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在Awash Melkesa的地下地质物理分析:洞察石质和资源潜力的洞察力

Eyayu Ayalew Dessalew^1,2, Tilahun Mamo², Mohammed Yesuf Ali¹

¹Department of Geology, College of Natural Science, Wollo University, Dessie, Ethiopia.

|October 6, 2025

概括

在Awash Melkesa的地质调查显示了具有含水层潜力的破碎火岩. 磁性和放射性数据也表明断层和矿物度,为地下资源提供了洞察力.

科学领域:

地质物理学地质物理学
水文地质学水文地质学
地质地质地质地质地质地

背景情况:

阿瓦什·梅尔克萨位于亚的斯亚贝巴东南106公里处.
综合地质物理研究对于了解地表特征至关重要.

研究的目的:

为了研究Awash Melkesa地区的地下地质物理特性.
识别潜在的地下水资源和地质结构.

主要方法:

使用电电阻,磁,放射和地震折射方法.
数据分析包括地缘电气分析,残余磁异常映射,倾斜衍生分析和地震速度建模.

主要成果:

一个低电阻区域表明破裂的火晶石表明了含水层潜力.
磁力数据显示出与吉断层带一致的断层.
放射测量数据显示,与岩石类型相关的和度的变化.

结论:

该研究成功地划分了地下层,并确定了含水层潜力很高的区域.
地质物理数据提供了关于Awash Melkesa地区地质结构和矿物分布的见解.

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