沙特阿拉伯沙特国王大学的剪切波速度结构,来自MASW和微震阵列
1Department of Geology and Geophysics, College of Science, King Saud University, 11451, Riyadh, Saudi Arabia. khassanein@ksu.edu.sa.
Scientific reports
|April 3, 2025
概括
沙特国王大学的地质调查显示,对于地震地点的分类至关重要的是不同的土壤层. 该研究确定了弱势区域,强调了剪切波速度对地质技术评估和可持续发展的重要性.
科学领域:
- 地质物理学 地质物理学
- 地质技术工程 地质技术工程
- 工程地震学 工程地震学
背景情况:
- 剪波速度 (Vs) 是评估土壤强度和岩石机械性能的一个关键参数.
- 了解地下条件对于地震现场分类和基础设施开发至关重要.
研究的目的:
- 在沙特国王大学遗址描述地下层并确定剪切波速度.
- 评估潜在的地质技术问题,并确定弱点区域.
- 评估地质物理方法的有效性,以确定地点的特征.
主要方法:
- 表面波多通道分析 (MASW) 调查.
- 微震测量 微震测量 微震测量 微震测量
- 地工学钻井调查. 地工学钻井调查.
主要成果:
- 根据剪切波速度 (Vs) 和国家地震危险降低计划 (NEHRP) 的分类,确定了三种不同的地下层:C地 (泥沙),B地 (风化石灰岩) 和A地 (紧石灰岩).
- 床岩深度在整个地点各不相同,在中央区域最浅.
- 在2-25米深处检测到弱区域,表明潜在的地质技术风险.
- 微震测量证实了VS和基岩深度的MASW结果.
结论:
- 地质物理技术,特别是MASW和微震分析,对于详细的地点表征是有效的.
- 已确定的地下层和弱区对地震设计和城市规划有重大影响.
- 整合剪波速度数据支持为可持续城市发展和基础设施弹性做出明智决策.
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