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Transient fault slip in Guerrero, southern Mexico
The Guerrero region of southern Mexico has accumulated more than 5 m of relative plate motion since the last major earthquake. In early 1998, a continuous GPS site in Guerrero recorded a transient displacement. Modeling indicates that anomalous fault slip propagated from east to west along‐strike of...
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Published in: | Geophysical research letters 2001-10, Vol.28 (19), p.3753-3756 |
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container_title | Geophysical research letters |
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creator | Lowry, Anthony R. Larson, Kristine M. Kostoglodov, Vladimir Bilham, Roger |
description | The Guerrero region of southern Mexico has accumulated more than 5 m of relative plate motion since the last major earthquake. In early 1998, a continuous GPS site in Guerrero recorded a transient displacement. Modeling indicates that anomalous fault slip propagated from east to west along‐strike of the subduction megathrust. Campaign GPS and leveling data corroborate the model. The moment release was equivalent to an Mw≥6.5 earthquake. No M>5 earthquakes accompanied the event, indicating the frictional regime is velocity‐strengthening at the location of slip. |
doi_str_mv | 10.1029/2001GL013238 |
format | article |
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In early 1998, a continuous GPS site in Guerrero recorded a transient displacement. Modeling indicates that anomalous fault slip propagated from east to west along‐strike of the subduction megathrust. Campaign GPS and leveling data corroborate the model. The moment release was equivalent to an Mw≥6.5 earthquake. No M>5 earthquakes accompanied the event, indicating the frictional regime is velocity‐strengthening at the location of slip.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2001GL013238</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Tectonics. Structural geology. 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Res. Lett</addtitle><description>The Guerrero region of southern Mexico has accumulated more than 5 m of relative plate motion since the last major earthquake. In early 1998, a continuous GPS site in Guerrero recorded a transient displacement. Modeling indicates that anomalous fault slip propagated from east to west along‐strike of the subduction megathrust. Campaign GPS and leveling data corroborate the model. The moment release was equivalent to an Mw≥6.5 earthquake. No M>5 earthquakes accompanied the event, indicating the frictional regime is velocity‐strengthening at the location of slip.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Tectonics. Structural geology. 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Structural geology. Plate tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lowry, Anthony R.</creatorcontrib><creatorcontrib>Larson, Kristine M.</creatorcontrib><creatorcontrib>Kostoglodov, Vladimir</creatorcontrib><creatorcontrib>Bilham, Roger</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lowry, Anthony R.</au><au>Larson, Kristine M.</au><au>Kostoglodov, Vladimir</au><au>Bilham, Roger</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Transient fault slip in Guerrero, southern Mexico</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2001-10-01</date><risdate>2001</risdate><volume>28</volume><issue>19</issue><spage>3753</spage><epage>3756</epage><pages>3753-3756</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The Guerrero region of southern Mexico has accumulated more than 5 m of relative plate motion since the last major earthquake. In early 1998, a continuous GPS site in Guerrero recorded a transient displacement. Modeling indicates that anomalous fault slip propagated from east to west along‐strike of the subduction megathrust. Campaign GPS and leveling data corroborate the model. The moment release was equivalent to an Mw≥6.5 earthquake. No M>5 earthquakes accompanied the event, indicating the frictional regime is velocity‐strengthening at the location of slip.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2001GL013238</doi><tpages>4</tpages></addata></record> |
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subjects | Earth sciences Earth, ocean, space Exact sciences and technology Tectonics. Structural geology. Plate tectonics |
title | Transient fault slip in Guerrero, southern Mexico |
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