The method converges faster than conventional successive approximation method (SAM) and can be applied to high conductivity contrast formation.
与传统的逐次逼近解法(SAM)相比，该方法收敛性强，应用范围广，可适用于高电导率对比地层。
The method converges faster than conventional successive approximation method (SAM) and can be applied to high conductivity contrast formation.
与传统的逐次逼近解法(SAM)相比，该方法收敛性强，应用范围广，可适用于高电导率对比地层。
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