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<dc:title>Aeromagnetic anomalies reveal the link between magmatism and tectonics during the early formation of the Canary Islands</dc:title>
<dc:creator>Blanco Montenegro, Isabel</dc:creator>
<dc:creator>Montesinos, Fuensanta G. .</dc:creator>
<dc:creator>Arnoso, José .</dc:creator>
<dc:subject>Física</dc:subject>
<dc:subject>Physics</dc:subject>
<dc:description>The 3-D inverse modelling of a magnetic anomaly measured over the NW submarine edifice of the&#xd;
volcanic island of Gran Canaria revealed a large, reversely-magnetized, elongated structure following&#xd;
an ENE-WSW direction, which we interpreted as a sill-like magmatic intrusion emplaced during the&#xd;
submarine growth of this volcanic island, with a volume that could represent up to about 20% of the&#xd;
whole island. The elongated shape of this body suggests the existence of a major crustal fracture in the&#xd;
central part of the Canary Archipelago which would have favoured the rapid ascent and emplacement of&#xd;
magmas during a time span from 0.5 to 1.9 My during a reverse polarity chron of the Earth’s magnetic&#xd;
field prior to 16 Ma. The agreement of our results with those of previous gravimetric, seismological and&#xd;
geodynamical studies strongly supports the idea that the genesis of the Canary Islands was conditioned&#xd;
by a strike-slip tectonic framework probably related to Atlas tectonic features in Africa. These results do&#xd;
not contradict the hotspot theory for the origin of the Canary magmatism, but they do introduce the&#xd;
essential role of regional crustal tectonics to explain where and how those magmas both reached the&#xd;
surface and built the volcanic edifices.</dc:description>
<dc:description>Project CGL2015-63799-P of the&#xd;
Spanish Ministry of Economy and Competitiveness</dc:description>
<dc:date>2018-01-26T09:03:46Z</dc:date>
<dc:date>2018-01-26T09:03:46Z</dc:date>
<dc:date>2018-01</dc:date>
<dc:type>info:eu-repo/semantics/article</dc:type>
<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
<dc:identifier>2045-2322</dc:identifier>
<dc:identifier>http://hdl.handle.net/10259/4716</dc:identifier>
<dc:identifier>10.1038/s41598-017-18813-w</dc:identifier>
<dc:language>eng</dc:language>
<dc:relation>Scientific Reports. 2018, 8, art. 42</dc:relation>
<dc:relation>https://doi.org/10.1038/s41598-017-18813-w</dc:relation>
<dc:relation>info:eu-repo/grantAgreement/MINECO/CGL2015-63799-P</dc:relation>
<dc:rights>Attribution 4.0 International</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>Nature Publishing Group</dc:publisher>
<europeana:object>https://riubu.ubu.es/bitstream/10259/4716/7/Blanco-SR_2018.pdf.jpg</europeana:object>
<europeana:provider>Hispana</europeana:provider>
<europeana:type>TEXT</europeana:type>
<europeana:rights>http://creativecommons.org/licenses/by/4.0/</europeana:rights>
<europeana:dataProvider>RIUBU. Repositorio Institucional de la Universidad de Burgos</europeana:dataProvider>
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