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沉积和成岩作用交互约束页岩油生储品质机理分析

滕建彬

油气地质与采收率2024,Vol.31Issue(6):18-32,15.
油气地质与采收率2024,Vol.31Issue(6):18-32,15.DOI:10.13673/j.pgre.202312018

沉积和成岩作用交互约束页岩油生储品质机理分析

Mechanism of interaction influence between sedimentation and diagenesis on quality of shale oil generation and storage:A case study of Paleogene shale of Shahejie Formation in Niuzhuang Subsag of Dongying Sag

滕建彬1

作者信息

  • 1. 中国石化胜利油田分公司 勘探开发研究院,山东 东营 257015||页岩油气富集机理与高效开发全国重点实验室,北京 102206||中国石油大学(华东)地球科学与技术学院,山东 青岛 266580||中国石化页岩油气勘探开发重点实验室,山东 东营 257015||中国石化胜利油田分公司 沉积模拟与储层评价实验室,山东 东营 257015||东营市低渗透油层产能评价与增产改造重点实验室,山东 东营 257015
  • 折叠

摘要

Abstract

The shale oil in the Lower Es3 and Upper Es4 Submembers of Niuzhuang Subsag of Dongying Sag is rich,with high yield,belonging to the typical terrestrial shale oil.Currently,the understanding of material exchanges and reservoir characteristics driven by diagenesis between shale laminae is not clear.The mechanism of the interaction influence of sedimentation and diagenesis on the quality of shale oil generation and storage was analyzed by the petrology,geochemical analysis of trace elements and rare earth elements,and other methods based on the sparry calcite veins and material transfer phenomena,as well as shale hydrocarbon generation and oil-bearing parameters.In addition,material transfer between shale laminae,generation of sparry calcite veins,and shale oil migration were scientifically explained.The geochemical microanalysis of rare earth elements reveals that the Th and U ele-ment contents within different material laminae in descending order are as follows:argillaceous layer,sparry calcite vein,recrystal-lized calcite layer,and contact surface between argillaceous layer and sparry calcite vein.The differentiation of light and heavy rare earth elements in the argillaceous layer and sparry calcite vein is obvious,showing significant enrichment of light rare earth ele-ments and loss of heavy rare earth elements,exhibiting obvious negative anomalies of Dy.The differentiation of light and heavy rare earth elements in the recrystallized calcite layer is not obvious,showing a negative anomaly of Dy.The contents of Th,U,and rare earth elements in the sparry calcite veins are lower than those in the argillaceous layer and higher than those in the recrystallized calcite layer,and it is an essential geochemical indicator to distinguish between the sparry calcite veins and the recrystallized calcite layer.The compaction effect and material component content are the main factors affecting shale porosity.According to the nuclear magnetic resonance experiment,the reduction in pore size greater than 30 nm is the most significant in shale with a burial depth of 3 300-3 600 m,and the reduction amplitude is about 1%/hm.The total content of terrestrial minerals is positively correlated with po-rosity due to the effect of overpressure fluid pore retention caused by hydrocarbon pressurization.Hydrogenated carbonate minerals have strong resistance to overlying rock pressure,which is beneficial for artificial fracturing.Their intergranular and dissolution pores have large sizes with superior oil storage capacity.

关键词

亮晶方解石脉/微量元素/稀土元素/成岩作用/页岩油/牛庄洼陷

Key words

sparry calcite vein/trace elements/rare earth elements/diagenesis/shale oil/Niuzhuang Subsag

分类

能源科技

引用本文复制引用

滕建彬..沉积和成岩作用交互约束页岩油生储品质机理分析[J].油气地质与采收率,2024,31(6):18-32,15.

基金项目

中国石化科技攻关项目"牛庄洼陷沙四上泥页岩流体-岩石作用机理研究"(KP23003)和"济阳坳陷古近系细粒沉积特征与古湖泊演化"(KL21042). (KP23003)

油气地质与采收率

OA北大核心CSTPCD

1009-9603

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