Relationship Between Seismic Moment and Source Duration for Seismogenic Earthquakes in Taiwan: Implications for the Product of Static Stress Drop and the Cube of Rupture Velocity
A systematic analysis of the source duration ( τ ) and seismic moment ( M 0 ) for seismogenic earthquakes ( M W 5.5–7.1) in the Taiwan region was completed by using a teleseismic P -wave inversion method. Irrespective of the source self-similarity, the M 0 – τ relationship derived in this study had...
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| Veröffentlicht in: | Pure and applied geophysics 2020-07, Vol.177 (7), p.3191-3203 |
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| container_title | Pure and applied geophysics |
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| creator | Hwang, Ruey-Der Ho, Cheng-Ying Lin, Tzu-Wei Chang, Wen-Yen Huang, Yi-Ling Lin, Cai-Yi Lin, Chiung-Yao |
| description | A systematic analysis of the source duration (
τ
) and seismic moment (
M
0
) for seismogenic earthquakes (
M
W
5.5–7.1) in the Taiwan region was completed by using a teleseismic
P
-wave inversion method. Irrespective of the source self-similarity, the
M
0
–
τ
relationship derived in this study had a power-law form, namely
M
0
∝
τ
3
, under the assumption that Δ
σV
r
3
is constant following a circular fault model (Δ
σ
: static stress drop;
V
r
: rupture velocity). For Taiwan’s earthquakes, the derived
M
0
–
τ
relationship not only provides information to predict the source duration of large earthquakes, but also probes the rupture features of seismogenic earthquakes. That is, there are different rupture patterns for earthquakes, but the product Δ
σV
r
3
remains nearly constant. |
| doi_str_mv | 10.1007/s00024-020-02429-9 |
| format | Article |
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τ
) and seismic moment (
M
0
) for seismogenic earthquakes (
M
W
5.5–7.1) in the Taiwan region was completed by using a teleseismic
P
-wave inversion method. Irrespective of the source self-similarity, the
M
0
–
τ
relationship derived in this study had a power-law form, namely
M
0
∝
τ
3
, under the assumption that Δ
σV
r
3
is constant following a circular fault model (Δ
σ
: static stress drop;
V
r
: rupture velocity). For Taiwan’s earthquakes, the derived
M
0
–
τ
relationship not only provides information to predict the source duration of large earthquakes, but also probes the rupture features of seismogenic earthquakes. That is, there are different rupture patterns for earthquakes, but the product Δ
σV
r
3
remains nearly constant.</description><identifier>ISSN: 0033-4553</identifier><identifier>EISSN: 1420-9136</identifier><identifier>DOI: 10.1007/s00024-020-02429-9</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Duration ; Earth and Environmental Science ; Earth Sciences ; Earthquake prediction ; Earthquakes ; Geophysics/Geodesy ; Legal issues ; P waves ; Rupture ; Rupturing ; Seismic activity ; Self-similarity ; Velocity</subject><ispartof>Pure and applied geophysics, 2020-07, Vol.177 (7), p.3191-3203</ispartof><rights>Springer Nature Switzerland AG 2020</rights><rights>Springer Nature Switzerland AG 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a342t-8510542f83b65026c376c3aedadd8944464657638cad10914871cf480b0383ab3</citedby><cites>FETCH-LOGICAL-a342t-8510542f83b65026c376c3aedadd8944464657638cad10914871cf480b0383ab3</cites><orcidid>0000-0003-2133-0685</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00024-020-02429-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00024-020-02429-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Hwang, Ruey-Der</creatorcontrib><creatorcontrib>Ho, Cheng-Ying</creatorcontrib><creatorcontrib>Lin, Tzu-Wei</creatorcontrib><creatorcontrib>Chang, Wen-Yen</creatorcontrib><creatorcontrib>Huang, Yi-Ling</creatorcontrib><creatorcontrib>Lin, Cai-Yi</creatorcontrib><creatorcontrib>Lin, Chiung-Yao</creatorcontrib><title>Relationship Between Seismic Moment and Source Duration for Seismogenic Earthquakes in Taiwan: Implications for the Product of Static Stress Drop and the Cube of Rupture Velocity</title><title>Pure and applied geophysics</title><addtitle>Pure Appl. Geophys</addtitle><description>A systematic analysis of the source duration (
τ
) and seismic moment (
M
0
) for seismogenic earthquakes (
M
W
5.5–7.1) in the Taiwan region was completed by using a teleseismic
P
-wave inversion method. Irrespective of the source self-similarity, the
M
0
–
τ
relationship derived in this study had a power-law form, namely
M
0
∝
τ
3
, under the assumption that Δ
σV
r
3
is constant following a circular fault model (Δ
σ
: static stress drop;
V
r
: rupture velocity). For Taiwan’s earthquakes, the derived
M
0
–
τ
relationship not only provides information to predict the source duration of large earthquakes, but also probes the rupture features of seismogenic earthquakes. That is, there are different rupture patterns for earthquakes, but the product Δ
σV
r
3
