The Regional Tidal Response of the Geophysical Medium
The results of long-term experimental observations of tidal deformations of the Earth’s crust are reported. These studies have been conducted with the use of the unique laser interferometer of the Sternberg State Astronomical Institute (GAISh), Moscow State University, installed in the deep undergro...
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| Veröffentlicht in: | Doklady earth sciences 2022-04, Vol.503 (2), p.205-210 |
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| creator | Myasnikov, A. V. Sobisevich, L. E. Likhodeev, D. V. |
| description | The results of long-term experimental observations of tidal deformations of the Earth’s crust are reported. These studies have been conducted with the use of the unique laser interferometer of the Sternberg State Astronomical Institute (GAISh), Moscow State University, installed in the deep underground tunnel of the Baksan Neutrino Observatory. A fifteen-year series of continuous in-situ observations of the lithospheric deformations and the corresponding theoretical calculated values of the tide with the basic lunar wave M
2
being distinguishing have been analyzed. The features of the tidal response have been studied for a given volume of the layered geophysical medium on the basis of the data obtained. Changes in the amplitude and phase parameters of the medium were analyzed taking into consideration the patterns of the seismic process. The possibilities of using the parameters of the tidal response of the geophysical medium as possible indicators of the formation and development of focal structures of regional seismic events were considered. |
| doi_str_mv | 10.1134/S1028334X22040146 |
| format | Article |
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2
being distinguishing have been analyzed. The features of the tidal response have been studied for a given volume of the layered geophysical medium on the basis of the data obtained. Changes in the amplitude and phase parameters of the medium were analyzed taking into consideration the patterns of the seismic process. The possibilities of using the parameters of the tidal response of the geophysical medium as possible indicators of the formation and development of focal structures of regional seismic events were considered.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X22040146</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Celestial bodies ; Deformation ; Earth and Environmental Science ; Earth crust ; Earth Sciences ; Earthquakes ; Geophysics ; Interferometers ; Lasers ; Neutrinos ; Parameters ; Regional development ; Seismic activity</subject><ispartof>Doklady earth sciences, 2022-04, Vol.503 (2), p.205-210</ispartof><rights>Pleiades Publishing, Ltd. 2022. ISSN 1028-334X, Doklady Earth Sciences, 2022, Vol. 503, Part 2, pp. 205–210. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Doklady Rossiiskoi Akademii Nauk. Nauki o Zemle, 2022, Vol. 503, pp. 78–84.</rights><rights>COPYRIGHT 2022 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a260t-f1261b2015f003041dfd3d7f0544772ba32192763be45a3fdd7537470b7fba283</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/S1028334X22040146$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1028334X22040146$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Myasnikov, A. V.</creatorcontrib><creatorcontrib>Sobisevich, L. E.</creatorcontrib><creatorcontrib>Likhodeev, D. V.</creatorcontrib><title>The Regional Tidal Response of the Geophysical Medium</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><description>The results of long-term experimental observations of tidal deformations of the Earth’s crust are reported. These studies have been conducted with the use of the unique laser interferometer of the Sternberg State Astronomical Institute (GAISh), Moscow State University, installed in the deep underground tunnel of the Baksan Neutrino Observatory. A fifteen-year series of continuous in-situ observations of the lithospheric deformations and the corresponding theoretical calculated values of the tide with the basic lunar wave M
2
being distinguishing have been analyzed. The features of the tidal response have been studied for a given volume of the layered geophysical medium on the basis of the data obtained. Changes in the amplitude and phase parameters of the medium were analyzed taking into consideration the patterns of the seismic process. The possibilities of using the parameters of the tidal response of the geophysical medium as possible indicators of the formation and development of focal structures of regional seismic events were considered.</description><subject>Celestial bodies</subject><subject>Deformation</subject><subject>Earth and Environmental Science</subject><subject>Earth crust</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Geophysics</subject><subject>Interferometers</subject><subject>Lasers</subject><subject>Neutrinos</subject><subject>Parameters</subject><subject>Regional development</subject><subject>Seismic activity</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp1kE9LAzEQxYMoWKsfwNuC560z-bPpHkvRKihCreBtyW6SNqXdrMn20G9vygoeRAKTMO_9hpch5BZhgsj4_TsCnTLGPykFDsiLMzJCwTCfMsHP0zvJ-Um_JFcxbgE456IcEbHamGxp1s63apetnE51aWLn22gyb7M-yQvju80xuiZpr0a7w_6aXFi1i-bm5x6Tj8eH1fwpf3lbPM9nL7miBfS5RVpgTQGFBWDAUVvNtLQgOJeS1opRLKksWG24UMxqLQWTXEItba3Sf8bkbpjbBf91MLGvtv4QUtJY0UIIZAVwmlyTwbVWO1O51vo-qCYdbfau8a2xLvVnErCgZUlFAnAAmuBjDMZWXXB7FY4VQnVaZ_VnnYmhAxOTt12b8Bvlf-gbYl5zpg</recordid><startdate>20220401</startdate><enddate>20220401</enddate><creator>Myasnikov, A. V.</creator><creator>Sobisevich, L. E.</creator><creator>Likhodeev, D. V.</creator><general>Pleiades Publishing</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20220401</creationdate><title>The Regional Tidal Response of the Geophysical Medium</title><author>Myasnikov, A. V. ; Sobisevich, L. E. ; Likhodeev, D. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a260t-f1261b2015f003041dfd3d7f0544772ba32192763be45a3fdd7537470b7fba283</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Celestial bodies</topic><topic>Deformation</topic><topic>Earth and Environmental Science</topic><topic>Earth crust</topic><topic>Earth Sciences</topic><topic>Earthquakes</topic><topic>Geophysics</topic><topic>Interferometers</topic><topic>Lasers</topic><topic>Neutrinos</topic><topic>Parameters</topic><topic>Regional development</topic><topic>Seismic activity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Myasnikov, A. V.</creatorcontrib><creatorcontrib>Sobisevich, L. E.</creatorcontrib><creatorcontrib>Likhodeev, D. V.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Doklady earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Myasnikov, A. V.</au><au>Sobisevich, L. E.</au><au>Likhodeev, D. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Regional Tidal Response of the Geophysical Medium</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2022-04-01</date><risdate>2022</risdate><volume>503</volume><issue>2</issue><spage>205</spage><epage>210</epage><pages>205-210</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>The results of long-term experimental observations of tidal deformations of the Earth’s crust are reported. These studies have been conducted with the use of the unique laser interferometer of the Sternberg State Astronomical Institute (GAISh), Moscow State University, installed in the deep underground tunnel of the Baksan Neutrino Observatory. A fifteen-year series of continuous in-situ observations of the lithospheric deformations and the corresponding theoretical calculated values of the tide with the basic lunar wave M
2
being distinguishing have been analyzed. The features of the tidal response have been studied for a given volume of the layered geophysical medium on the basis of the data obtained. Changes in the amplitude and phase parameters of the medium were analyzed taking into consideration the patterns of the seismic process. The possibilities of using the parameters of the tidal response of the geophysical medium as possible indicators of the formation and development of focal structures of regional seismic events were considered.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1028334X22040146</doi><tpages>6</tpages></addata></record> |
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| subjects | Celestial bodies Deformation Earth and Environmental Science Earth crust Earth Sciences Earthquakes Geophysics Interferometers Lasers Neutrinos Parameters Regional development Seismic activity |
| title | The Regional Tidal Response of the Geophysical Medium |
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