2016
DOI: 10.1016/j.jvolgeores.2016.05.006
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Internal architecture of the Tuxtla volcanic field, Veracruz, Mexico, inferred from gravity and magnetic data

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Cited by 17 publications
(10 citation statements)
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“…From the geophysical evidence presented in Figure 2, we can infer the presence of shallow magmatic bodies underlying the LTVF region. Espindola et al (2016) also interpreted the presence of hot magmatic bodies with their tops at about 6 km depth. Therefore, the thermal regime beneath the LTVF is likely to be relatively hot, implying that the magmas may well have originated in the shallower part of the (garnet‐bearing) upper mantle.…”
Section: Discussionmentioning
confidence: 96%
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“…From the geophysical evidence presented in Figure 2, we can infer the presence of shallow magmatic bodies underlying the LTVF region. Espindola et al (2016) also interpreted the presence of hot magmatic bodies with their tops at about 6 km depth. Therefore, the thermal regime beneath the LTVF is likely to be relatively hot, implying that the magmas may well have originated in the shallower part of the (garnet‐bearing) upper mantle.…”
Section: Discussionmentioning
confidence: 96%
“…Both extensional regime and strike‐slip faulting have been amply documented in the LTVF from geological and geophysical constraints (e.g., Andreani, Le Pichon, et al, 2008; Andreani, Rangin, et al, 2008; Espindola et al, 2016; Nelson et al, 1995; Nelson & Gonzalez‐Caver, 1992). The multidimensional geochemical evidence presented in this article supports an extensional regime in the LTVF.…”
Section: Discussionmentioning
confidence: 99%
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