固化古代岩的破裂阻碍了之前的群体迁移,导致了2024年诺托地震
Ryota Takagi1, Keisuke Yoshida1, Tomomi Okada1
1Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan.
Science advances
|October 15, 2025
概括
一个通过地震成像识别的凝固的岩体,作为控制地震群和2024年诺托半岛地震破裂的屏障. 古代火山活动影响了断层透性和地震发生.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 火山学 火山学是一门学科.
背景情况:
- 2024年诺托半岛地震 (Mw 7.5) 之前发生了一次强烈的,约3年的地震群.
- 地震群演变和断裂动态中的空间复杂性仍然不太了解.
研究的目的:
- 研究控制地震群演变和破裂的空间复杂性的因素.
- 了解地下结构在2024年诺托半岛地震发生中的作用.
主要方法:
- 利用高分辨率的地下成像技术.
- 采用密集的地震观测网络.
- 分析地震数据以确定地下结构及其属性.
主要成果:
- 确定了一个高速度的物体,与2024年地震的主要滑动区域保持一致.
- 之前的地震群避开了这种高速运动的物体.
- 这颗被认为是凝固的古老岩的高速物体,作为流体迁移的不透屏障.
- 这种岩体最终破裂,在主震中起到了性作用.
结论:
- 地下层的异质性,特别是古老的火山入侵,显著控制了断层区域的透性.
- 这种透性的异质性决定了地震群的演化和大地震的产生.
- 古代火山活动 (>1500万年前) 影响了2024年诺托半岛地震的特征.
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