1. China University of Geosciences, Beijing 100083; 2. Scientific Research Institute of Exploration and Development, Zhongyuan O ilf ie ld Company, SINOPEC, Puyang 457001, China
摘要
在阐述M agra提出的泥岩压实曲线法恢复地层剥蚀厚度方法原理的基础上, 通
过对泥岩压实曲线反映地层间断的6种形态模式和东濮凹陷泥岩压实曲线的形态特征的分
析, 论述了该方法在东濮凹陷的适用性。选择东濮凹陷100余口井的泥岩压实曲线应用该方
法计算了东营组地层剥蚀厚度, 结果与盆地模拟拟合的结果相近, 证明了该方法的可行性。
Abstract
Based on the desc ription of the estim ation m ethod of erosion sedim ent th ickness by the sha le com paction curv e m entioned or ig ina lly by M ag ra, th is paper d iscussed six m ode ls of the form ation discontinuance demonstrated by the sha le com paction curve. The app licab ility of this m ethod in Dongpu depression is expounded through the charac teristics analysis o f the sha le com paction curve. The erosion sed im ent thickness o f Dongy ing fo rm ation is estim ated in te rm s of this m ethod by e lecting shale compaction curve over 100 w e lls in Dongpu Depression. The results from this m ethod and from the basin m ode lling are qu ite sim ilar, wh ich proves tha t this m ethod is re liab le.
关键词:
东濮凹陷;东营组;剥蚀厚度;压实曲线;
Keywords:
Dongpu depression, Dongy ing form ation, Erosion sedim ent th ickness, C om paction curve;