From Explosive Vent Opening to Effusive Outpouring: Mineral Constraints on Magma Dynamics and Timescales at Paricutin Monogenetic Volcano

نویسندگان

چکیده

Abstract Paricutin volcano is the youngest monogenetic cone of Michoacán–Guanajuato volcanic field (Mexico), with an excellent historical eruption record from February 1943 to March 1952. The magma emitted during 9 years activity was compositionally zoned basaltic andesite andesite. This has been considered a classic example differentiation controlled by crustal assimilation combined fractional crystallization. However, recent geochemical study products points mantle source heterogeneity and crystallization as key processes involved in compositional variability magmas. Here we present detailed petrological characterization minerals [olivine, plagioclase, pyroxene, Cr-spinel, (Ti-)magnetite] shed light on that led chemical evolution eruptive products. Our sample set includes early tephra first weeks or months whole sequence lava flows followed. mineral assemblage, their texture, composition show systematic between opening explosive vent effusive stage. are andesites oscillatory-zoned olivine rare pyroxene xenocrysts. In contrast, later erupted post-January 1944 lavas normally olivine, Cr-spinel inclusions equilibrium host frequent orthopyroxene (after December 1947) minor zoning. Mineral chemistry data diffusion timescales, together whole-rock geochemistry, suggest convective regime large temperature oxygen fugacity gradients characterized short timescales (few days) stage, followed steadier longer months) including periodic recharge, mixing, addition, mineralogical evidence have gathered does not support considerable at Paricutin. shows eruptions far being geochemically simple, instead involve multiple batches complex storage mixing stages before eruption.

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ژورنال

عنوان ژورنال: Journal of Petrology

سال: 2021

ISSN: ['1460-2415', '0022-3530']

DOI: https://doi.org/10.1093/petrology/egaa112