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dc.creatorDavis, R.O.
dc.creatorBerrill, J.B.
dc.date2001-06-30
dc.identifierhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/464
dc.identifier10.5459/bnzsee.34.2.91-106
dc.descriptionIn November 1987, two earthquakes occurred near a site in the Imperial Valley, California, where extensive field instrumentation had been placed by the US Geological Survey. The site was part of a wildlife refuge and has come to be called the Wildlife Site, or simply Wildlife. Some controversy arose subsequent to the earthquakes because of concern the field piezometers at the site may not have responded accurately in the second, larger earthquake. In this paper we re-examine the data from both earthquakes in an effort to (i) better understand the response of Wildlife during shaking, (ii) shed some light on the validity of the measured pore pressures from the larger earthquake, and (iii) investigate an alternative hypothesis for how liquefaction may develop.en-US
dc.formatapplication/pdf
dc.languageeng
dc.publisherNew Zealand Society for Earthquake Engineeringen-US
dc.relationhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/464/443
dc.rightsCopyright (c) 2001 R.O. Davis, J.B. Berrillen-US
dc.rightshttps://creativecommons.org/licenses/by/4.0en-US
dc.sourceBulletin of the New Zealand Society for Earthquake Engineering; Vol 34 No 2 (2001); 91-106en-US
dc.source2324-1543
dc.source1174-9857
dc.titleLiquefaction at the Imperial Valley Wildlife Siteen-US
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeArticleen-US


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