<?xml version="1.0" encoding="UTF-8"?><rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcq="http://purl.org/dc/terms/"><records count="1" morepages="false" start="1" end="1"><record rownumber="1"><dc:product_type>Journal Article</dc:product_type><dc:title>Complex multi-fault rupture and triggering during the 2023 earthquake doublet in southeastern Türkiye</dc:title><dc:creator>Liu, Chengli; Lay, Thorne; Wang, Rongjiang; Taymaz, Tuncay; Xie, Zujun; Xiong, Xiong; Irmak, Tahir Serkan; Kahraman, Metin; Erman, Ceyhun</dc:creator><dc:corporate_author/><dc:editor/><dc:description>&lt;title&gt;Abstract&lt;/title&gt; &lt;p&gt;Two major earthquakes (M&lt;sub&gt;W&lt;/sub&gt;7.8 and M&lt;sub&gt;W&lt;/sub&gt;7.7) ruptured left-lateral strike-slip faults of the East Anatolian Fault Zone (EAFZ) on February 6, 2023, causing &gt;59,000 fatalities and ~$119B in damage in southeastern Türkiye and northwestern Syria. Here we derived kinematic rupture models for the two events by inverting extensive seismic and geodetic observations using complex 5-6 segment fault models constrained by satellite observations and relocated aftershocks. The larger event nucleated on a splay fault, and then propagated bilaterally ~350 km along the main EAFZ strand. The rupture speed varied from 2.5-4.5 km/s, and peak slip was ~8.1 m. 9-h later, the second event ruptured ~160 km along the curved northern EAFZ strand, with early bilateral supershear rupture velocity (&gt;4 km/s) followed by a slower rupture speed (~3 km/s). Coulomb Failure stress increase imparted by the first event indicates plausible triggering of the doublet aftershock, along with loading of neighboring faults.&lt;/p&gt;</dc:description><dc:publisher>Nature</dc:publisher><dc:date>2023-12-01</dc:date><dc:nsf_par_id>10520410</dc:nsf_par_id><dc:journal_name>Nature Communications</dc:journal_name><dc:journal_volume>14</dc:journal_volume><dc:journal_issue>1</dc:journal_issue><dc:page_range_or_elocation/><dc:issn>2041-1723</dc:issn><dc:isbn/><dc:doi>https://doi.org/10.1038/s41467-023-41404-5</dc:doi><dcq:identifierAwardId>1802364</dcq:identifierAwardId><dc:subject/><dc:version_number/><dc:location/><dc:rights/><dc:institution/><dc:sponsoring_org>National Science Foundation</dc:sponsoring_org></record></records></rdf:RDF>