Magma plumbing system below the Popocatepetl and Iztaccihuatl volcanoes, central Mexico, as revealed by aeromagnetic data


Por: Lopez-Loera, H., Espindola, J. M., Sosa-Ceballos, G., Macias, J. L., Urrutia-Fucugauchi, J., Torres-Gaytan, D. E., Garcia-Tenorio, F.

Publicada: 1 abr 2022
Categoría: Geochemistry and petrology

Resumen:
One of the principal tasks of volcanology is to infer the eruptive history of volcanoes. However, the processes culminating in volcanic events include many occurring under the surface; thus, a complete understanding of magmatic activity requires information on the subsurface magmatic bodies. Such information is crucial in the case of large active volcanoes. This paper analyzed the aeromagnetic data from a survey performed through the Iztaccihuatl and Popocatepetl volcanoes in central Mexico, as examined in the light of the petrology and geology of the area. To achieve this objective, we processed the residual magnetic field of the area to obtain the geomagnetic anomalies due to bodies of contrasting magnetic susceptibility. We obtained improved imaging of the anomalies through several techniques and defined a pattern of anomalies grouped in six aeromagnetic domains (AMD). A large domain (AMD I) holds positive anomalies with maxima around the volcanoes. The inverted data yielded models of the main bodies under the large volcanoes, which extended into other smaller structures or sites without emergence to the surface. Large magma bodies stalled below Popocatepetl (similar to 54.5 km(3)) and Iztaccihuatl (similar to 30.5 km(3)); they contrast in volume with the irregularly shaped Paso de Cortes intrusion (4.7 km(3)), which halted at a depth of 1.6 km. The latter intrusion is likely associated with mush-like bodies formed by magmas from the Popocatepetl plumbing system forced away from the volcano's principal network of conduits. The positive intensity of magnetization of the bodies suggests they are of mafic composition and were intruded into silicic rocks.

Filiaciones:
(Corresponding Author), Inst Potosino Invest Cient & Tecnol, Geociencias Aplicadas, AC Camino La Presa San Jose 2055, San Luis Potosi 78216, San Luis Potosi, Mexico
Inst Potosino Invest Cient & Tecnol, Geociencias Aplicadas, AC Camino La Presa San Jose 2055, San Luis Potosi 78216, San Luis Potosi, Mexico
Univ Nacl Autonoma Mexico, Inst Geofis, UNAM, Av Univ 3000, Cd De Mexico 04510, Mexico
Univ Nacl Autonoma Mexico, Inst Geofis Unidad Michoacan, Antigua Carretera Patzcuaro 8701, Morelia 58059, Michoacan, Mexico
ISSN: 02588900
Editorial
Springer-Verlag, 233 SPRING STREET, NEW YORK, NY 10013 USA, Estados Unidos America
Tipo de documento: Article
Volumen: 84 Número: 4
Páginas:
WOS Id: 000772077600001

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