Deep sea in situ excess pore pressure and sediment deformation off NW Sumatra and its relation with the December 26, 2004 Great Sumatra-Andaman Earthquake

The swath bathymetric data acquired during the “Sumatra Aftershocks” cruise from the Sunda trench in the Indian Ocean to the north of the Sumatra Island imaged several scars and deposits. In situ pore pressure measurements using the Ifremer piezometer and coring demonstrate that high excess pore pre...

Full description

Saved in:
Bibliographic Details
Published in:International journal of earth sciences : Geologische Rundschau 2009-06, Vol.98 (4), p.823-837
Main Authors: Sultan, Nabil, Cattaneo, Antonio, Sibuet, Jean-Claude, Schneider, Jean-Luc
Format: Article
Language:English
Subjects:
Bathymetry
Deep sea
Deformation
Earth and Environmental Science
Earth Sciences
Earthquakes
Geochemistry
Geology
Geophysics/Geodesy
Marine
Mineral Resources
Original Paper
Physical oceanography
Pore pressure
Sedimentology
Sediments
Seismic activity
Seismology
Structural Geology
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-a412t-335f3267eedf2552a9fb8394d228a26845cbe7f660ea980caf0f75f2f5afa4f3
cites cdi_FETCH-LOGICAL-a412t-335f3267eedf2552a9fb8394d228a26845cbe7f660ea980caf0f75f2f5afa4f3
container_end_page 837
container_issue 4
container_start_page 823
container_title International journal of earth sciences : Geologische Rundschau
container_volume 98
creator Sultan, Nabil
Cattaneo, Antonio
Sibuet, Jean-Claude
Schneider, Jean-Luc
description The swath bathymetric data acquired during the “Sumatra Aftershocks” cruise from the Sunda trench in the Indian Ocean to the north of the Sumatra Island imaged several scars and deposits. In situ pore pressure measurements using the Ifremer piezometer and coring demonstrate that high excess pore pressure and sediment deformation was generated by a recent event in the scar of the slope failure zone identified by J.T. Henstock and co-authors. This excess pore pressure is localized in the upper sedimentary layers and is not related to an interplate subduction process. Numerical simulations of the hydrological system that take into account the hydro-mechanical properties of the upper sediment layer show that the excess pore pressure and sediment deformations could be generated at the time of the December 26, 2004 Great Sumatra Earthquake.
doi_str_mv 10.1007/s00531-008-0334-z
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_21121814</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1891611641</sourcerecordid><originalsourceid>FETCH-LOGICAL-a412t-335f3267eedf2552a9fb8394d228a26845cbe7f660ea980caf0f75f2f5afa4f3</originalsourceid><addsrcrecordid>eNp1kc1O3DAUha0KpMLQB-juqouumvbazt8sEQy0EioLkLq07iTXncDECbYjfh6lT1tP01IJiZWP7e8cXfsI8V7iZ4lYfQmIhZYZYp2h1nn29EYcyFxXmVal2nvWRf5WHIZwg7g7kAfi1ynzCIEJOgehixPwQ8MhwDh4htEnOSVBrk1Q2_XsIrRsB99T7AYHg7Xw_QdcTWnv6Q_XxQCet_P9fRc3EDcMp9xwv2YPqvwECjGHc88U_zmzY9dSTw5W5OPmbqJbPhL7lraB3_1dF-L6bHV98jW7uDz_dnJ8kVEuVcy0Lmx6ZMXcWlUUipZ2Xetl3ipVkyrrvGjWXNmyRKZljQ1ZtFVhlS3IUm71QnycY0c_3E0coum70PB2S46HKRglpZJ1-q6F-PACvBkm79JoRmGKV7pcJkjOUOOHEDxbM_quJ_9oJJpdU2ZuyqSmzK4p85Q8avaExLqf7P8Hv276DS3Al1s</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>206602369</pqid></control><display><type>article</type><title>Deep sea in situ excess pore pressure and sediment deformation off NW Sumatra and its relation with the December 26, 2004 Great Sumatra-Andaman Earthquake</title><source>Springer Link</source><creator>Sultan, Nabil ; Cattaneo, Antonio ; Sibuet, Jean-Claude ; Schneider, Jean-Luc</creator><creatorcontrib>Sultan, Nabil ; Cattaneo, Antonio ; Sibuet, Jean-Claude ; Schneider, Jean-Luc ; the Sumatra Aftershocks team</creatorcontrib><description>The swath bathymetric data acquired during the “Sumatra Aftershocks” cruise from the Sunda trench in the Indian Ocean to the north of the Sumatra Island imaged several scars and deposits. In situ pore pressure measurements using the Ifremer piezometer and coring demonstrate that high excess pore pressure and sediment deformation was generated by a recent event in the scar of the slope failure zone identified by J.T. Henstock and co-authors. This excess pore pressure is localized in the upper sedimentary layers and is not related to an interplate subduction process. Numerical simulations of the hydrological system that take into account the hydro-mechanical properties of the upper sediment layer show that the excess pore pressure and sediment deformations could be generated at the time of the December 26, 2004 Great Sumatra Earthquake.