摘要
选取黄骅坳陷乌深1井的富含烃源岩的山西组地层为研究对象,并结合相关研究资料,在揭示其埋藏史与受热史的基础上,应用EASY%R0与TTI数值模拟方法对有机质成熟度进行了反演、对比分析。研究结果表明,EASY%R0反演的成熟度较合理与准确,在实际应用中的价值更大。
Because of its being full of hydrocarbon source rock, the Shanxi Formation of well Wushen 1 in Huanghua depression is selected for investigation in this paper. Based on abundant correlated research data in this area, we have disclosed the burial history and thermal history of that formation.Then we applied both EASY%R0 and TTI-R0 numerical simulation model to evaluate the source rock's organic maturation history,and compared EASY%R0 with TTI-R0.The result suggested that the EASY%R0 model is more reasonable, more accurate and more useful than the TTI-R0 model.
出处
《中国煤田地质》
2005年第2期4-7,共4页
Coal Geology of China
