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.
实现大地电磁法快速三维反演的关键在于找到快速计算灵敏度矩阵的方案。
The crucial step in doing 3d inversion for the magnetotelluric method is to find an effective way to calculate the sensitivity matrix.
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