Geology and geochemistry of Amealco Caldera, Qro., Mexico

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Abstract

Amealco Caldera, located in the central part of the Mexican Volcanic Belt (MVB), about 130 km NW of Mexico City, is characterized by a quasi-circular, ∼11-km-diameter structure whose southern portion is partly truncated by a regional fault. The caldera was formed (< 5 m.y. ago) due to a voluminous eruption of 65 km3 (eq. magma volume) of ignimbrites which covered an area of ∼1800 km2. This was followed by eruption of ∼2 km3 of andesitic and dacitic lava flows from the border of the caldera and emplacement of a total of 8 silicic (rhyolitic) domes (∼8 km3) inside the caldera. Finally, postcaldera volcanism (∼4 km3) consisted of extrusion of andesitic and basaltic andesite lavas and scoriae.

We have analyzed 17 representative rock-samples for their major- and trace-element contents by X-ray fluorescence spectrometry and for rare earth elements by high-performance liquid chromatography. All samples were also analyzed for their Sr and Nd isotopic compositions which range as follows: 87Sr/86Sr 0.70379–0.70451, 143Nd/144Nd 0.51267–0.51278. The chemical and isotopic data are used to constrain the origin and evolution of magmas in the caldera. No combination of altered MORB and overlying sediments from the subducted slab (Cocos plate) can produce the Sr and Nd isotopic compositions observed in rocks from Amealco caldera. Further modelling reveals that the mantle-derived primary magmas in Amealco caldera may have assimilated up to ∼10% of a crustal component during their evolution from basaltic-andesites to dacites, but no further assimilation appears to have taken place during the evolution of the rhyolitic magmas. The structure and genesis of the Amealco caldera are comparable to some other calderas of the MVB.

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    Present address: Dept. of Geology, Michigan Technological University, Houghton, MI 49931, USA.

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