<rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dct="http://purl.org/dc/terms/" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#">
  <rdf:Description rdf:about="https://doi.org/10.1002/eqe.3286">
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    <dct:isPartOf>Earthquake Engineering &amp;amp; Structural Dynamics</dct:isPartOf>
    <dct:license>Open Access</dct:license>
    <dct:created>2020-06-22</dct:created>
    <dc:description>Summary&lt;p&gt;Megathrust earthquake sequences, comprising mainshocks and triggered aftershocks along the subduction interface and in the overriding crust, can impact multiple buildings and infrastructure in a city. The time between the mainshocks and aftershocks usually is too short to retrofit the structures; therefore, moderate&#65506;&#65408;&#65424;size aftershocks can cause additional damage. To have a better understanding of the impact of aftershocks on city&#65506;&#65408;&#65424;wide seismic risk assessment, a new simulation framework of spatiotemporal seismic hazard and risk assessment of future M9.0 sequences in the Cascadia subduction zone is developed. The simulation framework consists of an epidemic&#65506;&#65408;&#65424;type aftershock sequence (ETAS) model, ground&#65506;&#65408;&#65424;motion model, and state&#65506;&#65408;&#65424;dependent seismic fragility model. The spatiotemporal ETAS model is modified to characterise aftershocks of large and anisotropic M9.0 mainshock ruptures. To account for damage accumulation of wood&#65506;&#65408;&#65424;frame houses due to aftershocks in Victoria, British Columbia, Canada, state&#65506;&#65408;&#65424;dependent fragility curves are implemented. The new simulation framework can be used for quasi&#65506;&#65408;&#65424;real&#65506;&#65408;&#65424;time aftershock hazard and risk assessments and city&#65506;&#65408;&#65424;wide post&#65506;&#65408;&#65424;event risk management.&lt;/p&gt;</dc:description>
    <dc:subject>Mainshock-aftershock sequences</dc:subject>
    <dc:subject>550</dc:subject>
    <dc:subject>seismic risk</dc:subject>
    <dc:subject>Damage accumulation</dc:subject>
    <dc:subject>seismic hazard</dc:subject>
    <dc:subject>Cascadia</dc:subject>
    <dc:subject>City-wide seismic risk</dc:subject>
    <dc:subject>02 engineering and technology</dc:subject>
    <dc:subject>Wood-frame houses</dc:subject>
    <dc:subject>01 natural sciences</dc:subject>
    <dc:subject>aftershocks</dc:subject>
    <dc:subject>0201 civil engineering</dc:subject>
    <dc:subject>earthquake clustering</dc:subject>
    <dc:subject>13. Climate action</dc:subject>
    <dc:subject>Cascadia subduction earthquakes</dc:subject>
    <dc:subject>Spatiotemporal ETAS seismicity model</dc:subject>
    <dc:subject>earthquakes</dc:subject>
    <dc:subject>State-dependent aftershock fragility curves</dc:subject>
    <dc:subject>0105 earth and related environmental sciences</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0001-9093-6694"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-3900-2153"/>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-2430-2631"/>
    <dc:creator>Lizhong Zhang, Katsuichiro Goda, Maximilian J. Werner, Solomon Tesfamariam, </dc:creator>
    <dc:date>2020-06-21</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>Summary&lt;p&gt;Megathrust earthquake sequences, comprising mainshocks and triggered aftershocks along the subduction interface and in the overriding crust, can impact multiple buildings and infrastructure in a city. The time between the mainshocks and aftershocks usually is too short to retrofit the structures; therefore, moderate&#65506;&#65408;&#65424;size aftershocks can cause additional damage. To have a better understanding of the impact of aftershocks on city&#65506;&#65408;&#65424;wide seismic risk assessment, a new simulation framework of spatiotemporal seismic hazard and risk assessment of future M9.0 sequences in the Cascadia subduction zone is developed. The simulation framework consists of an epidemic&#65506;&#65408;&#65424;type aftershock sequence (ETAS) model, ground&#65506;&#65408;&#65424;motion model, and state&#65506;&#65408;&#65424;dependent seismic fragility model. The spatiotemporal ETAS model is modified to characterise aftershocks of large and anisotropic M9.0 mainshock ruptures. To account for damage accumulation of wood&#65506;&#65408;&#65424;frame houses due to aftershocks in Victoria, British Columbia, Canada, state&#65506;&#65408;&#65424;dependent fragility curves are implemented. The new simulation framework can be used for quasi&#65506;&#65408;&#65424;real&#65506;&#65408;&#65424;time aftershock hazard and risk assessments and city&#65506;&#65408;&#65424;wide post&#65506;&#65408;&#65424;event risk management.&lt;/p&gt;</dct:abstract>
    <dc:title>Spatiotemporal seismic hazard and risk assessment of M9.0 megathrust earthquake sequences of wood&#8208;frame houses in Victoria, British Columbia, Canada</dc:title>
    <dc:identifier>10.1002/eqe.3286</dc:identifier>
    <dct:references>https://doi.org/10.1002/eqe.3286</dct:references>
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