Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data—Was the asperity in Miyagi-oki ruptured?
We investigated the crustal deformation associated with the 2011 off the Pacific coast of Tohoku Earthquake ( M 9.0) that occurred on March 11, 2011, along the plate boundary off Tohoku district, northeastern Japan, based on dense GPS observation. Coseismic displacements due to this event were appli...
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| Veröffentlicht in: | Earth, planets, and space planets, and space, 2011-01, Vol.63 (7), p.643-648 |
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| creator | Iinuma, Takeshi Ohzono, Mako Ohta, Yusaku Miura, Satoshi |
| description | We investigated the crustal deformation associated with the 2011 off the Pacific coast of Tohoku Earthquake (
M
9.0) that occurred on March 11, 2011, along the plate boundary off Tohoku district, northeastern Japan, based on dense GPS observation. Coseismic displacements due to this event were applied to estimate the causal interplate slip by means of a geodetic inversion analysis. The major slip area is located around the asperities of the 1981 Miyagi-oki (
M
7.2) and 2003 Fukushima-oki (
M
6.8) earthquakes and the maximum slip is estimated as being up to 35 m. The estimated slip distribution suggests that the asperities of the Miyagi-oki earthquake in 1978 (
M
7.4) that had not been ruptured during the Miyagi-oki earthquake in 2005 were ruptured as a part of the main shock fault of the 2011 off the Pacific coast of Tohoku Earthquake. |
| doi_str_mv | 10.5047/eps.2011.06.013 |
| format | Article |
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M
9.0) that occurred on March 11, 2011, along the plate boundary off Tohoku district, northeastern Japan, based on dense GPS observation. Coseismic displacements due to this event were applied to estimate the causal interplate slip by means of a geodetic inversion analysis. The major slip area is located around the asperities of the 1981 Miyagi-oki (
M
7.2) and 2003 Fukushima-oki (
M
6.8) earthquakes and the maximum slip is estimated as being up to 35 m. The estimated slip distribution suggests that the asperities of the Miyagi-oki earthquake in 1978 (
M
7.4) that had not been ruptured during the Miyagi-oki earthquake in 2005 were ruptured as a part of the main shock fault of the 2011 off the Pacific coast of Tohoku Earthquake.</description><identifier>ISSN: 1343-8832</identifier><identifier>EISSN: 1880-5981</identifier><identifier>DOI: 10.5047/eps.2011.06.013</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Geology ; Geophysics/Geodesy ; Letter</subject><ispartof>Earth, planets, and space, 2011-01, Vol.63 (7), p.643-648</ispartof><rights>The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences; TERRAPUB. 2011</rights><rights>The Society of Geomagnetism and Earth, Planetary and Space Sciences, The Seismological Society of Japan 2011</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a553t-d62f8626ac140116983e15e14530e6aff7cf02166801c8f2acc2e987abf48f423</citedby><cites>FETCH-LOGICAL-a553t-d62f8626ac140116983e15e14530e6aff7cf02166801c8f2acc2e987abf48f423</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.5047/eps.2011.06.013$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.5047/eps.2011.06.013$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,27901,27902,41096,41464,42165,42533,51294,51551</link.rule.ids></links><search><creatorcontrib>Iinuma, Takeshi</creatorcontrib><creatorcontrib>Ohzono, Mako</creatorcontrib><creatorcontrib>Ohta, Yusaku</creatorcontrib><creatorcontrib>Miura, Satoshi</creatorcontrib><title>Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data—Was the asperity in Miyagi-oki ruptured?</title><title>Earth, planets, and space</title><addtitle>Earth Planet Sp</addtitle><description>We investigated the crustal deformation associated with the 2011 off the Pacific coast of Tohoku Earthquake (
M
9.0) that occurred on March 11, 2011, along the plate boundary off Tohoku district, northeastern Japan, based on dense GPS observation. Coseismic displacements due to this event were applied to estimate the causal interplate slip by means of a geodetic inversion analysis. The major slip area is located around the asperities of the 1981 Miyagi-oki (
