<?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>2026-07-30T21:34:10Z</responseDate><request verb="GetRecord" identifier="oai:riubu.ubu.es:10259/6109" metadataPrefix="marc">https://riubu.ubu.es/oai/request</request><GetRecord><record><header><identifier>oai:riubu.ubu.es:10259/6109</identifier><datestamp>2022-12-19T09:49:15Z</datestamp><setSpec>com_10259.4_2560</setSpec><setSpec>com_10259_5086</setSpec><setSpec>com_10259_2604</setSpec><setSpec>col_10259.4_2561</setSpec></header><metadata><record xmlns="http://www.loc.gov/MARC21/slim" xmlns:doc="http://www.lyncode.com/xoai" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dcterms="http://purl.org/dc/terms/" xsi:schemaLocation="http://www.loc.gov/MARC21/slim http://www.loc.gov/standards/marcxml/schema/MARC21slim.xsd">
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<subfield code="a">dc</subfield>
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<subfield code="a">Calvín Ballester, Pablo</subfield>
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<subfield code="a">Pueyo Morer, Emilio L.</subfield>
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<subfield code="a">Ramón Ortiga, Mª José</subfield>
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<datafield tag="720" ind1=" " ind2=" ">
<subfield code="a">Casas Sainz, Antonio M.</subfield>
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<subfield code="a">Villalaín Santamaria, Juan José</subfield>
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<subfield code="c">2020-08</subfield>
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<subfield code="a">The Small Circle (SC) tools analyse the stereographic tracks (small circles) followed by the&#xd;
palaeomagnetic vectors during folding processes. Working with interfolding and synfolding&#xd;
remagnetizations, the Small Circle Intersection (SCI) method allows finding the best solution&#xd;
of grouping that should correspond with the remagnetization direction. Once this is known,&#xd;
it is possible to determine the magnetization age as well as the degree of bed tilting at this&#xd;
moment. The SC tools are based on some assumptions, among which the coaxiality between&#xd;
the different deformation events is the one addressed in this work (i.e. absence of vertical&#xd;
axis rotations, VARs, or differential horizontal axis rotations, dHARs). This assumption is&#xd;
based on the necessity of knowing the rotation axis for folding after the acquisition of the&#xd;
remagnetization, and SC tools consider the bedding strike as this axis, something that is&#xd;
only accomplished under coaxial folding. In order to explore how non-coaxiality affects the&#xd;
solutions derived from the SC methods, we first (i) identify the variables that control these&#xd;
errors through simple models that only consider two theoretical palaeomagnetic sites, after&#xd;
that it is possible (ii) to derive the mathematical relationships between them. Finally, we (iii)&#xd;
simulate errors derived from the use of SC tools using a population of 30 palaeomagnetic sites&#xd;
recreating different possible scenarios with VARs and dHARs in nature.</subfield>
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<subfield code="a">0956-540X</subfield>
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<subfield code="a">http://hdl.handle.net/10259/6109</subfield>
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<subfield code="a">10.1093/gji/ggaa217</subfield>
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<subfield code="a">Palaeomagnetism</subfield>
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<subfield code="a">Remagnetization</subfield>
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<datafield tag="245" ind1="0" ind2="0">
<subfield code="a">Analysing non-coaxial folding effects in the Small Circle Intersection method</subfield>
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