东营凹陷胜坨地区沙四上亚段浊积扇致密砂砾岩储层孔隙演化
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摘要
利用钻井岩心、铸体薄片、扫描电镜、物性分析、包裹体测温等资料,结合盆地埋藏演化史,研究东营凹陷胜坨地区沙四上亚段浊积扇致密砂砾岩储层成岩作用及孔隙度演化过程。结果表明:研究区沙四上亚段浊积扇致密砂砾岩储层现今孔隙度为8.75%,发育压实作用、胶结作用、溶蚀作用及两期油气充注;典型成岩—油气充注序列表现为早期绿泥石胶结—早期油气充注—早期溶蚀作用—石英次生加大/自生石英—压实作用—黏土胶结—方解石胶结—白云石胶结—晚期油气充注—石英溶蚀—晚期溶蚀作用—晚期黄铁矿胶结,储层成岩阶段达到中成岩B期;恢复储层原始孔隙度为34.53%,压实作用减孔率达到72%,各期胶结作用持续降低孔隙度,溶蚀作用调整和保存孔隙,浊积扇砂砾岩储层经历早期成藏—致密—边成藏边致密的过程。该研究结果可为东营凹陷致密储层的研究提供参考。
The diagenesis and porosity evolution of turbidite fan tight glutenite reservoir in Shengtuo Area of Dongying Depression were studied by drilling core,casting thin section,scanning electron microscope,physical property analysis,inclusion temperature measurement and other test data,combined with burial evolution history of the basin.The results show that the porosity of the turbidite fan tight glutenite reservoir in the Es4s of the study area is 8.75%,and there are compaction,cementation,dissolution and two stages of oil and gas filling.Typical diagenesis-hydrocarbon charging sequence is shown as early-stage chlorite cementation,hydrocarbon charging stage early phase,early-stage dissolution,quartz overgrowths/authigenic quartz,compaction,clay cementation,calcite cementation,dolomite cementation,hydrocarbon charging stage later period,quartz dissolution,late dissolution,late pyrite cementation.And the reservoir diagenesis stage has reached middle diagenesis stage B.The primary porosity of the reservoir is 34.53%,the porosity reduced rate is 72%,and the degree of development is gradually decreased,the porosity is continuously reduced by cementation at each stages,the porosity is adjusted and preserved by dissolution.The turbidite fan glutenite reservoir undergoes the process of early-stage accumulation,compaction-accumulation while compaction.The research results can provide reference for the study of tight reservoirs in Dongying Depression.
The diagenesis and porosity evolution of turbidite fan tight glutenite reservoir in Shengtuo Area of Dongying Depression were studied by drilling core,casting thin section,scanning electron microscope,physical property analysis,inclusion temperature measurement and other test data,combined with burial evolution history of the basin.The results show that the porosity of the turbidite fan tight glutenite reservoir in the Es4s of the study area is 8.75%,and there are compaction,cementation,dissolution and two stages of oil and gas filling.Typical diagenesis-hydrocarbon charging sequence is shown as early-stage chlorite cementation,hydrocarbon charging stage early phase,early-stage dissolution,quartz overgrowths/authigenic quartz,compaction,clay cementation,calcite cementation,dolomite cementation,hydrocarbon charging stage later period,quartz dissolution,late dissolution,late pyrite cementation.And the reservoir diagenesis stage has reached middle diagenesis stage B.The primary porosity of the reservoir is 34.53%,the porosity reduced rate is 72%,and the degree of development is gradually decreased,the porosity is continuously reduced by cementation at each stages,the porosity is adjusted and preserved by dissolution.The turbidite fan glutenite reservoir undergoes the process of early-stage accumulation,compaction-accumulation while compaction.The research results can provide reference for the study of tight reservoirs in Dongying Depression.
引文
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[11]汪洋,刘洛夫,李树同,等.鄂尔多斯盆地姬塬西部三叠系延长组长8油层组成岩作用与致密化过程[J].古地理学报,2017,19(5):892-906.WANG Yang,LIU Luofu,LI Shutong,et al.Diagenesis and densification process of the Chang8interval of Triassic Yanchang Formation,Western Jiyuan Area,Ordos Basin[J].Journal of Palaeogeography,2017,19(5):892-906.
[12]卢杰河,王香增,贺永红,等.鄂尔多斯盆地富县地区长7油层组致密砂岩成岩作用及孔隙演化[J].东北石油大学学报,2017,41(3):9-20.LU Jiehe,WANG Xiangzeng,HE Yonghong,et al.Diagenesis and porosity evolution of Chang7tight sandstone in Fuxian Area,Ordos Basin[J].Journal of Northeast Petroleum University,2017,41(3):9-20.
[13]MAKOWITZ A,LANDER R H,MILLIKEN K L.Diagenetic modeling to assess the relative timing of quartz cementation and brittle grain processes during compaction[J].AAPG Bulletin,2006,90(6):873-885.
[14]操应长,杨田,宋明水,等.陆相断陷湖盆低渗透碎屑岩储层特征及相对优质储层成因:以济阳坳陷东营凹陷古近系为例[J].石油学报,2018,39(7):727-743.CAO Yingchang,YANG Tian,SONG Mingshui,et al.Characteristics of low-permeability clastic reservoirs and genesis of relatively high-quality reservoirs in the continental rift lake basin:a case study of Paleogene in the Dongying Sag,Jiyang Depression[J].Acta Petrolei Sinica,2018,39(7):727-743.
[15]许同,刘洛夫,汪洋,等.乌尔禾-风南地区百口泉组碎屑岩储层成岩作用及孔隙演化[J].东北石油大学学报,2018,42(4):27-39.XU Tong,LIU Luofu,WANG Yang,et al.Diagenesis and porosity evolution of clastic reservoir of Baikouquan Formation in Wuerhr-Fengnan Area[J].Journal of Northeast Petroleum University,2018,42(4):27-39.
[16]万青青,刘洛夫,肖飞,等.准噶尔盆地车排子地区下侏罗统八道湾组砂岩储层成岩作用与孔隙演化[J].东北石油大学学报,2017,41(1):21-32.WAN Qiangqing,LIU Luofu,XIAO Fei,et al.Diagenesis and porosity evolution of sandstone reservoir in the Lower Jurassic Badaowan Formation in Chepaizi Area,Junggar Basin[J].Journal of Northeast Petroleum University,2017,41(1):21-32.
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