Paleomagnetic study of El Metate shield volcano (Michoacan, Mexico) confirms its monogenetic nature and young age (similar to 1250 CE)


Por: Mahgoub, Ahmed Nasser, Bohnel, Harald, Siebe, Claus, Chevrel, Magdalena Oryaelle

Publicada: 15 abr 2017
Resumen:
In a recent study, Chevrel et al. (2016a, b) radiocarbon-dated the oldest lava flow of the voluminous (similar to 9.2 km(3)) El Metate shield volcano (Michoacan, Mexico) at cal 1250-1260 CE and proposed that its eruption was monogenetic in origin, with twelve younger lava flows emplaced during a short period of only similar to 35 years, but certainly <275 years. In order to test this hypothesis, we undertook a detailed paleomagnetic study of five lava flows from El Metate to check the consistency of their paleomagnetic directions. Additionally, a group of representative specimens was treated with the double-heating Thellier experiment using the IZZI protocol for paleointensity determination. Flow mean paleomagnetic directions obtained for four of the flows are indistinguishable, and discordant directions were obtained from the site of the 5th flow measured, probably due to the tilting of the sampled block after remanence acquisition. Mean paleodirections and intensities were used for paleomagnetic dating applying the global paleosecular variation model SHA.DIF.14k. The resulting age range for the eruption is 11501290 CE, which overlaps with the range previously determined by the C-14 method by Chevrel et al. (2016a). Accepting the C-14 age of the oldest flow as the maximum age, the age range would be reduced to 1250-1290 CE, which strongly supports the hypothesis of a monogenetic nature of the El Metate eruption. (C) 2017 Elsevier B.V. All rights reserved.

Filiaciones:
Mahgoub, Ahmed Nasser:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Bohnel, Harald:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Mexico

Siebe, Claus:
 Univ Nacl Autonoma Mexico, Inst Geofis, Dept Vulcanol, Ciudad De Mexico 04510, Mexico

Chevrel, Magdalena Oryaelle:
 Univ Blaise Pascal, CNRS, Lab Magmas & Volcans, 6 Av Blaise Pascal, F-63178 Aubiere, France
ISSN: 03770273
Editorial
ELSEVIER SCIENCE BV, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS, Países Bajos
Tipo de documento: Article
Volumen: 336 Número:
Páginas: 209-218
WOS Id: 000402216400014

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