在仪器和处理解释技术方面的进展使得大地电磁法现在能够快速采集大地电磁数据并进行二维或三维地质模型解释。
Developments in instrumentation and analysis techniques now permit MT data to be collected rapidly and interpreted in terms of two dimensional and three dimensional Earth models.
处理了典型重磁异常二维及三维及三维地质模型，给出了各模型的处理结果及误差曲线；
The typical 2D and 3D gravitational magnetive anomalies models are processed, and the results and error curves from the typical models are given.
处理了典型重磁异常二维及三维及三维地质模型，给出了各模型的处理结果及误差曲线；
The typical 2D and 3D gravitational magnetive anomalies models are processed, and the results and error curves from the typical models are given.
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