Staged storage and magma convection at Ambrym Volcano, Vanuatu

Sheehan, Fionnuala and Barclay, Jennifer ORCID: (2016) Staged storage and magma convection at Ambrym Volcano, Vanuatu. Journal of Volcanology and Geothermal Research, 322. 144–157. ISSN 0377-0273

[thumbnail of 1-s2.0-S0377027316300117-main]
PDF (1-s2.0-S0377027316300117-main) - Published Version
Available under License Creative Commons Attribution.

Download (3MB) | Preview


New mineral-melt thermobarometry and mineral chemistry data are presented for basaltic scoriae erupted from the Mbwelesu crater of Ambrym volcano, Vanuatu, during persistent lava lake activity in 2005 and 2007. These data reveal crystallisation conditions and enable the first detailed attempt at reconstruction of the central magma plumbing system of Ambrym volcano. Pressures and temperatures of magma crystallisation at Ambrym are poorly constrained. This study focuses on characterising the magma conditions underlying the quasipermanent lava lakes at the basaltic central vents, and examines petrological evidence for magma circulation. Mineral-melt equilibria for clinopyroxene, olivine and plagioclase allow estimation of pressures and temperatures of crystallisation, and reveal two major regions of crystallisation, at 24–29 km and 11–18 km depth, in agreement with indications from earthquake data of crustal storage levels at c.25–29 km and 12–21 km depth. Temperature estimates are ~1150–1170 ºC for the deeper region, and ~1110 1140 ºC in the midcrustal region, with lower temperatures of ~1090–1100 ºC for late-stage crystallisation. More primitive plagioclase antecrysts are thought to sample a slightly more mafic melt at sub-Moho depths. Resorption textures combined with effectively constant mafic mineral compositions suggest phenocryst convection in a storage region of consistent magma composition. In addition, basalt erupted at Ambrym has predominantly maintained a constant composition throughout the volcanic succession. This, coupled with recurrent periods of elevated central vent activity on the scale of months, suggest frequent magmatic recharge via steady-state melt generation at Ambrym.

Item Type: Article
Additional Information: Open access under a Creative Commons Attribution 4.0 International (CC BY 4.0)
Uncontrolled Keywords: ambrym,thermobarometry,petrology,recharge,convection,mafic
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: Pure Connector
Date Deposited: 22 Mar 2016 09:34
Last Modified: 22 Oct 2022 00:53
DOI: 10.1016/j.jvolgeores.2016.02.024

Actions (login required)

View Item View Item