2024年7.4级卡拉马地震的深层板块内部破裂和机制过渡
Zhe Jia1, Wei Mao2,3, María Constanza Flores4,5
1Institute for Geophysics, Jackson School of Geosciences, UT Austin, Austin, USA. zjia@ig.utexas.edu.
Nature communications
|August 30, 2025
概括
虽然地震深度中等, 但往往被忽视, 这项研究揭示了2024年智利地震可能是由脱水脆化引起的,并通过热失控传播,突出了复杂的破裂机制.
科学领域:
- 地球科学
- 地震学
- 地质学
背景情况:
- 地震的深度 (70-300公里) 在沉降板块中构成重大危险,但它们的基础物理仍然不清楚.
- 虽然巨大的冲击事件主导着俯冲区的危险评估,但中等深度的地震也可能产生毁灭性的影响.
- 这些事件的拟议机制包括脱水脆化和热失控,但直接证据和机制之间的过渡尚不清楚.
研究的目的:
- 调查2024年智利7.4级中级地震的破裂物理.
- 为了比较地震的破裂程度与热力学模型的温度条件.
- 阐明破裂机制的转变及其对地震危害的影响.
主要方法:
- 区域地质测量与地震变形数据的分析
- 与事件相关的高分辨率地震分析.
- 观察到的破裂程度与板块温度的热力学模型的比较.
主要成果:
- 2024年智利地震呈现出一个复杂的破裂在一个特殊的深度范围,度延伸到深沉的石化层.
- 破裂始于冷板芯,但扩散到超过~650°C的异温,这是有效的蛇形脱水的典型极限.
- 证据表明,最初的破裂机制是脱水脆化,随后通过剪切热逃生传播.
结论:
- 中等深度地震破裂可能涉及脱水脆化和热失控机制之间的过渡.
- 这种过渡促进了大规模的破裂,并可以激活潜水板内的典型无地震,高温区域.
- 了解破裂机制,板块热条件和构成的相互作用对于评估中等深度地震危险至关重要.
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