Barclay, Jenni ORCID: https://orcid.org/0000-0002-6122-197X, Herd, Richard A., Edwards, Ben R., Christopher, Thomas, Kiddle, Emma J., Plail, Melissa and Donovan, Amy (2010) Caught in the act: Implications for the increasing abundance of mafic enclaves during the eruption of the Soufriere Hills Volcano, Montserrat. Geophysical Research Letters, 37. ISSN 1944-8007
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Abstract
An exceptional opportunity to sample several large blocks sourced from the same region of the growing Soufrière Hills lava dome has documented a significant increase in the presence of mafic enclaves in the host andesite during the course of a long-lived eruptive episode with several phases. In 1997 (Phase I) mafic inclusions comprised ~1 volume percent of erupted material; in 2007 (Phase III) deposits their volumetric abundance increased to 5–7 percent. A broader range of geochemically distinctive types occurs amongst the 2007 enclaves. Crystal-poor enclaves generally have the least evolved (basaltic) compositions; porphyritic enclaves represent compositions intermediate between basaltic and andesitic compositions. The absence of porphyritic enclaves prior to Phase III magmatism at Soufrière Hills Volcano suggests that a mixing event occurred during the course of the current eruptive episode, providing direct evidence consistent with geophysical observations that the system is continuously re-invigorated from depth.
Item Type: | Article |
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Faculty \ School: | Faculty of Science > School of Environmental Sciences |
UEA Research Groups: | Faculty of Science > Research Groups > Geosciences Faculty of Science > Research Groups > Volcanoes@UEA (former - to 2018) Faculty of Science > Research Groups > Geosciences and Natural Hazards (former - to 2017) |
Depositing User: | Rachel Snow |
Date Deposited: | 28 Mar 2011 09:55 |
Last Modified: | 27 Mar 2023 16:30 |
URI: | https://ueaeprints.uea.ac.uk/id/eprint/27282 |
DOI: | 10.1029/2010GL042509 |
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