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DOI | 10.1126/science.aba4798 |
Deep long-period earthquakes generated by second boiling beneath Mauna Kea volcano | |
Wech A.G.; Thelen W.A.; Thomas A.M. | |
发表日期 | 2020 |
ISSN | 0036-8075 |
起始页码 | 775 |
结束页码 | 779 |
卷号 | 368期号:6492 |
英文摘要 | Deep long-period earthquakes (DLPs) are an enigmatic type of volcanic seismicity that sometimes precedes eruptions but mostly occurs at quiescent volcanoes. These earthquakes are depleted in high-frequency content and typically occur near the base of the crust. We observed a near-periodic, long-lived sequence of more than one million DLPs in the past 19 years beneath the dormant postshield Mauna Kea volcano in Hawai‘i. We argue that this DLP sequence was caused by repeated pressurization of volatiles exsolved through crystallization of cooling magma stalled beneath the crust. This “second boiling” of magma is a well-known process but has not previously been linked to DLP activity. Our observations suggest that, rather than portending eruptions, global DLP activity may more commonly be indicative of stagnant, cooling magma. Copyright © 2020 The Authors. |
关键词 | crystallizationearthquakemagmaseismicityvolcanic eruptionHawaii [(ISL) Hawaiian Islands]Hawaii [United States]Hawaiian IslandsMauna Keaarticlecoolingcrystallizationearthquakevolcano |
语种 | 英语 |
来源机构 | Science |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/133493 |
推荐引用方式 GB/T 7714 | Wech A.G.,Thelen W.A.,Thomas A.M.. Deep long-period earthquakes generated by second boiling beneath Mauna Kea volcano[J]. Science,2020,368(6492). |
APA | Wech A.G.,Thelen W.A.,&Thomas A.M..(2020).Deep long-period earthquakes generated by second boiling beneath Mauna Kea volcano.,368(6492). |
MLA | Wech A.G.,et al."Deep long-period earthquakes generated by second boiling beneath Mauna Kea volcano".368.6492(2020). |
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