Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/162512
Title: Dynamics and timescales of mafic–silicic magma interactions at Soufrière Hills Volcano, Montserrat
Authors: Didonna, Rosa
Costa, Fidel
Handley, Heather
Turner, Simon
Barclay, Jenni
Keywords: Science::Geology
Issue Date: 2022
Source: Didonna, R., Costa, F., Handley, H., Turner, S. & Barclay, J. (2022). Dynamics and timescales of mafic–silicic magma interactions at Soufrière Hills Volcano, Montserrat. Contributions To Mineralogy and Petrology, 177(2). https://dx.doi.org/10.1007/s00410-022-01891-z
Project: NRFNRFI2017-06 
Journal: Contributions to Mineralogy and Petrology 
Abstract: Mafic magma intrusions into silica-rich magmatic reservoirs are commonly proposed to drive the eruptions of andesitic hybrid magmas that characterise many arc volcanoes. However, interactions between contrasting magmas involve large gradients of physical and chemical properties that change over time, and the details of such processes have proven difficult to constrain. In this paper we investigate the dynamics of magma mingling and mixing using chemical and textural zoning patterns recorded in plagioclase crystals from the February 2010 eruption at Soufrière Hills Volcano, Montserrat. This eruption is considered a classic example of interactions between the andesite magma that constitutes the bulk of the erupted volume and the basaltic andesite that occurs as enclaves. We find that plagioclase crystals are characterised by two well-defined zones that record mafic–silicic magma interaction: a crystal interior, often identified by a patchy, dusty and oscillatory zoning, and an overgrowth zone (rim) of a different composition. We use the anorthite and Mg contents to track the thermal and compositional changes experienced by the crystals over time. Our results reveal that the crystal rims formed a few hours to days prior to eruption, during co-eruptive magmatic interactions. The interaction between the two magmas with contrasting rheology is likely increased by a narrowing conduit geometry towards the surface, which facilitates convection and additional interface contact of the two magmas. Our findings shed new light on the nature and timing of magmatic interactions driving the final eruptive phase at Soufrière Hills Volcano and help to propose an interpretative framework of the monitoring signals.
URI: https://hdl.handle.net/10356/162512
ISSN: 0010-7999
DOI: 10.1007/s00410-022-01891-z
Rights: © Crown 2022. Open Access. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
Fulltext Permission: open
Fulltext Availability: With Fulltext
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EOS Journal Articles

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