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dc.contributor.authorMadrigal, Pilaren
dc.contributor.authorGazel, Estebanen
dc.contributor.authorFlores, Kennet E.en
dc.contributor.authorBizimis, Michaelen
dc.contributor.authorJicha, Brianen
dc.date.accessioned2017-03-28T17:31:56Zen
dc.date.available2017-03-28T17:31:56Zen
dc.date.issued2016-11-08en
dc.identifier.urihttp://hdl.handle.net/10919/76700en
dc.description.abstractLarge igneous provinces, as the surface expression of deep mantle processes, play a key role in the evolution of the planet. Here we analyse the geochemical record and timing of the Pacific Ocean Large Igneous Provinces and preserved accreted terranes to reconstruct the history of pulses of mantle plume upwellings and their relation with a deep-rooted source like the Pacific large low-shear velocity Province during the Mid-Jurassic to Upper Cretaceous. Petrological modelling and geochemical data suggest the need of interaction between these deep-rooted upwellings and mid-ocean ridges in pulses separated by ∼10–20 Ma, to generate the massive volumes of melt preserved today as oceanic plateaus. These pulses impacted the marine biota resulting in episodes of anoxia and mass extinctions shortly after their eruption.en
dc.format.mimetypeapplication/pdfen
dc.language.isoen_USen
dc.publisherNatureen
dc.rightsCreative Commons Attribution 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en
dc.titleRecord of massive upwellings from the Pacific large low shear velocity provinceen
dc.typeArticle - Refereeden
dc.contributor.departmentGeosciencesen
dc.title.serialNature Communicationsen
dc.identifier.doihttps://doi.org/10.1038/ncomms13309en
dc.identifier.volume7en
dc.type.dcmitypeTexten


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Creative Commons Attribution 4.0 International
License: Creative Commons Attribution 4.0 International