Approximate Interpretation of 3-D Data Using 2-D Inversion Program in the DC Resistivity Sounding
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摘要: 直流电阻率测深剖面数据解释最好的方法是二维反演, 这是由于它反演速度快, 而三维反演则需要很多的实测数据、很长的计算时间.而且通过对几种三维模型测深数据的二维反演结果的研究, 发现尽管对无走向的良导矿体, 二维反演方法所圈定的异常中心与真实矿体中心有一定的误差, 但基本上还是能反映矿体的真实形态和中心位置.当矿体具有一定的走向长度时, 则无论对高阻矿体还是良导矿体二维反演的效果都很好.Abstract: The 2-D inversion is the best method in the interpretation of DC resistivity sounding profiles data owing to its high speed, but the 3-D inversion, by contrast, needs more measured data and more computer time. Through the 2-D inversional study of several 3-D models, we know that for the good conductor ore-body without strike, there is some deflection between the center of real ore-body and the center of anomaly enclosed by the 2-D inversion, however, the anomaly can still reflect the true shape and the center position of the ore-body in the main. When the ore-body has certain lengths in strike, the effect of 2-D inversion is good to it, no matter its resistivity is high or low.
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Key words:
- DC resistivity sounding /
- 2-D inversion /
- 3-D model /
- approximate interpretation
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表 1 有限单元网格间距
Table 1. Mesh intervals of finite element
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