本文详细地论述了大地电磁阵列剖面法的基本原理、野外数据采集和资料处理方法。
The basic principle, data acquisition and data processing of the electromagnetic array profiling (EMAP) are minutely discussed in this paper.
理论和实践都表明，该反演方法比同步阵列大地电磁测深(SAMT)和连续电磁剖面法(CEMP)等MT方法的效果更佳。
The theory and the practice show that the inversion method has better results than synchronized array MT sounding (SAMT) and continuous electromagnetic profiling (CEMP).
理论和实践都表明，该反演方法比同步阵列大地电磁测深(SAMT)和连续电磁剖面法(CEMP)等MT方法的效果更佳。
The theory and the practice show that the inversion method has better results than synchronized array MT sounding (SAMT) and continuous electromagnetic profiling (CEMP).
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