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《科学》 第393卷 第6817期 · 2026年9月17日 · 中文解读

朝鲜核试验引发地幔山断层持续复活

SEISMOLOGY Nuclear tests at Mt. Mantap have reactivated intraplate faults · Xingli Fan, Kwang-Hee Kim, Su Young Kang, Lanbo Liu, Jie Song, Yujin Sohn, Hyeong-Tae Jou, Qi-Fu Chen, Le Li, Lian-Feng Zhao, Yuan Wang, Tianyao Hao
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这篇讲什么
本文基于2008年以来的区域地震波形数据,分析了朝鲜丰溪里核试验场万塔山周边地震活动的时空演化,发现2017年最后一次大当量核爆后地震活动持续增强并沿断层构造分布,表明地下核试验可驱动多年尺度的断层复活。
原文开头
Xingli Fan1*†, Kwang- Hee Kim2*†, Su Young Kang3, Lanbo Liu3,4, Jie Song1, Yujin Sohn2, Hyeong- Tae Jou3, Qi- Fu Chen5,6, Le Li7, Lian- Feng Zhao5,6, Yuan Wang6,8, Tianyao Hao6,8 Underground nuclear explosions typically produce short- lived seismic sequences that decay rapidly after testing ceases. by contrast, seismicity near the punggye- ri nuclear test site at mt. mantap in the Democratic people’s republic of Korea has persisted and intensified for years after the final large- yield explosion in 2017, evolving from diffuse activity to spatially organized distribution along fault- controlled structures. Analysis of 17 years of continuous waveform data reveals a progressive increase in seismicity and delayed reactivation of shallow faults. …
摘自《科学》(Science)第393卷 第6817期 · 2026年9月17日,Xingli Fan, Kwang-Hee Kim, Su Young Kang, Lanbo Liu, Jie Song, Yujin Sohn, Hyeong-Tae Jou, Qi-Fu Chen, Le Li, Lian-Feng Zhao, Yuan Wang, Tianyao Hao。仅引用开头一小段供了解文章,版权归原刊所有,全文请阅读原刊。
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