The crustal thickness from East China Sea to North Fiji Basin was calculated on the basis of the actually measured water depth and the gravimetric data from continuousprofiling.
根据我们实测的水深、重力 连续 剖面资料,计算了自东海至北斐济盆地的地壳厚度。
2
The theory and the practice show that the inversion method has better results than synchronized array MT sounding (SAMT) and continuous electromagnetic profiling (CEMP).