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arXiv · 2011.06974

Negative isotropic seismic moment tensors, migrating and cyclic seismicity during the 2018 summit collapse at K\={\i}lauea caldera

Celso R. Alvizuri·Robin S. Matoza·Paul G. Okubo
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Abstract

The 2018 rift zone eruption of K\={\i}lauea volcano was accompanied by a remarkable and episodic collapse of its summit. Between May-August the eruption and collapse sequence included over 70,000 earthquakes (M$\geq$0) and 54 major earthquakes (M$\geq$5). We analyzed the seismicity in the K\={\i}lauea summit region and estimated seismic full moment tensors with their uncertainties for the 54 M$\geq$5 events. These events occurred at almost daily intervals and were accompanied by intense seismicity which was concentrated between 0-3 km depths beneath the Halema`uma`u pit crater. The hypocenters reveal partial elliptical patterns (map view) that migrated downward by $\sim$200 m. The moment tensors reveal remarkably consistent mechanisms, with negative isotropic source types and localized uncertainties, and vertical P-axis orientations. From the moment tensors we derived Poisson's ratios which are variable ($\nu=0.1-0.3)$ for the first half of the collapse events and converged to $\nu\sim0.28$ from June 26 onward.

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Celso R. Alvizuri, Robin S. Matoza, Paul G. Okubo. 2020-11-13. Negative isotropic seismic moment tensors, migrating and cyclic seismicity during the 2018 summit collapse at K\={\i}lauea caldera. https://arxiv.org/abs/2011.06974

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