Geological Society of America

T82 Source to Surface Magma Thermodynamics and Transport: Interdisciplinary Approaches to Documenting the How, Where, and When of Magma Generation and Evolution during Ascent, Storage, and Eruption I

Monday, 10 October 2022
8:00 AM - 12:00 PM
502

EXPLOSIVE ACTIVITY ON KĪLAUEA’S LOWER EAST RIFT ZONE FUELLED BY A VOLATILE-RICH, DACITIC MELT

Paper number: T82-5
Program: Technical Sessions
Time: 8:50 AM – 9:10 AM

Authors

Penny Wieser Presenting Author
UC Berkeley, Berkeley, CA
Marie Edmonds
University of Cambridge, Cambridge
Cheryl Gansecki
University of Hawaii - Hilo, Hilo, HI
John Maclennan
University of Cambridge, Cambridge
Frances E. Jenner
The Open University, Milton Keynes, N/A
Barbara E. Kunz
The Open University, Milton Keynes, N/A
Paula Antoshechkina
California Institute of Technology, Pasadena, CA
Frank Trusdell
Hawaiian Volcano Observatory, Hilo, HI
Lopaka Lee
U.S. Geological Survey, Hawaii National Park, HI

Abstract

Magmas with matrix glass compositions ranging from basalt to dacite erupted from a series of 24 fissures in the first two weeks of the 2018 Lower East Rift Zone (LERZ) eruption of Kīlauea Volcano. Eruption styles ranged from low spattering and fountaining, to strombolian activity. The combination of strombolian activity and highly evolved compositions is unprecedented in historic eruptions at Kīlauea. Major element trajectories in matrix glasses and melt inclusions hosted by olivine, pyroxene and plagioclase are consistent with variable amounts of fractional crystallization, with incompatible elements (e.g., Cl, F, H₂O) becoming enriched by 4-5 times as melt MgO contents evolve from 6 to 0.5 wt%. MELTS modelling of fractional crystallization and volatile exsolution during magma ascent demonstrates that the high viscosity and high H₂O contents (~2 wt%) of the dacitic melts erupting at Fissure 17 account for the observed explosive Strombolian behaviour, in contrast to the low fountaining and spattering observed at fissures erupting basaltic to basaltic-andesite melts. Saturation pressures calculated from melt inclusions CO₂-H₂O contents indicate that the magma reservoir(s) supplying these fissures was located at ~2-3 km depth, which is in agreement with the depth of a dacitic magma body intercepted during drilling in 2005 (~2.5 km) and a seismically-imaged low Vp/Vs anomaly (~2 km depth). Nb/Y ratios in erupted products are similar to lavas erupted between 1955-1960, indicating that melts were stored and underwent variable amounts of crystallization in the LERZ for >60 years before being remobilized by a dike intrusion in 2018. We demonstrate that extensive fractional crystallization generates viscous and volatile-rich magma with potential for hazardous explosive eruptions, which may be lurking undetected at many ocean island volcanoes.

Geological Society of America Abstracts with Programs. Vol. 54, No. 6

doi: 10.1130/abs/2022AM-379565

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