Melt inclusion constraints on petrogenesis of the 2014-2015 Holuhraun eruption, Iceland

Margaret E Hartley; Enikö Bali; John Maclennan; David A Neave; Sæmundur A Halldórsson

doi:10.1007/s00410-017-1435-0

Melt inclusion constraints on petrogenesis of the 2014-2015 Holuhraun eruption, Iceland

Contrib Mineral Petrol. 2018;173(2):10. doi: 10.1007/s00410-017-1435-0. Epub 2018 Jan 12.

Authors

Margaret E Hartley¹, Enikö Bali², John Maclennan³, David A Neave⁴, Sæmundur A Halldórsson²

Affiliations

¹ 1School of Earth and Environmental Sciences, University of Manchester, Manchester, UK.
² 2Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland.
³ 3Department of Earth Sciences, University of Cambridge, Cambridge, UK.
⁴ 4Institut für Mineralogie, Leibniz Universität Hannover, Hannover, Germany.

Abstract

The 2014-2015 Holuhraun eruption, on the Bárðarbunga volcanic system in central Iceland, was one of the best-monitored basaltic fissure eruptions that has ever occurred, and presents a unique opportunity to link petrological and geochemical data with geophysical observations during a major rifting episode. We present major and trace element analyses of melt inclusions and matrix glasses from a suite of ten samples collected over the course of the Holuhraun eruption. The diversity of trace element ratios such as La/Yb in Holuhraun melt inclusions reveals that the magma evolved via concurrent mixing and crystallization of diverse primary melts in the mid-crust. Using olivine-plagioclase-augite-melt (OPAM) barometry, we calculate that the Holuhraun carrier melt equilibrated at 2.1 ± 0.7 kbar (7.5 ± 2.5 km), which is in agreement with the depths of earthquakes (6 ± 1 km) between Bárðarbunga central volcano and the eruption site in the days preceding eruption onset. Using the same approach, melt inclusions equilibrated at pressures between 0.5 and 8.0 kbar, with the most probable pressure being 3.2 kbar. Diffusion chronometry reveals minimum residence timescales of 1-12 days for melt inclusion-bearing macrocrysts in the Holuhraun carrier melt. By combining timescales of diffusive dehydration of melt inclusions with the calculated pressure of H₂O saturation for the Holuhraun magma, we calculate indicative magma ascent rates of 0.12-0.29 m s^-1. Our petrological and geochemical data are consistent with lateral magma transport from Bárðarbunga volcano to the eruption site in a shallow- to mid-crustal dyke, as has been suggested on the basis of seismic and geodetic datasets. This result is a significant step forward in reconciling petrological and geophysical interpretations of magma transport during volcano-tectonic episodes, and provides a critical framework for the interpretation of premonitory seismic and geodetic data in volcanically active regions.

Keywords: Crystallization; Holuhraun; Iceland; Melt barometry; Melt inclusions.