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通过碳酸盐岩压溶作用基本特征的分析,笔者提出了压溶的碳酸盐岩地层厚度恢复的原理和公式,同时还探讨了缝合线有机质丰度的校正方法与公式。实际计算结果表明了碳酸盐岩地层的压溶作用是很强的,压溶的碳酸盐岩地层厚度在相应的碳酸盐岩岩心长度中所占的百分比最低为2.10％,最高可达58％,主要集中于31％以下,平均为11.60％。
Based on the analysis of the basic characteristics of carbonatite pressure dissolving, the author put forward the principles and formulas for the thickness recovery of the dissolved carbonate rock stratum, and also discussed the correction methods and formulas for organic matter abundance of suture. The actual calculation shows that the pressure-dissolving effect of carbonate stratum is very strong. The thickness of compressive carbonate stratum accounts for 2.10% of the minimum length of corresponding carbonate core, up to 58%, mainly below 31%, with an average of 11.60%.