摘要
根据压实前后压实曲线的相似性及单调性，设定古孔隙度-深度、古密度-深度函数，结合压实前后地层骨架体积不变、骨架质量不变原理．建立回剥压实校正方程，从而恢复地层古厚度及地层古密度，并且保证压实前后地层骨架密度不变。
According to the similtrity and the montonic characteristics of the comaction curves between the compacted and the decompacted states, the paleo-porosity-depth function (Z) and the paleo-density-depth function (Z) was supnd. By using the principle which formation grain volume and mass have been keeping consant,the compaction corrction equations has been established. Further, the decomacted thickness S and the average paleo-density s can be calculated and the grain density of the compacted and decomacted states can be kept constant.
出处
《石油实验地质》
CAS
CSCD
北大核心
2000年第2期110-114,共5页
Petroleum Geology & Experiment
基金
国家自然科学基金!49732005
国土资源部定量预测及勘查评价开放实验室基金
关键词
压实校正
盆地
模拟
地层厚度
地层密度
compaction correction
grain volume
grain mass
similarity
monotonic increasing and decreasing
