier>ISSN: 0747-9239</identifier><identifier>EISSN: 1934-7871</identifier><identifier>DOI: 10.3103/S0747923919050074</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Aftershocks ; Cross correlation ; Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Geophysics/Geodesy ; P waves ; S waves ; Seismic activity ; Sequencing ; Wave phase ; Waveforms</subject><ispartof>Seismic instruments, 2019-09, Vol.55 (5), p.544-558</ispartof><rights>Allerton Press, Inc. 2019</rights><rights>Copyright Springer Nature B.V. 2019</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a269t-601b064b26cbac07d75737c205aa70cf1bc8278c17f5c75610eb0cb0b80b51e53</citedby><cites>FETCH-LOGICAL-a269t-601b064b26cbac07d75737c205aa70cf1bc8278c17f5c75610eb0cb0b80b51e53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.3103/S0747923919050074$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.3103/S0747923919050074$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Kitov, I. O.</creatorcontrib><creatorcontrib>Turuntaev, S. B.</creatorcontrib><creatorcontrib>Konovalov, A. V.</creatorcontrib><creatorcontrib>Stepnov, A. A.</creatorcontrib><creatorcontrib>Pupatenko, V. V.</creatorcontrib><title>Use of Waveform Cross Correlation to Reconstruct the Aftershock Sequence of the August 14, 2016, Sakhalin Earthquake</title><title>Seismic instruments</title><addtitle>Seism. Instr</addtitle><description>The waveform cross correlation technique is used to detect signals from aftershocks of the ML = 6.1, August 14, 2016, Sakhalin earthquake using regional seismic network data. Regular
P
- and
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-wave phase arrivals are associated with seismic sources; the resulting cross correlation bulletin is compared with a standard seismic bulletin for the same aftershock sequence. An advantage of the cross correlation bulletin is that it has more detected seismic events tied to three or more stations and a lower catalog completeness threshold; even the epicenters of the weakest aftershocks are located with greater accuracy. The exact aftershock locations tend to cluster along a narrow zone related to the Central Sakhalin Fault.</description><subject>Aftershocks</subject><subject>Cross correlation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Geophysics/Geodesy</subject><subject>P waves</subject><subject>S waves</subject><subject>Seismic activity</subject><subject>Sequencing</subject><subject>Wave phase</subject><subject>Waveforms</subject><issn>0747-9239</issn><issn>1934-7871</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1UEtLAzEQDqJgrf4AbwGvXZ1JNpvdYym-oCBYi8clidluX5s2yQr-e3dbwYN4GobvMd98hFwj3HIEfjcDmcqC8QILENAtJ2SABU8TmUs8JYMeTnr8nFyEsAIQBedsQOI8WOoq-q4-beX8lk68C4FOnPd2o-LSNTQ6-mqNa0L0rYk01paOq2h9qJ1Z05ndt7YxB5MD1C7aECmmI8oAsxGdqXWtNsuG3isf632r1vaSnFVqE-zVzxyS-cP92-Qpmb48Pk_G00SxrIhJBqghSzXLjFYG5IcUkkvDQCglwVSoTc5kblBWwkiRIVgNRoPOQQu0gg_JzdF3512XMsRy5VrfdCdLxgpMsxRS1rHwyDL9695W5c4vt8p_lQhlX275p9xOw46a0HGbhfW_zv-LvgE5onpY</recordid><startdate>20190901</startdate><enddate>20190901</enddate><creator>Kitov, I. O.</creator><creator>Turuntaev, S. B.</creator><creator>Konovalov, A. V.</creator><creator>Stepnov, A. A.</creator><creator>Pupatenko, V. V.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope></search><sort><creationdate>20190901</creationdate><title>Use of Waveform Cross Correlation to Reconstruct the Aftershock Sequence of the August 14, 2016, Sakhalin Earthquake</title><author>Kitov, I. O. ; Turuntaev, S. B. ; Konovalov, A. V. ; Stepnov, A. A. ; Pupatenko, V. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a269t-601b064b26cbac07d75737c205aa70cf1bc8278c17f5c75610eb0cb0b80b51e53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Aftershocks</topic><topic>Cross correlation</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earthquakes</topic><topic>Geophysics/Geodesy</topic><topic>P waves</topic><topic>S waves</topic><topic>Seismic activity</topic><topic>Sequencing</topic><topic>Wave phase</topic><topic>Waveforms</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kitov, I. O.</creatorcontrib><creatorcontrib>Turuntaev, S. B.</creatorcontrib><creatorcontrib>Konovalov, A. V.</creatorcontrib><creatorcontrib>Stepnov, A. A.</creatorcontrib><creatorcontrib>Pupatenko, V. V.</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Seismic instruments</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kitov, I. O.</au><au>Turuntaev, S. B.</au><au>Konovalov, A. V.</au><au>Stepnov, A. A.</au><au>Pupatenko, V. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Use of Waveform Cross Correlation to Reconstruct the Aftershock Sequence of the August 14, 2016, Sakhalin Earthquake</atitle><jtitle>Seismic instruments</jtitle><stitle>Seism. Instr</stitle><date>2019-09-01</date><risdate>2019</risdate><volume>55</volume><issue>5</issue><spage>544</spage><epage>558</epage><pages>544-558</pages><issn>0747-9239</issn><eissn>1934-7871</eissn><abstract>The waveform cross correlation technique is used to detect signals from aftershocks of the ML = 6.1, August 14, 2016, Sakhalin earthquake using regional seismic network data. Regular
P
- and
S
-wave phase arrivals are associated with seismic sources; the resulting cross correlation bulletin is compared with a standard seismic bulletin for the same aftershock sequence. An advantage of the cross correlation bulletin is that it has more detected seismic events tied to three or more stations and a lower catalog completeness threshold; even the epicenters of the weakest aftershocks are located with greater accuracy. The exact aftershock locations tend to cluster along a narrow zone related to the Central Sakhalin Fault.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.3103/S0747923919050074</doi><tpages>15</tpages></addata></record> |
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| issn | 0747-9239 1934-7871 |
| language | eng |
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| source | Springer Nature - Complete Springer Journals |
| subjects | Aftershocks Cross correlation Earth and Environmental Science Earth Sciences Earthquakes Geophysics/Geodesy P waves S waves Seismic activity Sequencing Wave phase Waveforms |
| title | Use of Waveform Cross Correlation to Reconstruct the Aftershock Sequence of the August 14, 2016, Sakhalin Earthquake |
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