通过对实验室岩心分析资料的研究，认为高电阻率水层的成因是岩性变化、残余油的存在及局部地区地层水矿化度的变化引起的。
Core analysis data from laboratory showed the origin of water layers with high resistivity is due to changes of lithology, residual oil and formation water salinity in local areas.
岩心面孔率参数的分析计算，弥补了实验室对火成岩、灰岩等特殊岩性非均质储层孔隙度参数计算的不足。
Analysis and calculation of parameters of core plane porosity make up the calculation inadequacy of porosity parameter in heterogeneous reservoirs.
岩心面孔率参数的分析计算，弥补了实验室对火成岩、灰岩等特殊岩性非均质储层孔隙度参数计算的不足。
Analysis and calculation of parameters of core plane porosity make up the calculation inadequacy of porosity parameter in hetero...
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