remains nearly constant.</description><subject>Duration</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquake prediction</subject><subject>Earthquakes</subject><subject>Geophysics/Geodesy</subject><subject>Legal issues</subject><subject>P waves</subject><subject>Rupture</subject><subject>Rupturing</subject><subject>Seismic activity</subject><subject>Self-similarity</subject><subject>Velocity</subject><issn>0033-4553</issn><issn>1420-9136</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kc9qGzEQxkVoIK7TF-hJ0PM2o5X2X2-JnbSBlIQ47VXI2llbji2tJS3Br9UnrOwN9NbDMAzz--aD-Qj5zOArA6iuAgDkIoMcUom8yZozMmEijQ3j5QcyAeA8E0XBL8jHEDYArKqKZkL-PONWReNsWJue3mB8Q7R0gSbsjKY_3Q5tpMq2dOEGr5HOB3_Caef8iLkV2oTeKh_X-0G9YqDG0hdl3pT9Ru93_dbo0eGkiWukT961g47UdXQR006n5jEEOveuP7kdqdmwxCPyPPRx8Eh_49ZpEw-X5LxT24Cf3vuU_Lq7fZn9yB4ev9_Prh8yxUUes7pgUIi8q_myLCAvNa9SKWxV29aNEKIUZVGVvNaqZdAwUVdMd6KGJfCaqyWfki_j3d67_YAhyk36gU2WMr2Y5YUo6ypR-Uhp70Lw2Mnem53yB8lAHrORYzYyZSNP2cgmifgoCgm2K_T_Tv9H9Rcuh5Nw</recordid><startdate>20200701</startdate><enddate>20200701</enddate><creator>Hwang, Ruey-Der</creator><creator>Ho, Cheng-Ying</creator><creator>Lin, Tzu-Wei</creator><creator>Chang, Wen-Yen</creator><creator>Huang, Yi-Ling</creator><creator>Lin, Cai-Yi</creator><creator>Lin, Chiung-Yao</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>M2P</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0003-2133-0685</orcidid></search><sort><creationdate>20200701</creationdate><title>Relationship Between Seismic Moment and Source Duration for Seismogenic Earthquakes in Taiwan: Implications for the Product of Static Stress Drop and the Cube of Rupture Velocity</title><author>Hwang, Ruey-Der ; Ho, Cheng-Ying ; Lin, Tzu-Wei ; Chang, Wen-Yen ; Huang, Yi-Ling ; Lin, Cai-Yi ; Lin, Chiung-Yao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a342t-8510542f83b65026c376c3aedadd8944464657638cad10914871cf480b0383ab3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Duration</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earthquake prediction</topic><topic>Earthquakes</topic><topic>Geophysics/Geodesy</topic><topic>Legal issues</topic><topic>P waves</topic><topic>Rupture</topic><topic>Rupturing</topic><topic>Seismic activity</topic><topic>Self-similarity</topic><topic>Velocity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hwang, Ruey-Der</creatorcontrib><creatorcontrib>Ho, Cheng-Ying</creatorcontrib><creatorcontrib>Lin, Tzu-Wei</creatorcontrib><creatorcontrib>Chang, Wen-Yen</creatorcontrib><creatorcontrib>Huang, Yi-Ling</creatorcontrib><creatorcontrib>Lin, Cai-Yi</creatorcontrib><creatorcontrib>Lin, Chiung-Yao</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</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>Agricultural & Environmental Science 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>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Science Database</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science 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>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Pure and applied geophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hwang, Ruey-Der</au><au>Ho, Cheng-Ying</au><au>Lin, Tzu-Wei</au><au>Chang, Wen-Yen</au><au>Huang, Yi-Ling</au><au>Lin, Cai-Yi</au><au>Lin, Chiung-Yao</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Relationship Between Seismic Moment and Source Duration for Seismogenic Earthquakes in Taiwan: Implications for the Product of Static Stress Drop and the Cube of Rupture Velocity</atitle><jtitle>Pure and applied geophysics</jtitle><stitle>Pure Appl. Geophys</stitle><date>2020-07-01</date><risdate>2020</risdate><volume>177</volume><issue>7</issue><spage>3191</spage><epage>3203</epage><pages>3191-3203</pages><issn>0033-4553</issn><eissn>1420-9136</eissn><abstract>A systematic analysis of the source duration (
τ
) and seismic moment (
M
0
) for seismogenic earthquakes (
M
W
5.5–7.1) in the Taiwan region was completed by using a teleseismic
P
-wave inversion method. Irrespective of the source self-similarity, the
M
0
–
τ
relationship derived in this study had a power-law form, namely
M
0
∝
τ
3
, under the assumption that Δ
σV
r
3
is constant following a circular fault model (Δ
σ
: static stress drop;
V
r
: rupture velocity). For Taiwan’s earthquakes, the derived
M
0
–
τ
relationship not only provides information to predict the source duration of large earthquakes, but also probes the rupture features of seismogenic earthquakes. That is, there are different rupture patterns for earthquakes, but the product Δ
σV
r
3
remains nearly constant.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s00024-020-02429-9</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0003-2133-0685</orcidid></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0033-4553 |
| ispartof | Pure and applied geophysics, 2020-07, Vol.177 (7), p.3191-3203 |
| issn | 0033-4553 1420-9136 |
| language | eng |
| recordid | cdi_proquest_journals_2421254687 |
| source | SpringerLink Journals |
| subjects | Duration Earth and Environmental Science Earth Sciences Earthquake prediction Earthquakes Geophysics/Geodesy Legal issues P waves Rupture Rupturing Seismic activity Self-similarity Velocity |
| title | Relationship Between Seismic Moment and Source Duration for Seismogenic Earthquakes in Taiwan: Implications for the Product of Static Stress Drop and the Cube of Rupture Velocity |
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