2025年桑托里尼附近的地震群由脉冲岩浆引发,揭示了两座火山之间的隐藏联系,但没有发生火山喷发。 A 2025 quake swarm near Santorini, caused by pulsing magma, revealed a hidden link between two volcanoes, but no eruption occurred.

一项新研究显示,在圣托里尼附近,2025年地震群聚集,涉及25 000多个地震,其起因是岩浆通过深层地壳骨折移动,造成地震群涌动。 A 2025 earthquake swarm near Santorini, involving over 25,000 quakes, was caused by pulsing magma moving through deep crustal fractures, a new study reveals. 利用机器学习和全球定位系统数据,研究人员发现岩浆从连接圣托里尼火山口和科隆博水下火山的共用地下水库中涌出,引起引发地震的压力。 Using machine learning and GPS data, researchers found magma surged from a shared underground reservoir linking Santorini’s caldera and the Kolumbo underwater volcano, generating stress that triggered the quakes. 尽管岩浆体积相当于200 000个奥林匹克游泳池,但它缺乏爆发的压力。 Though the magma volume equaled 200,000 Olympic pools, it lacked pressure to erupt. 研究结果发表在《科学》上,排除了构造断层滑坡,为监测偏远或水下火山地区的动乱提供了新方法。 The findings, published in Science, rule out tectonic fault slip and offer a new method to monitor unrest in remote or underwater volcanic zones.