Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/157206
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dc.contributor.authorNelson, Alan R.en_US
dc.contributor.authorDuRoss, Christopher B.en_US
dc.contributor.authorWitter, Robert C.en_US
dc.contributor.authorKelsey, Harvey M.en_US
dc.contributor.authorEngelhart, Simon E.en_US
dc.contributor.authorMahan, Shannon A.en_US
dc.contributor.authorGray, Harrison J.en_US
dc.contributor.authorHawkes, Andrea D.en_US
dc.contributor.authorHorton, Benjamin Peteren_US
dc.contributor.authorPadgett, Jason S.en_US
dc.date.accessioned2022-05-10T06:48:44Z-
dc.date.available2022-05-10T06:48:44Z-
dc.date.issued2021-
dc.identifier.citationNelson, A. R., DuRoss, C. B., Witter, R. C., Kelsey, H. M., Engelhart, S. E., Mahan, S. A., Gray, H. J., Hawkes, A. D., Horton, B. P. & Padgett, J. S. (2021). A maximum rupture model for the central and southern Cascadia subduction zone—reassessing ages for coastal evidence of megathrust earthquakes and tsunamis. Quaternary Science Reviews, 261, 106922-. https://dx.doi.org/10.1016/j.quascirev.2021.106922en_US
dc.identifier.issn0277-3791en_US
dc.identifier.urihttps://hdl.handle.net/10356/157206-
dc.description.abstractA new history of great earthquakes (and their tsunamis) for the central and southern Cascadia subduction zone shows more frequent (17 in the past 6700 yr) megathrust ruptures than previous coastal chronologies. The history is based on along-strike correlations of Bayesian age models derived from evaluation of 554 radiocarbon ages that date earthquake evidence at 14 coastal sites. We reconstruct a history that accounts for all dated stratigraphic evidence with the fewest possible ruptures by evaluating the sequence of age models for earthquake or tsunami contacts at each site, comparing the degree of temporal overlap of correlated site age models, considering evidence for closely spaced earthquakes at four sites, and hypothesizing only maximum-length megathrust ruptures. For the past 6700 yr, recurrence for all earthquakes is 370–420 yr. But correlations suggest that ruptures at ∼1.5 ka and ∼1.1 ka were of limited extent (<400 km). If so, post-3-ka recurrence for ruptures extending throughout central and southern Cascadia is 510–540 yr. But the range in the times between earthquakes is large: two instances may be ∼50 yr, whereas the longest are ∼550 and ∼850 yr. The closely spaced ruptures about 1.6 ka may illustrate a pattern common at subduction zones of a long gap ending with a great earthquake rupturing much of the subduction zone, shortly followed by a rupture of more limited extent. The ruptures of limited extent support the continued inclusion of magnitude-8 earthquakes, with longer ruptures near magnitude 9, in assessments of seismic hazard in the region.en_US
dc.description.sponsorshipMinistry of Education (MOE)en_US
dc.description.sponsorshipNational Research Foundation (NRF)en_US
dc.language.isoenen_US
dc.relationMOE2019-T3-1-004en_US
dc.relationMOE2018-T2-1-030en_US
dc.relation.ispartofQuaternary Science Reviewsen_US
dc.rights© 2021 The Author(s). Published by Elsevier Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).en_US
dc.subjectScience::Geologyen_US
dc.titleA maximum rupture model for the central and southern Cascadia subduction zone—reassessing ages for coastal evidence of megathrust earthquakes and tsunamisen_US
dc.typeJournal Articleen
dc.contributor.schoolAsian School of the Environmenten_US
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.identifier.doi10.1016/j.quascirev.2021.106922-
dc.description.versionPublished versionen_US
dc.identifier.scopus2-s2.0-85105692483-
dc.identifier.volume261en_US
dc.identifier.spage106922en_US
dc.subject.keywordsMegathrust Earthquakeen_US
dc.subject.keywordsTsunamisen_US
dc.subject.keywordsCascadiaen_US
dc.subject.keywordsRupture Modelen_US
dc.description.acknowledgementThis work was supported by the Earthquake Hazards Program of the U.S. Geological Survey and by U.S. National Science Foundation Awards EAR-1419824 to Horton, EAR-1419844 to Engelhart, and EAR-9405263 to Kelsey. Kelsey, Witter, Engelhart, and Padgett were also funded by the National Earthquake Hazards Reduction Pro- gram of the U.S. Geological Survey (Award Numbers 02HQGR0056, 02HQGR0057, G14AP00128, G14AP00129, G17AP00028, G19AP00105, and 1434-93-G-2321). Horton’s research was sup- ported by the Earth Observatory of Singapore via its funding from the National Research Foundation Singapore and the Singapore Ministry of Education under the Research Centres of Excellence initiative. Horton was additionally funded by the Singapore Min- istry of Education Academic Research Fund (MOE2019-T3-1-004 and MOE2018-T2-1-030). The National Ocean Sciences Accelerator Mass Spectrometry facility (NOSAMS) at Woods Hole Oceanographic Institution (WHOI) supported the analysis of five 14C AMS samples during Hawkes’ WHOI NOSAMS postdoctoral fellowship. Able field and laboratory assistance was provided by Rich Briggs, Lee Ann Bradley, Zeb Maharrey (all with U.S. Geological Survey, Golden, Colorado), Andy Grand Pre (University of Penn- sylvania), and SeanPaul La Selle (U.S. Geological Survey, Santa Cruz, California). This manuscript was improved through reviews by Lisa Ely (Central Washington University, Ellensburg, Washington), Kate Clark (GNS Science, Lower Hutt, New Zealand), Chris Goldfinger (Oregon State University, Corvallis, Oregon), and an anonymous reviewer. This work comprises Earth Observatory of Singapore contribution number 355.en_US
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