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首页> 外文期刊>Exploration Geophysics >Aeromagnetic 3D subsurface imaging with effective source volume minimisation and its application to data from the Otoge cauldron, Shitara, Central Japan
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Aeromagnetic 3D subsurface imaging with effective source volume minimisation and its application to data from the Otoge cauldron, Shitara, Central Japan

机译:有效减少源体积的航空3D地下成像技术及其在来自日本中部十谷市Otoge大锅的数据中的应用

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摘要

Three-dimensional (3D) imaging techniques using the conjugate gradient solution are discussed for magnetic anomaly source reconstruction, especially for areas of rugged terrain, such as those of volcanoes. The analysis model configuration permits surface undulation and variable depth slicing. First, primitive source model data are put into the analysis to confirm the characteristic behaviour of the regularisation methods and parameter scaling. The compact regularisation method is then applied to synthetic geologic models to understand the resolving power of the method given the problem of the inherent weakness of a non-unique solution. Finally, the field data of a helicopter-borne magnetic survey of the Otoge cauldron are put into the 3D imaging analysis with the method. The analysis reveals a quite reasonable subsurface image of the magma reservoir and the Otoge cone sheets and Otoge stocks of post-cauldron activity, as inferred from geological studies.
机译:讨论了使用共轭梯度解的三维(3D)成像技术,用于磁异常源的重建,尤其是对于崎terrain地形的区域,如火山区域。分析模型配置允许表面起伏和可变深度切片。首先,将原始源模型数据放入分析中,以确认正则化方法和参数缩放的特征行为。考虑到非唯一解的固有弱点问题,将紧凑的正则化方法应用于合成地质模型,以了解该方法的解析能力。最后,使用该方法将Otoge大锅的直升机磁测的场数据放入3D成像分析中。分析显示,从地质研究中可以得出岩浆储层,奥托格锥板和大锅后活动的奥托格储层的相当合理的地下图像。

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