dc.creator | Martínez Ardila, Ana María | |
dc.creator | Paterson, Scott R. | |
dc.creator | Memeti, Vali | |
dc.creator | Parada, Miguel A. | |
dc.creator | Molina, Pablo G. | |
dc.date.accessioned | 2019-10-11T17:32:43Z | |
dc.date.available | 2019-10-11T17:32:43Z | |
dc.date.created | 2019-10-11T17:32:43Z | |
dc.date.issued | 2019 | |
dc.identifier | Lithos, Volumen 326-327, | |
dc.identifier | 18726143 | |
dc.identifier | 00244937 | |
dc.identifier | 10.1016/j.lithos.2018.12.007 | |
dc.identifier | https://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.language | en | |
dc.publisher | Elsevier B.V. | |
dc.rights | http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ | |
dc.rights | Attribution-NonCommercial-NoDerivs 3.0 Chile | |
dc.source | Lithos | |
dc.subject | Arcs | |
dc.subject | Assimilation | |
dc.subject | Crust | |
dc.subject | Flare-up | |
dc.subject | Isotopes | |
dc.subject | Mantle | |
dc.title | Mantle driven cretaceous flare-ups in Cordilleran arcs | |
dc.type | Artículos de revistas | |