M
7.2) and 2003 Fukushima-oki (
M
6.8) earthquakes and the maximum slip is estimated as being up to 35 m. The estimated slip distribution suggests that the asperities of the Miyagi-oki earthquake in 1978 (
M
7.4) that had not been ruptured during the Miyagi-oki earthquake in 2005 were ruptured as a part of the main shock fault of the 2011 off the Pacific coast of Tohoku Earthquake.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Letter</subject><issn>1343-8832</issn><issn>1880-5981</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>BENPR</sourceid><recordid>eNp1kb1qHDEUhQeTgB0ndVqBC9vFjPUz0moqYxbHCdjEEIeU4q5G8sq7Oxrraort8hB5gbxaniTabIpgSCHpCr5zOJxbVe8ZbSRtZxduxIZTxhqqGsrEQXXEtKa17DR7VWbRilprwQ-rN4hPlAraKnFU_ZxHdAE3wRJch5H0AXMKiymHOJDoSV46snMt8_5zDzb4QtsImHfEQ1zG1USuIeXl8wQrR87uSNfQc-Iwhw1k15MFYLmL4839F9JDhl_ff3wD_GMIOLoU8paEgdyFLTyGOq4CSdOYp-T6y7fVaw9rdO_-vsfV1w_XD_OP9e3nm0_zq9sapBS57hX3WnEFlrUlr-q0cEw61kpBnQLvZ9ZTzpTSlFntOVjLXadnsPCt9i0Xx9Xp3ndM8Xkq2c0moHXrNQwuTmg6LnhpTXaFPHlBPsUpDSWcYUrKclqpCnWxp2yKiMl5M6ZSR9oaRs1uY6ZszOy6NVSZsrGioHsFFnJ4dOkf3_9IfgMcm5lE</recordid><startdate>20110101</startdate><enddate>20110101</enddate><creator>Iinuma, Takeshi</creator><creator>Ohzono, Mako</creator><creator>Ohta, Yusaku</creator><creator>Miura, Satoshi</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>H8D</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L7M</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope></search><sort><creationdate>20110101</creationdate><title>Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data—Was the asperity in Miyagi-oki ruptured?</title><author>Iinuma, Takeshi ; Ohzono, Mako ; Ohta, Yusaku ; Miura, Satoshi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a553t-d62f8626ac140116983e15e14530e6aff7cf02166801c8f2acc2e987abf48f423</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><topic>Letter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Iinuma, Takeshi</creatorcontrib><creatorcontrib>Ohzono, Mako</creatorcontrib><creatorcontrib>Ohta, Yusaku</creatorcontrib><creatorcontrib>Miura, Satoshi</creatorcontrib><collection>Springer Nature OA/Free Journals</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Aerospace Database</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><jtitle>Earth, planets, and space</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Iinuma, Takeshi</au><au>Ohzono, Mako</au><au>Ohta, Yusaku</au><au>Miura, Satoshi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data—Was the asperity in Miyagi-oki ruptured?</atitle><jtitle>Earth, planets, and space</jtitle><stitle>Earth Planet Sp</stitle><date>2011-01-01</date><risdate>2011</risdate><volume>63</volume><issue>7</issue><spage>643</spage><epage>648</epage><pages>643-648</pages><issn>1343-8832</issn><eissn>1880-5981</eissn><abstract>We investigated the crustal deformation associated with the 2011 off the Pacific coast of Tohoku Earthquake (
M
9.0) that occurred on March 11, 2011, along the plate boundary off Tohoku district, northeastern Japan, based on dense GPS observation. Coseismic displacements due to this event were applied to estimate the causal interplate slip by means of a geodetic inversion analysis. The major slip area is located around the asperities of the 1981 Miyagi-oki (
M
7.2) and 2003 Fukushima-oki (
M
6.8) earthquakes and the maximum slip is estimated as being up to 35 m. The estimated slip distribution suggests that the asperities of the Miyagi-oki earthquake in 1978 (
M
7.4) that had not been ruptured during the Miyagi-oki earthquake in 2005 were ruptured as a part of the main shock fault of the 2011 off the Pacific coast of Tohoku Earthquake.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.5047/eps.2011.06.013</doi><tpages>6</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Earth and Environmental Science Earth Sciences Geology Geophysics/Geodesy Letter |
| title | Coseismic slip distribution of the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0) estimated based on GPS data—Was the asperity in Miyagi-oki ruptured? |
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