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10 第三组模型等值线 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472 m后的等值线; c—A组模型北向分量上延3 540 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826 m后的等值线; f—B组模型北向分量上延3 540 m后的等值线

Fig.10 Contour map of the third 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 472 m;c—the contour map of A group model's north-component after continuation 3 540 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 826 m;f—the contour map of B group model's north-component after continuation 3 540 m