航磁三分量向上延拓在判断地质体物性参数上的应用研究

李西子, 郭华, 韩松, 刘浩军, 郑强

The application of aeromagnetic three-component upward continuation to recognizing physical parameters of geological body

Xi-Zi LI, Hua GUO, Song HAN, Hao-Jun LIU, Qiang ZHENG

图6 第二组模型等值线 a—A组模型北向分量延拓前等值线; b—A组模型北向分量上延708 m后的等值线; c—A组模型北向分量上延4 956 m后的等值线; d—B组模型北向分量延拓前等值线; e—B组模型北向分量上延590 m后的等值线; f—B组模型北向分量上延826 m后的等值线; g—B组模型北向分量上延4 248 m后的等值线

Fig.6 Contour map of the second group model a—the contour map of A group model's north-component before continuation;b—the contour map of A group model's north-component after continuation 708 m;c—the contour map of A group model's north-component after continuation 4 956 m;d—the contour map of B group model's north-component before continuation;e—the contour map of B group model's north-component after continuation 590 m;f—the contour map of B group model's north-component after continuation 826 m;g—the contour map of B group model's north-component after continuation 4 248 m