1) terrestrial electricity
地电;大地电
2) MT
大地电磁
1.
RESEARCH ON INVERSION OF MT3D MODEL APPROXIMATELY BY 1D,2D INVERSION METHOD;
大地电磁三维模型的一维二维反演近似问题研究
2.
RESEARCH ON MT CURVE DISTORTION BY SURFACE ELECTRIC BODY;
表层电性不均匀对大地电磁测深曲线的畸变研究
3.
An improved MT topographic correction method and discussion on relative issues;
一种改进的大地电磁地形校正方法及相关问题探讨
3) ground potential survey
大地电位
1.
Four fundamental methods are introduced,namely well temperature,ground potential survey,microearthquake and radioactivity isotope,which were used to monitor the fracture geometry of fractured coalbed methane wells in North China.
介绍了井温测试法、放射性同位素法、大地电位测试法和微地震测试法监测煤层水力压裂裂缝的基本原理。
4) magnetotelluric
[mæɡ,ni:təute'lurik]
大地电磁
1.
A 2-D fast magnetotelluric forward method;
一种快速二维大地电磁正演方法
2.
The application of PC104 in sea-floor magnetotelluric signal acquisition;
PC104嵌入式计算机在海底大地电磁信号采集中的应用
3.
Three Dimentional Magnetotelluric Forward Modeling Using Integral Equation;
利用积分方程法的大地电磁三维正演
5) magnetotellurics
大地电磁
1.
Because of currently more general earth magnetotellurics (MT) 3D non-homogeneous problem having not get good resolve, we still do 1D and 2D forward and inversion explanation under most circumstances.
由于大地电磁(MT)三维非均匀问题尚未得到很好的解决,大多数情况下仍立足于一、二维正反演解释,因此消除地表非均匀性引起的曲线畸变,而后作常规的正反演解释,乃是当前最流行而又实际的研究途径。
补充资料：地电
地球内部不稳定的自然电流。其在地下空间中的分布和随时间变化的特征，可用于解决矿产、地质构造和地震研究问题。常通过视电阻率、自然电位和地电流的观测来研究。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条