<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-06-28T04:44:54Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/23697" metadataPrefix="qdc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/23697</identifier><datestamp>2024-07-29T13:44:49Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</setSpec></header><metadata><qdc:qualifieddc xmlns:qdc="http://dspace.org/qualifieddc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://purl.org/dc/elements/1.1/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dc.xsd http://purl.org/dc/terms/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dcterms.xsd http://dspace.org/qualifieddc/ http://www.ukoln.ac.uk/metadata/dcmi/xmlschema/qualifieddc.xsd">
   <dc:title>Refining seismic parameters in low seismicity areas by 3D trenching: TheAlhama de Murcia fault, SE Iberia</dc:title>
   <dc:creator>Ferrater, Marta</dc:creator>
   <dc:creator>Ortuño, María</dc:creator>
   <dc:creator>Masana, Eulàlia</dc:creator>
   <dc:creator>Pallàs, Raimon</dc:creator>
   <dc:creator>Perea Manera, Héctor</dc:creator>
   <dc:creator>Baize, Stephane</dc:creator>
   <dc:creator>Martínez Díaz, José Jesús</dc:creator>
   <dc:creator>García Meléndez, Eduardo</dc:creator>
   <dc:creator>Echeverria, Anna</dc:creator>
   <dc:creator>Rockwell, Thomas K.</dc:creator>
   <dc:creator>Sharp, Warren D.</dc:creator>
   <dc:creator>Medialdea, Alicia</dc:creator>
   <dc:creator>Rhodes, Edward J.</dc:creator>
   <dcterms:abstract>hree-dimensional paleoseismology in strike-slip faults with slip rates less than 1 mm per year involves a greatmethodological challenge. We adapted 3D trenching to track buried channels offset by the Alhama de Murciaseismogenic left-lateral strike-slip fault (SE Iberia). A fault net slip of 0.9 ± 0.1 mm/yr was determined usingstatistical analysis of piercing lines for one buried channel, whose age is constrained between 15.2 ± 1.1 kaand 21.9–22.3 cal BP. This value is larger and more accurate than the previously published slip rates for thisfault. The minimum number offive paleo-earthquakes identified since the deposition of dated layers suggestsa maximum average recurrence interval of approximately 5 ka. The combination of both seismic parametersyields a maximum slip per event between 5.3 and 6.3 m. We show that accurately planned trenching strategiesand data processing may be key to obtaining robust paleoseismic parameters in low seismicity ares</dcterms:abstract>
   <dcterms:dateAccepted>2023-06-18T05:59:02Z</dcterms:dateAccepted>
   <dcterms:available>2023-06-18T05:59:02Z</dcterms:available>
   <dcterms:created>2023-06-18T05:59:02Z</dcterms:created>
   <dcterms:issued>2016-06</dcterms:issued>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/23697</dc:identifier>
   <dc:identifier>0040-1951</dc:identifier>
   <dc:identifier>10.1016/j.tecto.2016.05.020</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>SHAKE CGL2011-30005-C02-02</dc:relation>
   <dc:relation>RISKNAT-2014SGR/1243</dc:relation>
   <dc:rights>restricted access</dc:rights>
   <dc:publisher>Elsevier</dc:publisher>
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