Seismic characteristics of the April 2024 eruption of Ruang Volcano, North Sulawesi, Indonesia

IF 2.5 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Journal of Volcanology and Geothermal Research Pub Date : 2026-04-01 Epub Date: 2026-01-29 DOI:10.1016/j.jvolgeores.2026.108537
Sri Hidayati , Hetty Triastuty , Sulistiyani Sulistiyani , Wendy A. McCausland , Christina Widiwijayanti , Martanto Martanto , Sofyan Primulyana , Heruningtyas Desi Purnamasari , P. Hadi Wijaya
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Abstract

The two most recent eruptions of Ruang volcano, in 2002 and 2024, have been large (VEI 4) with very short precursory periods, 3 and 6 days, respectively. Background seismicity at Ruang volcano is generally low with 0–2 volcano-tectonic (VT) earthquakes per day. The 2024 eruptions were preceded by a notable increase in VT earthquakes from 11 to 15 April with a rapid escalation from 16 to 17 April in the form of increased VT swarms, and the appearance of low frequency earthquakes and short bursts of VT drumbeats shortly before the eruption. Similar VT seismic unrest was recorded in March 2015, May 2016, and April 2022, although none of these episodes culminated in an eruption. A comparison of seismic energy release between April 2022 and April 2024 shows distinct differences. In 2024, cumulative seismic energy reached its peak within 5 days, just before the onset of eruption on 17 April. In contrast, during the 2022-episode, energy release followed a more gradual increase over 8 days peaking on 16 April, then declining gradually without leading to eruption. Notably, low frequency (LF) and drumbeat earthquakes were absent in non-eruptive unrest episodes. The transition to proximal LFs in 2024 likely signals pressure fluctuations, intensified magma degassing, and conduit formation, acting as an important precursor to eruption. Additionally, the occurrence of short bursts of drumbeat seismicity likely reflects the onset of the shallow magma ascent and was an important short-term precursor to the eruption. Finally, we examine the potential influence of regional tectonic earthquakes on the escalation of precursory unrest in 2024.
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印度尼西亚北苏拉威西Ruang火山2024年4月喷发的地震特征
阮氏火山最近的两次喷发分别发生在2002年和2024年,规模很大(VEI 4),前兆周期非常短,分别为3天和6天。黄山火山背景地震活动性一般较低,每天发生0-2次火山构造地震。在2024年火山爆发之前,4月11日至15日,VT地震显著增加,4月16日至17日,VT群增加,出现低频地震和短时间的VT鼓点爆发。2015年3月、2016年5月和2022年4月都记录到了类似的VT地震动荡,尽管这些事件都没有以火山喷发告终。2022年4月和2024年4月的地震能量释放对比显示出明显的差异。在2024年,累积地震能量在5天内达到峰值,就在4月17日爆发之前。与此相反,在2022年期间,能量释放在8天内逐渐增加,在4月16日达到峰值,然后逐渐下降,但没有导致喷发。值得注意的是,在非喷发性动乱事件中没有低频地震和鼓状地震。2024年向近端LFs过渡可能标志着压力波动、岩浆脱气加剧和管道形成,是喷发的重要前兆。此外,鼓状地震活动的短暂爆发可能反映了浅层岩浆上升的开始,是喷发的重要短期前兆。最后,分析了2024年区域构造地震对前兆动荡升级的潜在影响。
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来源期刊
CiteScore
5.90
自引率
13.80%
发文量
183
审稿时长
19.7 weeks
期刊介绍: An international research journal with focus on volcanic and geothermal processes and their impact on the environment and society. Submission of papers covering the following aspects of volcanology and geothermal research are encouraged: (1) Geological aspects of volcanic systems: volcano stratigraphy, structure and tectonic influence; eruptive history; evolution of volcanic landforms; eruption style and progress; dispersal patterns of lava and ash; analysis of real-time eruption observations. (2) Geochemical and petrological aspects of volcanic rocks: magma genesis and evolution; crystallization; volatile compositions, solubility, and degassing; volcanic petrography and textural analysis. (3) Hydrology, geochemistry and measurement of volcanic and hydrothermal fluids: volcanic gas emissions; fumaroles and springs; crater lakes; hydrothermal mineralization. (4) Geophysical aspects of volcanic systems: physical properties of volcanic rocks and magmas; heat flow studies; volcano seismology, geodesy and remote sensing. (5) Computational modeling and experimental simulation of magmatic and hydrothermal processes: eruption dynamics; magma transport and storage; plume dynamics and ash dispersal; lava flow dynamics; hydrothermal fluid flow; thermodynamics of aqueous fluids and melts. (6) Volcano hazard and risk research: hazard zonation methodology, development of forecasting tools; assessment techniques for vulnerability and impact.
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