在波数域中使用重力和重力梯度的3D密度成像及其在Decorah中的应用
Huiyou He1,2, Jian Fang3, Dongmei Guo1
1State Key Laboratory of Geodesy and Earth's Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, 340 Xudong Road, Wuhan, 430077, China.
Scientific reports
|January 3, 2024
概括
这项研究使用重力和重力梯度数据展示了3D密度成像. 该方法准确地重建了地下密度,揭示了Decorah地区的地质结构和侵入性途径.
科学领域:
- 地质物理学 地质物理学
- 地质成像 - - 地质成像
背景情况:
- 密度成像是一种用于地下勘探的地球物理方法.
- 它涉及在波数域中逆转重力和重力梯度光谱.
研究的目的:
- 评估3D密度成像的准确性和效率.
- 在Decorah地区应用详细地质分析的方法.
主要方法:
- 在波数域中利用了重力和重力梯度光谱的反转.
- 在理论数据和噪声添加数据上使用深度权衡,用于3D密度重建.
- 将该技术应用于Decorah地区的地质物理数据.
主要成果:
- 生成精确的3D密度模型,与理论数据一致.
- 成功识别了高密度的Decorah复合体和侵入性岩石质量.
- 在研究区域内绘制低密度状侵入性岩石的地图.
结论:
- 证实了3D密度成像的有效性和计算效率.
- 提供了对迪科拉地区侵入性路径和结构划分的见解.
- 支持更深入地了解该地区的地质演变.
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