</description><identifier>ISSN: 1437-3254</identifier><identifier>EISSN: 1437-3262</identifier><identifier>DOI: 10.1007/s00531-008-0334-z</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Bathymetry ; Deep sea ; Deformation ; Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Geochemistry ; Geology ; Geophysics/Geodesy ; Marine ; Mineral Resources ; Original Paper ; Physical oceanography ; Pore pressure ; Sedimentology ; Sediments ; Seismic activity ; Seismology ; Structural Geology</subject><ispartof>International journal of earth sciences : Geologische Rundschau, 2009-06, Vol.98 (4), p.823-837</ispartof><rights>Springer-Verlag 2008</rights><rights>Springer-Verlag 2009</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a412t-335f3267eedf2552a9fb8394d228a26845cbe7f660ea980caf0f75f2f5afa4f3</citedby><cites>FETCH-LOGICAL-a412t-335f3267eedf2552a9fb8394d228a26845cbe7f660ea980caf0f75f2f5afa4f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Sultan, Nabil</creatorcontrib><creatorcontrib>Cattaneo, Antonio</creatorcontrib><creatorcontrib>Sibuet, Jean-Claude</creatorcontrib><creatorcontrib>Schneider, Jean-Luc</creatorcontrib><creatorcontrib>the Sumatra Aftershocks team</creatorcontrib><title>Deep sea in situ excess pore pressure and sediment deformation off NW Sumatra and its relation with the December 26, 2004 Great Sumatra-Andaman Earthquake</title><title>International journal of earth sciences : Geologische Rundschau</title><addtitle>Int J Earth Sci (Geol Rundsch)</addtitle><description>The swath bathymetric data acquired during the “Sumatra Aftershocks” cruise from the Sunda trench in the Indian Ocean to the north of the Sumatra Island imaged several scars and deposits. In situ pore pressure measurements using the Ifremer piezometer and coring demonstrate that high excess pore pressure and sediment deformation was generated by a recent event in the scar of the slope failure zone identified by J.T. Henstock and co-authors. This excess pore pressure is localized in the upper sedimentary layers and is not related to an interplate subduction process. Numerical simulations of the hydrological system that take into account the hydro-mechanical properties of the upper sediment layer show that the excess pore pressure and sediment deformations could be generated at the time of the December 26, 2004 Great Sumatra Earthquake.</description><subject>Bathymetry</subject><subject>Deep sea</subject><subject>Deformation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Marine</subject><subject>Mineral Resources</subject><subject>Original Paper</subject><subject>Physical oceanography</subject><subject>Pore pressure</subject><subject>Sedimentology</subject><subject>Sediments</subject><subject>Seismic activity</subject><subject>Seismology</subject><subject>Structural Geology</subject><issn>1437-3254</issn><issn>1437-3262</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNp1kc1O3DAUha0KpMLQB-juqouumvbazt8sEQy0EioLkLq07iTXncDECbYjfh6lT1tP01IJiZWP7e8cXfsI8V7iZ4lYfQmIhZYZYp2h1nn29EYcyFxXmVal2nvWRf5WHIZwg7g7kAfi1ynzCIEJOgehixPwQ8MhwDh4htEnOSVBrk1Q2_XsIrRsB99T7AYHg7Xw_QdcTWnv6Q_XxQCet_P9fRc3EDcMp9xwv2YPqvwECjGHc88U_zmzY9dSTw5W5OPmbqJbPhL7lraB3_1dF-L6bHV98jW7uDz_dnJ8kVEuVcy0Lmx6ZMXcWlUUipZ2Xetl3ipVkyrrvGjWXNmyRKZljQ1ZtFVhlS3IUm71QnycY0c_3E0coum70PB2S46HKRglpZJ1-q6F-PACvBkm79JoRmGKV7pcJkjOUOOHEDxbM_quJ_9oJJpdU2ZuyqSmzK4p85Q8avaExLqf7P8Hv276DS3Al1s</recordid><startdate>20090601</startdate><enddate>20090601</enddate><creator>Sultan, Nabil</creator><creator>Cattaneo, Antonio</creator><creator>Sibuet, Jean-Claude</creator><creator>Schneider, Jean-Luc</creator><general>Springer-Verlag</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>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7TN</scope></search><sort><creationdate>20090601</creationdate><title>Deep sea in situ excess pore pressure and sediment deformation off NW Sumatra and its relation with the December 26, 2004 Great Sumatra-Andaman Earthquake</title><author>Sultan, Nabil ; Cattaneo, Antonio ; Sibuet, Jean-Claude ; Schneider, Jean-Luc</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a412t-335f3267eedf2552a9fb8394d228a26845cbe7f660ea980caf0f75f2f5afa4f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Bathymetry</topic><topic>Deep