Please use this identifier to cite or link to this item: https://doi.org/10.1016/j.margeo.2007.02.017
DC FieldValue
dc.titleSediments deposited by the 2004 Indian Ocean Tsunami along the Malaysia-Thailand Peninsula
dc.contributor.authorHawkes, A.D.
dc.contributor.authorHorton, B.P.
dc.contributor.authorBird, M.
dc.contributor.authorCowie, S.
dc.contributor.authorLaw, L.
dc.contributor.authorMacgregor, C.
dc.contributor.authorRobinson, R.
dc.contributor.authorGrundy-Warr, C.
dc.contributor.authorTan-Mullins, M.
dc.contributor.authorShau, Hwai A.T.
dc.contributor.authorYasin, Z.
dc.contributor.authorNott, J.
dc.contributor.authorOng, J.E.
dc.contributor.authorRigg, J.
dc.contributor.authorSa, T.T.
dc.contributor.authorAik, L.W.
dc.date.accessioned2011-02-23T06:13:17Z
dc.date.available2011-02-23T06:13:17Z
dc.date.issued2007
dc.identifier.citationHawkes, A.D., Horton, B.P., Bird, M., Cowie, S., Law, L., Macgregor, C., Robinson, R., Grundy-Warr, C., Tan-Mullins, M., Shau, Hwai A.T., Yasin, Z., Nott, J., Ong, J.E., Rigg, J., Sa, T.T., Aik, L.W. (2007). Sediments deposited by the 2004 Indian Ocean Tsunami along the Malaysia-Thailand Peninsula. Marine Geology 242 (1-3) : 169-190. ScholarBank@NUS Repository. https://doi.org/10.1016/j.margeo.2007.02.017
dc.identifier.issn00253227
dc.identifier.urihttp://scholarbank.nus.edu.sg/handle/10635/19827
dc.description.abstractStratigraphy, grain size distribution and foraminiferal assemblages of pre-tsunami and tsunami sediment from the Indian Ocean Tsunami at five sites along the Malaysia-Thailand Peninsula were analyzed to gain information on tsunami sediment source and deposition style. Between three and five stratigraphic units were identified at each site and contained between one and three fining upward sequences reflecting waning flow or pre-backwash deposition. Coarser sand layers reflecting uprush high-energy flow separated the fining upward sequences, with the exception of one site (Sungai Burong), which contained a coarsening upward sequence. All contacts between the pre-tsunami and tsunami sediment were sharp or erosional. Medium and coarse sand dominated all of the tsunami sediment deposits and often contained shell fragments. Foraminiferal assemblages were able to differentiate pre-tsunami sediment from tsunami sediment where no lithological or grain size distribution change was evident. Between two and four foraminiferal zones were identified at each of the five sites and provided estimates of sediment source and wave characteristics. © 2007 Elsevier B.V. All rights reserved.
dc.description.urihttp://libproxy1.nus.edu.sg/login?url=http://dx.doi.org/10.1016/j.margeo.2007.02.017
dc.sourceScopus
dc.subjectforaminifera
dc.subjectgrain size
dc.subjectMalaysia
dc.subjectThailand
dc.subjecttsunami
dc.typeArticle
dc.contributor.departmentGEOGRAPHY
dc.description.doi10.1016/j.margeo.2007.02.017
dc.description.sourcetitleMarine Geology
dc.description.volume242
dc.description.issue1-3
dc.description.page169-190
dc.description.codenMAGEA
dc.identifier.isiut000248857900011
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