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<dc:title>Rock Magnetism of Lapilli and Lava Flows from Cumbre Vieja Volcano, 2021 Eruption (La Palma, Canary Islands): Initial Reports</dc:title>
<dc:creator>Parés Casanova, Josep M.</dc:creator>
<dc:creator>Vernet Tarrago, Eva</dc:creator>
<dc:creator>Calvo Rathert, Manuel</dc:creator>
<dc:creator>Soler, Vicente</dc:creator>
<dc:creator>Bógalo Román, Mª Felicidad</dc:creator>
<dc:creator>Álvaro, Ana</dc:creator>
<dc:subject>Rock magnetism</dc:subject>
<dc:subject>Canary Islands</dc:subject>
<dc:subject>Recent volcanic eruption</dc:subject>
<dc:subject>Lapilli</dc:subject>
<dc:subject>Basaltic lava flow</dc:subject>
<dc:subject>Física</dc:subject>
<dc:subject>Geología</dc:subject>
<dc:subject>Physics</dc:subject>
<dc:subject>Geology</dc:subject>
<dc:description>We present initial rock magnetic results for both lava flows and lapilli produced by the 2021&#xd;
eruption of the Cumbre Vieja, La Palma (Canary Islands). Samples were taken during the eruption to&#xd;
minimize early alteration and weathering of the rocks and tephra. Standard procedures included&#xd;
progressive alternating field and thermal demagnetization, hysteresis curves, thermomagnetic experiments, progressive acquisition of isothermal remanent magnetization (IRM), and First-Order Reversal&#xd;
Curves (FORCs). Overall, our observations, including low to medium unblocking temperatures,&#xd;
isothermal remanent magnetization to 1 Tesla, and the abundance of wasp-waist hysteresis loops,&#xd;
strongly suggest the presence of Ti-rich titanomagnetites as the main remanence carriers in both lava&#xd;
flows and lapilli, in addition to some hematite as well. Whereas the former has been directly seen&#xd;
(SEM), hematite is elusive with nonmagnetic-based methods. Rock magnetic data, on a Day plot, also&#xd;
reveal that the magnetic grain size tends to be larger in the lava flows than in the lapilli.</dc:description>
<dc:description>This research was funded by Agencia Estatal de Investigación, Spain, grant no. PID2019-105796GB-00/AEI/10.13039/501100011033.</dc:description>
<dc:date>2023-03-24T11:44:00Z</dc:date>
<dc:date>2023-03-24T11:44:00Z</dc:date>
<dc:date>2022-07</dc:date>
<dc:type>info:eu-repo/semantics/article</dc:type>
<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
<dc:identifier>http://hdl.handle.net/10259/7597</dc:identifier>
<dc:identifier>10.3390/geosciences12070271</dc:identifier>
<dc:identifier>2076-3263</dc:identifier>
<dc:language>eng</dc:language>
<dc:relation>Geosciences. 2022, V. 12, n. 7, 271</dc:relation>
<dc:relation>https://doi.org/10.3390/geosciences12070271</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2019-105796 GB-I00/ES/LAS VARIACIONES DEL REGISTRO ARQUEOMAGNETICO PREHISTORICO EN LA PENINSULA IBERICA Y EL CAUCASO/</dc:relation>
<dc:rights>Atribución 4.0 Internacional</dc:rights>
<dc:rights>http://creativecommons.org/licenses/by/4.0/</dc:rights>
<dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
<dc:format>application/pdf</dc:format>
<dc:publisher>MDPI</dc:publisher>
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