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Interevent Seismicity Statistics Associated With the 2018 Quasiperiodic Collapse Events at Kīlauea, HI, USA.

Authors :
Fildes, Rebecca A.
Kellogg, Louise H.
Turcotte, Donald L.
Rundle, John B.
Source :
Earth & Space Science. Mar2020, Vol. 7 Issue 3, p1-12. 12p.
Publication Year :
2020

Abstract

Following the Mw 6.9 Hawaiian earthquake on 4 May 2018, a remarkable quasiperiodic sequence of collapse events began at Halema'uma'u Crater at the summit of Kīlauea Volcano. The collapse events were associated with the drainage of magma from beneath the summit to the Lower East Rift Zone where fissure eruptions occurred. From 4 June 2018 to 2 August 2018 forty‐seven collapse events Mw 5.3 ± 0.1 occurred with the same temporal pattern of seismicity occurring between sequential pairs of collapse events. This paper focuses on this interevent seismicity pattern. Following a collapse event, there was a relatively quiescent period. This was followed by a sudden increase in seismicity, occurring at a nearly linear rate of 397 ± 96 earthquakes per day. These seismically active periods lasted until the next collapse event occurred. The pattern then repeated itself beginning again with postcollapse quiescence. We provide a statistical summary of this seismicity behavior by isolating the quiescent and active times to look at immediate precollapse and postcollapse activity. In mid‐June there were significant changes in the quiescent time lengths (decreased), the number of earthquakes during the interevent times (increased), and the rates of seismicity during the active times (increased). This type of interevent study could be conducted with other seismically well recorded, sequential caldera collapse events and also with other data types to look for potential physical explanations and an improved understanding of precollapse and postcollapse activity. Key Points: The same pattern of seismically quiescent and active periods occurred between every pair of collapse events at the summitThe active times had linear rates of seismicity, and the quiescent times had fewer earthquakesFollowing a large increase in June 2018, there was a general decrease in the active time seismicity rates until the end of the sequence [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
23335084
Volume :
7
Issue :
3
Database :
Academic Search Index
Journal :
Earth & Space Science
Publication Type :
Academic Journal
Accession number :
142417566
Full Text :
https://doi.org/10.1029/2019EA000766