Pu Hsin-Chieh, Lin Cheng-Horng, Lai Ya-Chuan, Shih Min-Hung, Li Yi-Heng
Seismological Center, Central Weather Administration, 64, Gongyuan Road, Taipei, 100006, Taiwan.
Institute of Earth Sciences, Academia Sinica, 128, Sec. 2, Academia Road, Nankang, Taipei, 115201, Taiwan.
Sci Rep. 2025 May 25;15(1):18220. doi: 10.1038/s41598-025-02345-9.
The Tatun Volcano Group (TVG) is in close proximity to the Taipei metropolitan area, which is home to over 7 million residents. Although there has been no recorded volcanic eruption in the TVG throughout human history, recent seismic observations suggest that it may still be active. To investigate possible volcanic seismicity and activity in the TVG, we conducted a 4-dimensional seismic tomography study using abundant seismic data collected from 2014 to 2021. We obtained 3D seismic velocity structures to examine both the temporal and spatial variations in seismicity each year. Our results show that the dramatic increase in seismicity in 2019 followed an increase in P-wave seismic velocity in the Dayoukeng fumarole area and Mt. Chihsin in 2018. This increase in seismic velocity may have been caused by rocks or sediments subjected to higher pressure beneath the TVG, resembling a pressure cooker on a flame. Thus, the sequential rise in both seismic velocity and seismicity strongly suggests that careful monitoring of temporal velocity variations in the volcanic area might provide an early warning of potential seismic swarms or volcanic activity in the future.
大屯火山群(TVG)紧邻台北都会区,该地区有超过700万居民。尽管在人类历史上大屯火山群没有记录到火山喷发,但最近的地震观测表明它可能仍处于活跃状态。为了调查大屯火山群可能存在的火山地震活动,我们利用2014年至2021年收集的大量地震数据进行了四维地震层析成像研究。我们获得了三维地震速度结构,以研究每年地震活动的时空变化。我们的结果表明,2019年地震活动的急剧增加之前,2018年大油坑喷气孔区和七星山的P波地震速度有所增加。地震速度的增加可能是由大屯火山群下方承受更高压力的岩石或沉积物引起的,类似于放在火焰上的高压锅。因此,地震速度和地震活动的相继上升强烈表明,密切监测火山区的时间速度变化可能为未来潜在的地震群或火山活动提供早期预警。