新西兰陶普火山十年来的地震活动

IF 2.5 Q2 Earth and Planetary Sciences
F. Illsley‐Kemp, P. Herath, C. Chamberlain, Konstantinos Michailos, C. Wilson
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引用次数: 1

摘要

新西兰陶普火山是一座活跃的破火山口,近年来平均每500年爆发一次,最近一次爆发时间为232±10 CE。Taupō的监测具有挑战性,因为有记录的历史上没有爆发活动;然而,陶普确实经历了大约十年的动荡时期,比如2019年。识别这些动乱时期的关键是了解什么是“正常”的动乱活动。在这项研究中,我们为陶普生成了2010-2019年的地震目录,包括46481次地震。这表明,陶普地区的背景地震率为每月50-200次,在2019年动乱之前,地震率呈指数级增长。我们还表明,当考虑衰减时,没有证据表明陶普发生低频地震,这是火山监测和确定是否存在重大岩浆运动的重要考虑因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A decade of earthquake activity at Taupō Volcano, New Zealand
Taupō, New Zealand, is an active caldera volcano that in recent times has erupted on average every ~500 years, with the latest explosive eruption in 232±10 CE. Monitoring at Taupō is challenging as there has been no eruptive activity in documented history; however, Taupō does undergo periods of unrest on roughly a decadal timescale, such as in 2019. Key to identifying these unrest periods is understanding what represents 'normal' inter-unrest activity. In this study, we generate an earthquake catalogue for Taupō for 2010–2019 inclusive, consisting of 46,481 earthquakes. This shows that the Taupō region has background earthquake rates of 50–200 earthquakes per month and the 2019 unrest episode was preceded by an exponential increase in earthquake rate. We also show that when attenuation is accounted for there is no evidence for low-frequency earthquakes at Taupō, and that this is an important consideration for volcano monitoring and determining the presence of significant magma movement.
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来源期刊
Volcanica
Volcanica Earth and Planetary Sciences-Geology
CiteScore
4.40
自引率
0.00%
发文量
21
审稿时长
21 weeks
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