The 2010 Mw 7.8 Mentawai earthquake: Very shallow source of a rare tsunami earthquake determined from tsunami field survey and near-field GPS data

The Mw 7.8 October 2010 Mentawai, Indonesia, earthquake was a “tsunami earthquake,” a rare type of earthquake that generates a tsunami much larger than expected based on the seismic magnitude. It produced a locally devastating tsunami, with runup commonly in excess of 6 m. We examine this event usin...

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Veröffentlicht in:Journal of Geophysical Research: Solid Earth 2012-06, Vol.117 (B6), p.n/a
Hauptverfasser: Hill, Emma M., Borrero, Jose C., Huang, Zhenhua, Qiu, Qiang, Banerjee, Paramesh, Natawidjaja, Danny H., Elosegui, Pedro, Fritz, Hermann M., Suwargadi, Bambang W., Pranantyo, Ignatius Ryan, Li, LinLin, Macpherson, Kenneth A., Skanavis, Vassilis, Synolakis, Costas E., Sieh, Kerry
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container_issue B6
container_start_page
container_title Journal of Geophysical Research: Solid Earth
container_volume 117
creator Hill, Emma M.
Borrero, Jose C.
Huang, Zhenhua
Qiu, Qiang
Banerjee, Paramesh
Natawidjaja, Danny H.
Elosegui, Pedro
Fritz, Hermann M.
Suwargadi, Bambang W.
Pranantyo, Ignatius Ryan
Li, LinLin
Macpherson, Kenneth A.
Skanavis, Vassilis
Synolakis, Costas E.
Sieh, Kerry
description The Mw 7.8 October 2010 Mentawai, Indonesia, earthquake was a “tsunami earthquake,” a rare type of earthquake that generates a tsunami much larger than expected based on the seismic magnitude. It produced a locally devastating tsunami, with runup commonly in excess of 6 m. We examine this event using a combination of high‐rate GPS data, from instruments located on the nearby islands, and a tsunami field survey. The GPS displacement time series are deficient in high‐frequency energy, and show small coseismic displacements (
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It produced a locally devastating tsunami, with runup commonly in excess of 6 m. We examine this event using a combination of high‐rate GPS data, from instruments located on the nearby islands, and a tsunami field survey. The GPS displacement time series are deficient in high‐frequency energy, and show small coseismic displacements (&lt;22 cm horizontal and &lt;4 cm subsidence). The field survey shows that maximum tsunami runup was &gt;16 m. Our modeling results show that the combination of the small GPS displacements and large tsunami can only be explained by high fault slip at very shallow depths, far from the islands and close to the oceanic trench. Inelastic uplift of trench sediments likely contributed to the size of the tsunami. Recent results for the 2011 Mw 9.0 Tohoko‐Oki earthquake have also shown shallow fault slip, but the results from our study, which involves a smaller earthquake, provide much stronger constraints on how shallow the rupture can be, with the majority of slip for the Mentawai earthquake occurring at depths of &lt;6 km. This result challenges the conventional wisdom that the shallow tips of subduction megathrusts are aseismic, and therefore raises important questions both about the mechanical properties of the shallow fault zone and the potential seismic and tsunami hazard of this shallow region. Key Points This event ruptured a very shallow area of the Sunda megathrust This shallow area was previously thought to be aseismic A combination of GPS and tsunami data were required to understand this event</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-9313</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-9356</identifier><identifier>DOI: 10.1029/2012JB009159</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Earth sciences ; Earth, ocean, space ; earthquake ; Earthquakes ; Exact sciences and technology ; Geodetics ; Geophysics ; Global positioning systems ; GPS ; Islands ; Physical oceanography ; Plate tectonics ; Rock deformation ; Seismic activity ; Seismic hazard ; Seismology ; subduction ; Sumatra ; tectonics ; tsunami ; Tsunamis ; Weather hazards</subject><ispartof>Journal of Geophysical Research: Solid Earth, 2012-06, Vol.117 (B6), p.n/a</ispartof><rights>Copyright 2012 by the American Geophysical Union</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3570-23728942fb65876a55291a03e8e54b7791ba2cdf0678984f9e3466f4518f205b3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2012JB009159$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2012JB009159$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=26363709$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Hill, Emma M.</creatorcontrib><creatorcontrib>Borrero, Jose C.</creatorcontrib><creatorcontrib>Huang, Zhenhua</creatorcontrib><creatorcontrib>Qiu, Qiang</creatorcontrib><creatorcontrib>Banerjee, Paramesh</creatorcontrib><creatorcontrib>Natawidjaja, Danny H.</creatorcontrib><creatorcontrib>Elosegui, Pedro</creatorcontrib><creatorcontrib>Fritz, Hermann M.</creatorcontrib><creatorcontrib>Suwargadi, Bambang W.