Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/70100
DC FieldValueLanguage
dc.contributor.authorLario, Javieren_US
dc.contributor.authorSpencer, Chrisen_US
dc.contributor.authorBardají, Teresaen_US
dc.contributor.authorMarchante Ortega, Angelen_US
dc.contributor.authorGarduño-monroy, Victor H.en_US
dc.contributor.authorMacias, Jorgeen_US
dc.contributor.authorOrtega, Sergioen_US
dc.date.accessioned2020-02-05T12:52:24Z-
dc.date.accessioned2020-10-21T09:53:52Z-
dc.date.available2020-02-05T12:52:24Z-
dc.date.available2020-10-21T09:53:52Z-
dc.date.issued2019en_US
dc.identifier.issn0037-0746en_US
dc.identifier.otherScopus-
dc.identifier.otherWoS-
dc.identifier.urihttp://hdl.handle.net/10553/70100-
dc.description.abstractThe Yucatan Peninsula, Mexico, has typically been considered a tectonically stable region with little significant seismic activity. The region though, is one that is regularly affected by hurricanes. A detailed survey of ca 100 km of the eastern Yucatan and Cozumel coast identified the presence of ridges containing individual boulders measuring >1 m in length. The boulder ridges reach 5 m in height and their origin is associated with extreme wave event activity. Previously modelled tsunami waves from known seismically active zones in the region (Muertos Thrust Belt and South Caribbean Deformed Belt) are not of sufficient scale in the area of the Yucatan Peninsula to have produced the boulder ridges recorded in this study. The occurrence of hurricanes in this region is more common, but two of the most destructive (Hurricane Gilbert 1988 and Hurricane Wilma 2005) produced coastal waves too small to have created the ridges recorded here. In this paper, a new tsunami model with a source area located on the Motagua/Swan Island Fault System has been generated that indicates a tsunami event may have caused the extreme wave events that resulted in the deposition of the boulder ridges.en_US
dc.languagespaen_US
dc.relation.ispartofSedimentologyen_US
dc.sourceSedimentology [ISSN 0037-0746], (2019)en_US
dc.subject.otherBouldersen_US
dc.subject.otherExtreme Wave Eventen_US
dc.subject.otherPalaeoseismologyen_US
dc.subject.otherTsunamien_US
dc.titleAn extreme wave event in eastern Yucatán, Mexico: Evidence of a palaeotsunami event during the Mayan timesen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1111/sed.12662en_US
dc.identifier.scopus85074754489-
dc.identifier.isi000493010400001-
dc.contributor.authorscopusid6604064621-
dc.contributor.authorscopusid7201519626-
dc.contributor.authorscopusid6602621118-
dc.contributor.authorscopusid57211668053-
dc.contributor.authorscopusid6602775299-
dc.contributor.authorscopusid7007084198-
dc.contributor.authorscopusid57197500140-
dc.identifier.eissn1365-3091-
dc.type2Artículoen_US
dc.contributor.daisngid31488739-
dc.contributor.daisngid30415674-
dc.contributor.daisngid1098404-
dc.contributor.daisngid28965445-
dc.contributor.daisngid31497594-
dc.contributor.daisngid31521285-
dc.contributor.daisngid2695505-
dc.description.numberofpages24en_US
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Lario, J-
dc.contributor.wosstandardWOS:Spencer, C-
dc.contributor.wosstandardWOS:Bardaji, T-
dc.contributor.wosstandardWOS:Marchante, A-
dc.contributor.wosstandardWOS:Garduno-Monroy, VH-
dc.contributor.wosstandardWOS:Macias, J-
dc.contributor.wosstandardWOS:Ortega, S-
dc.date.coverdate2019en_US
dc.identifier.ulpgces
dc.description.sjr1,491
dc.description.jcr3,405
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.orcid0000-0002-7648-3198-
crisitem.author.fullNameMarchante Ortega, Angel-
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