构造和动态过程的相互作用塑造了南中阿佩尼尼斯的多层延伸系统
Rita de Nardis1,2, Alessandro Vuan3,4, Luca Carbone5,6
1University of Chieti-Pescara, via dei Vestini 31, 66100, Chieti, Italy. rita.denardis@unich.it.
Scientific reports
|August 7, 2024
概括
2009年L'Aquila地震引发了微地震性,揭示了流体循环和一个深深的NNE-dipping断层区域. 这有助于更好地了解意大利高风险的阿宁地区的地震过程.
科学领域:
- * 地震学和构造学
- * 地质学和流体动力学
背景情况:
- *高危地震区域具有低地震性,这挑战了目前的理解.
- * 在2009年L'Aquila震 (MW 6.3) 之后,南中阿佩尼尼河经历了显著的地震活动.
研究的目的:
- * 综合分析L'Aquila震后的地震群和地震序列.
- * 调查流体循环和深层断层结构在地震活动中的作用.
- * 增强对扩展领域的地震构造过程的理解.
主要方法:
- * 增强了地震目录的创建,揭示了微地震性到ML 0.
- *对地震群,扩散率和Vp/Vs比率的分析.
- * 3D地震测绘与地质数据集成.
主要成果:
- *L'Aquila主震可能引发的微震性,影响断层特性.
- * 液体循环的证据表明高Vp/Vs值 (>1.88) 和扩散性.
- *在11-15公里的深度和更深的地震力确定了一个NNE浸入变形区域,这表明地幔CO2上升.
结论:
- * 流体参与在触发和维持延伸环境中的地震活动中起着至关重要的作用.
- * 该研究揭示了之前未知的断层系统和变形区域的几何方面.
- * 发现为高风险的阿佩宁山脉的地震构造环境提供了关键的见解.
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