2021
DOI: 10.1016/j.chemgeo.2021.120270
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The composition of fluids stored in the central Mexican lithospheric mantle: Inferences from noble gases and CO2 in mantle xenoliths

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Cited by 18 publications
(14 citation statements)
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“…Mantle xenoliths and lavas were crushed for noble gas and CO 2 isotopic determinations following the same methods and analytical procedures described in Rizzo et al (2018), Rizzo et al (2021), Sandoval-Velasquez et al (2021a), and Sandoval-Velasquez et al (2021b. After crushing, samples were sieved with the aim of hand-picking crystals (with diameters >0.25 mm) of Ol, Opx, and Cpx from mantle xenoliths and only Ol crystals from lavas.…”
Section: Samples and Methodsmentioning
confidence: 99%
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“…Mantle xenoliths and lavas were crushed for noble gas and CO 2 isotopic determinations following the same methods and analytical procedures described in Rizzo et al (2018), Rizzo et al (2021), Sandoval-Velasquez et al (2021a), and Sandoval-Velasquez et al (2021b. After crushing, samples were sieved with the aim of hand-picking crystals (with diameters >0.25 mm) of Ol, Opx, and Cpx from mantle xenoliths and only Ol crystals from lavas.…”
Section: Samples and Methodsmentioning
confidence: 99%
“…Like areas within the United States portion, the Mexican Basin and Range was accompanied by intraplate magmatism that generated several alkali basalt localities (Figure 1A; Basu, 1977;Gutmann, 1986;Aranda-Gómez and Ortega-Gutiérrez, 1987;Henry and Aranda-Gómez, 1992;Luhr and Aranda-Gomez, 1997). These volcanic fields represent a unique opportunity to study the characteristics of the local lithospheric mantle, since their deposits contain abundant mantle xenoliths (including both spinel peridotite varieties and pyroxenites; Basu, 1977;Gutmann, 1986;Aranda-Gómez and Ortega-Gutiérrez, 1987;Luhr et al, 1989;Pier et al, 1992;Luhr and Aranda-Gomez, 1997;Housh et al, 2010;Dávalos-Elizondo et al, 2016;Sandoval-Velasquez et al, 2021a); these (in view of the relatively rapid ascent of the host magma through the crust by short-lived monogenetic volcanic eruptions) are expected to retain the pristine mineralogy and geochemical/isotopic characteristics of the mantle source (Pier et al, 1989;Luhr and Aranda-Gomez, 1997;Jackson, 1998;Pearson et al, 2014).…”
Section: Introductionmentioning
confidence: 99%
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