sea</topic><topic>Deformation</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earthquakes</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><topic>Marine</topic><topic>Mineral Resources</topic><topic>Original Paper</topic><topic>Physical oceanography</topic><topic>Pore pressure</topic><topic>Sedimentology</topic><topic>Sediments</topic><topic>Seismic activity</topic><topic>Seismology</topic><topic>Structural Geology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sultan, Nabil</creatorcontrib><creatorcontrib>Cattaneo, Antonio</creatorcontrib><creatorcontrib>Sibuet, Jean-Claude</creatorcontrib><creatorcontrib>Schneider, Jean-Luc</creatorcontrib><creatorcontrib>the Sumatra Aftershocks team</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database (ProQuest)</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; 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><collection>Oceanic Abstracts</collection><jtitle>International journal of earth sciences : Geologische Rundschau</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sultan, Nabil</au><au>Cattaneo, Antonio</au><au>Sibuet, Jean-Claude</au><au>Schneider, Jean-Luc</au><aucorp>the Sumatra Aftershocks team</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Deep sea in situ excess pore pressure and sediment deformation off NW Sumatra and its relation with the December 26, 2004 Great Sumatra-Andaman Earthquake</atitle><jtitle>International journal of earth sciences : Geologische Rundschau</jtitle><stitle>Int J Earth Sci (Geol Rundsch)</stitle><date>2009-06-01</date><risdate>2009</risdate><volume>98</volume><issue>4</issue><spage>823</spage><epage>837</epage><pages>823-837</pages><issn>1437-3254</issn><eissn>1437-3262</eissn><abstract>The swath bathymetric data acquired during the “Sumatra Aftershocks” cruise from the Sunda trench in the Indian Ocean to the north of the Sumatra Island imaged several scars and deposits. In situ pore pressure measurements using the Ifremer piezometer and coring demonstrate that high excess pore pressure and sediment deformation was generated by a recent event in the scar of the slope failure zone identified by J.T. Henstock and co-authors. This excess pore pressure is localized in the upper sedimentary layers and is not related to an interplate subduction process. Numerical simulations of the hydrological system that take into account the hydro-mechanical properties of the upper sediment layer show that the excess pore pressure and sediment deformations could be generated at the time of the December 26, 2004 Great Sumatra Earthquake.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s00531-008-0334-z</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 1437-3254
ispartof International journal of earth sciences : Geologische Rundschau, 2009-06, Vol.98 (4), p.823-837
issn 1437-3254
1437-3262
language eng
recordid cdi_proquest_miscellaneous_21121814
source Springer Link
subjects Bathymetry
Deep sea
Deformation
Earth and Environmental Science
Earth Sciences
Earthquakes
Geochemistry
Geology
Geophysics/Geodesy
Marine
Mineral Resources
Original Paper
Physical oceanography
Pore pressure
Sedimentology
Sediments
Seismic activity
Seismology
Structural Geology
title Deep sea in situ excess pore pressure and sediment deformation off NW Sumatra and its relation with the December 26, 2004 Great Sumatra-Andaman Earthquake
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-20T20%3A42%3A52IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Deep%20sea%20in%20situ%20excess%20pore%20pressure%20and%20sediment%20deformation%20off%20NW%20Sumatra%20and%20its%20relation%20with%20the%20December%2026,%202004%20Great%20Sumatra-Andaman%20Earthquake&rft.jtitle=International%20journal%20of%20earth%20sciences%20:%20Geologische%20Rundschau&rft.au=Sultan,%20Nabil&rft.aucorp=the%20Sumatra%20Aftershocks%20team&rft.date=2009-06-01&rft.volume=98&rft.issue=4&rft.spage=823&rft.epage=837&rft.pages=823-837&rft.issn=1437-3254&rft.eissn=1437-3262&rft_id=info:doi/10.1007/s00531-008-0334-z&rft_dat=%3Cproquest_cross%3E1891611641%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a412t-335f3267eedf2552a9fb8394d228a26845cbe7f660ea980caf0f75f2f5afa4f3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=206602369&rft_id=info:pmid/&rfr_iscdi=true