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<front>
<journal-meta>
<journal-id journal-id-type="publisher">NHESSD</journal-id>
<journal-title-group>
<journal-title>Natural Hazards and Earth System Sciences Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">NHESSD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nat. Hazards Earth Syst. Sci. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2195-9269</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/nhess-2022-46</article-id>
<title-group>
<article-title>Quantifying the probability and uncertainty of multiple-structure rupture and recurrence intervals in Taiwan</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chang</surname>
<given-names>Chieh-Chen</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chang</surname>
<given-names>Chih-Yu</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chan</surname>
<given-names>Chung-Han</given-names>
<ext-link>https://orcid.org/0000-0003-1875-3652</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Earth Sciences, National Central University, Taoyuan, 32001, Taiwan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Earthquake-Disaster &amp; Risk Evaluation and Management (E-DREaM) Center, National Central University, Taoyuan, 32001, Taiwan</addr-line>
</aff>
<funding-group>
<award-group id="gs1">
<funding-source>Ministry of Science and Technology, Taiwan</funding-source>
<award-id>MOST 109-2116-M-008 -029 -MY3</award-id>
<award-id>MOST 110-2124-M-002 -008</award-id>
</award-group>
<award-group id="gs2">
<funding-source>Ministry of Education</funding-source>
<award-id>the Featured Areas Research Center Program within the framework of the Higher Education Sprout Project</award-id>
</award-group>
</funding-group>
<pub-date pub-type="epub">
<day>08</day>
<month>02</month>
<year>2022</year>
</pub-date>
<volume>2022</volume>
<fpage>1</fpage>
<lpage>22</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2022 Chieh-Chen Chang et al.</copyright-statement>
<copyright-year>2022</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://nhess.copernicus.org/preprints/nhess-2022-46/">This article is available from https://nhess.copernicus.org/preprints/nhess-2022-46/</self-uri>
<self-uri xlink:href="https://nhess.copernicus.org/preprints/nhess-2022-46/nhess-2022-46.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/preprints/nhess-2022-46/nhess-2022-46.pdf</self-uri>
<abstract>
<p>&lt;p&gt;This study identifies fault pairs with potential for simultaneous rupture in a coseismic period based on a physics-based model, and proposes a set of formulas to evaluate their recurrence intervals and uncertainties. To assess the potential for a multiple-fault rupture, we calculated the probability of stress triggering between active faults. We assumed that a multiple-fault rupture would occur if two faults could trigger each other by enhancing the plane with thresholds of a stress increase and the distance between the faults. To estimate the recurrence intervals for multiple-fault ruptures, we implemented a statistics-based model in which the slip rate could be partitioned based on the earthquake magnitudes of the individual fault and multiple-fault ruptures. Due to a larger characteristic magnitude and a larger displacement of the multiple-fault rupture, its recurrence interval could be longer. Therefore, application of the multiple-fault rupture could lead to an increase in seismic hazard in a long return period, which would be crucial for the safety evaluation of infrastructures, such as nuclear power plants and dams.&lt;/p&gt;</p>
</abstract>
<counts><page-count count="22"/></counts>
</article-meta>
</front>
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