在意大利南部的地震异构学研究石层规模的构造结构和地幔动力学
L Scarfì1, M Firetto Carlino2, C Musumeci2
1Istituto Nazionale di Geofisica e Vulcanologia - Osservatorio Etneo, Catania, Italy. luciano.scarfi@ingv.it.
Scientific reports
|November 28, 2023
概括
地震波分裂揭示了意大利下面的上层地幔结构. 不同类型的图案表明板块不连续性和断层系统,突出了地震不同类型在理解延伸到上层地幔的构造结构中的作用.
科学领域:
- 固体地球地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 俯冲区具有深层构造结构,影响上层板块断层和岩.
- 通过远震相研究上层地幔的异构性有助于理解地力学框架和断层根源.
研究的目的:
- 分析地中海中部的地震波分裂 (XKS),重点关注亚得里亚海-离子河流系统.
- 为了研究上层地幔的异质性模式及其与意大利南部构造结构的关系.
主要方法:
- 对XKS波分裂的分析.
- 测量快速波极化方位 (快速方向) 的测量.
- 地震异构模式与已知的地和地幔结构的相关性.
主要成果:
- 快速方向通常是与沟平行,归因于潜水板.
- 意大利中部和西西里的垂直快速方向表明板块不连续性.
- 意大利中部的逐渐旋转表明状地幔流通过板块撕裂,而西西里则显示与地结构和潜伏转变边缘传播器断层系统相关的突然变化.
结论:
- 在西西里岛上层地幔异构度的急剧变化突显了潜起变形边缘传播器断层系统在细分碰撞边缘方面的主要作用.
- 地震异构性研究对于确定构造结构是否局限于地或延伸到上层地幔至关重要.
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