dc.creatorMartínez Ardila, Ana María
dc.creatorPaterson, Scott R.
dc.creatorMemeti, Vali
dc.creatorParada, Miguel A.
dc.creatorMolina, Pablo G.
dc.date.accessioned2019-10-11T17:32:43Z
dc.date.available2019-10-11T17:32:43Z
dc.date.created2019-10-11T17:32:43Z
dc.date.issued2019
dc.identifierLithos, Volumen 326-327,
dc.identifier18726143
dc.identifier00244937
dc.identifier10.1016/j.lithos.2018.12.007
dc.identifierhttps://repositorio.uchile.cl/handle/2250/171411
dc.description.abstract© 2018 The AuthorsContinental arcs display episodic magmatism characterized by flare-ups and lulls. Models published to explain these patterns invoke (1) upper plate crustal processes driven by internal feedback; (2) episodic mantle melting processes, or (3) external lower plate tectonic events. This study addresses the role of mantle magmas during flare-ups in Mesozoic Cretaceous continental arcs using geochronological and geochemical data for three Cretaceous arc segments: the western Peninsular Ranges Batholith (wPRB), the Peruvian Coastal Batholith (PCB), and the Chilean Coastal Batholith (CCB). In all three arc segments, bedrock zircon age patterns defining a flare-up from ~125 to 90 Ma characterized by gabbro to granite units with Sri < 0.705, ƐNd from 0 to +7.5, 208Pb/204Pb from 38.2 to 38.7, and 206Pb/204Pb from 18.3 to 18.7. These values project well towards a depleted mantle source. Areal measurements show that gabbro forms ~18% (wPRB), ~24% (PCB), and ~10% (CCB) of exposed p
dc.languageen
dc.publisherElsevier B.V.
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile
dc.sourceLithos
dc.subjectArcs
dc.subjectAssimilation
dc.subjectCrust
dc.subjectFlare-up
dc.subjectIsotopes
dc.subjectMantle
dc.titleMantle driven cretaceous flare-ups in Cordilleran arcs
dc.typeArtículos de revistas


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