</creatorcontrib><creatorcontrib>Pranantyo, Ignatius Ryan</creatorcontrib><creatorcontrib>Li, LinLin</creatorcontrib><creatorcontrib>Macpherson, Kenneth A.</creatorcontrib><creatorcontrib>Skanavis, Vassilis</creatorcontrib><creatorcontrib>Synolakis, Costas E.</creatorcontrib><creatorcontrib>Sieh, Kerry</creatorcontrib><title>The 2010 Mw 7.8 Mentawai earthquake: Very shallow source of a rare tsunami earthquake determined from tsunami field survey and near-field GPS data</title><title>Journal of Geophysical Research: Solid Earth</title><addtitle>J. Geophys. Res</addtitle><description>The Mw 7.8 October 2010 Mentawai, Indonesia, earthquake was a “tsunami earthquake,” a rare type of earthquake that generates a tsunami much larger than expected based on the seismic magnitude. It produced a locally devastating tsunami, with runup commonly in excess of 6 m. We examine this event using a combination of high‐rate GPS data, from instruments located on the nearby islands, and a tsunami field survey. The GPS displacement time series are deficient in high‐frequency energy, and show small coseismic displacements (&lt;22 cm horizontal and &lt;4 cm subsidence). The field survey shows that maximum tsunami runup was &gt;16 m. Our modeling results show that the combination of the small GPS displacements and large tsunami can only be explained by high fault slip at very shallow depths, far from the islands and close to the oceanic trench. Inelastic uplift of trench sediments likely contributed to the size of the tsunami. Recent results for the 2011 Mw 9.0 Tohoko‐Oki earthquake have also shown shallow fault slip, but the results from our study, which involves a smaller earthquake, provide much stronger constraints on how shallow the rupture can be, with the majority of slip for the Mentawai earthquake occurring at depths of &lt;6 km. This result challenges the conventional wisdom that the shallow tips of subduction megathrusts are aseismic, and therefore raises important questions both about the mechanical properties of the shallow fault zone and the potential seismic and tsunami hazard of this shallow region. 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Geophys. Res</addtitle><date>2012-06</date><risdate>2012</risdate><volume>117</volume><issue>B6</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-9313</issn><eissn>2156-2202</eissn><eissn>2169-9356</eissn><abstract>The Mw 7.8 October 2010 Mentawai, Indonesia, earthquake was a “tsunami earthquake,” a rare type of earthquake that generates a tsunami much larger than expected based on the seismic magnitude. It produced a locally devastating tsunami, with runup commonly in excess of 6 m. We examine this event using a combination of high‐rate GPS data, from instruments located on the nearby islands, and a tsunami field survey. The GPS displacement time series are deficient in high‐frequency energy, and show small coseismic displacements (&lt;22 cm horizontal and &lt;4 cm subsidence). The field survey shows that maximum tsunami runup was &gt;16 m. Our modeling results show that the combination of the small GPS displacements and large tsunami can only be explained by high fault slip at very shallow depths, far from the islands and close to the oceanic trench. Inelastic uplift of trench sediments likely contributed to the size of the tsunami. Recent results for the 2011 Mw 9.0 Tohoko‐Oki earthquake have also shown shallow fault slip, but the results from our study, which involves a smaller earthquake, provide much stronger constraints on how shallow the rupture can be, with the majority of slip for the Mentawai earthquake occurring at depths of &lt;6 km. This result challenges the conventional wisdom that the shallow tips of subduction megathrusts are aseismic, and therefore raises important questions both about the mechanical properties of the shallow fault zone and the potential seismic and tsunami hazard of this shallow region. Key Points This event ruptured a very shallow area of the Sunda megathrust This shallow area was previously thought to be aseismic A combination of GPS and tsunami data were required to understand this event</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2012JB009159</doi><tpages>21</tpages><oa>free_for_read</oa></addata></record>
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source Wiley Online Library; Wiley Online Library Journals; Wiley-Blackwell AGU Digital Archive; Alma/SFX Local Collection
subjects Earth sciences
Earth, ocean, space
earthquake
Earthquakes
Exact sciences and technology
Geodetics
Geophysics
Global positioning systems
GPS
Islands
Physical oceanography
Plate tectonics
Rock deformation
Seismic activity
Seismic hazard
Seismology
subduction
Sumatra
tectonics
tsunami
Tsunamis
Weather hazards
title The 2010 Mw 7.8 Mentawai earthquake: Very shallow source of a rare tsunami earthquake determined from tsunami field survey and near-field GPS data
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