2017
DOI: 10.1007/s00410-017-1360-2
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A geochemical approach to distinguishing competing tectono-magmatic processes preserved in small eruptive centres

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Cited by 22 publications
(15 citation statements)
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References 76 publications
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“…Magma ascent at Cordón Caulle-Puyehue complex, by contrast, is suggested to have been rapid, from the result of uranium-series isotopes (Jicha et al, 2007). Parallel uranium-series work on magmas of the CHSEC by McGee et al (2017) has suggested both fast melting and ascent of magmas after fluid addition to the mantle region beneath.…”
Section: Accepted Manuscriptmentioning
confidence: 99%
“…Magma ascent at Cordón Caulle-Puyehue complex, by contrast, is suggested to have been rapid, from the result of uranium-series isotopes (Jicha et al, 2007). Parallel uranium-series work on magmas of the CHSEC by McGee et al (2017) has suggested both fast melting and ascent of magmas after fluid addition to the mantle region beneath.…”
Section: Accepted Manuscriptmentioning
confidence: 99%
“…The (Romero et al, 2018). c. Total-Alkali Silica (TAS Le Bas et al, 1986) diagram showing the bulk rock compositions of Villarrica eruptions and basement rocks from past studies (Clavero-Ribes, 1996;Hickey-Vargas et al, 1989Lohmar, 2008;McGee et al, 2017;Morgado et al, 2015;Pioli et al, 2015;Pizarro et al, 2019;Silva Parejas, 2008;Wehrmann et al, 2014;Witter et al, 2004;Zajacz & Halter, 2007). This shows the homogeneous nature of Villarrica eruptive products: the vast majority of the juvenile products (98%) have 52-57 wt% SiO2.…”
Section: Database Compilationmentioning
confidence: 99%
“…Thus, the extend of magma differentiation is variable and therefore the geochemistry of satellite monogenetic cones is modified to the polygenic edifices (i.e. Huililco monogenetic cones versus Llaima stratovolcano in Chile; [2]).…”
Section: Spatial Heterogeneities Of Magma Sourcementioning
confidence: 99%
“…from the effusive as explosive volcanic rocks also lead to various interrogations regarding origin of the magma that circulate in the lithosphere below monogenetic volcanic fields. Most of all, the presence of spatial magma heterogeneities is a major observation discussed and synthesized for volcanic fields in subduction zones [1][2][3]. Visualization tools are required to facilitate these observations and analyses for understanding the building of minor volcanic centers as defining the origin of the magma in monogenetic fields.…”
Section: Introductionmentioning
confidence: 99%