石油与天然气地质
石油與天然氣地質
석유여천연기지질
OIL & GAS GEOLOGY
2013年
5期
708-716
,共9页
耳闯%赵靖舟%白玉彬%樊豪%沈武显
耳闖%趙靖舟%白玉彬%樊豪%瀋武顯
이틈%조정주%백옥빈%번호%침무현
岩相%孔隙类型%孔隙结构%储层特征%富有机质泥页岩%延长组%鄂尔多斯盆地
巖相%孔隙類型%孔隙結構%儲層特徵%富有機質泥頁巖%延長組%鄂爾多斯盆地
암상%공극류형%공극결구%저층특정%부유궤질니혈암%연장조%악이다사분지
lithofacies%pore type%pore structure%reservoir characteristics%organic-rich shale%Yanchang Formation%Ordos Basin
富有机质泥页岩储层特征研究对认识页岩油气勘探潜力具有重要意义。为确定延长组富有机质泥页岩储层特征,开展了岩石薄片、扫描电镜、X-射线衍射、物性、比表面积孔径分析和有机碳含量等分析测试工作,揭示了泥页岩岩相、矿物含量、成岩作用、孔隙类型、物性和孔隙结构等特征。延长组泥页岩可划分为泥岩岩相、含粉砂泥岩岩相和粉砂质泥岩岩相3种岩相类型。泥岩岩相的有机碳含量最高,粘土矿物含量高(>50%),成岩作用较弱;粒间孔和粒内孔是中生界泥页岩储层主要的孔隙类型;微孔主要集中在0.4~1 nm,中孔主要集中在3~5 nm,中孔对孔隙体积和比表面积的贡献好于微孔。根据现有资料认为,延长组富有机质泥页岩塑性矿物含量高,成岩作用弱,对储层后期改造提出了严峻挑战。
富有機質泥頁巖儲層特徵研究對認識頁巖油氣勘探潛力具有重要意義。為確定延長組富有機質泥頁巖儲層特徵,開展瞭巖石薄片、掃描電鏡、X-射線衍射、物性、比錶麵積孔徑分析和有機碳含量等分析測試工作,揭示瞭泥頁巖巖相、礦物含量、成巖作用、孔隙類型、物性和孔隙結構等特徵。延長組泥頁巖可劃分為泥巖巖相、含粉砂泥巖巖相和粉砂質泥巖巖相3種巖相類型。泥巖巖相的有機碳含量最高,粘土礦物含量高(>50%),成巖作用較弱;粒間孔和粒內孔是中生界泥頁巖儲層主要的孔隙類型;微孔主要集中在0.4~1 nm,中孔主要集中在3~5 nm,中孔對孔隙體積和比錶麵積的貢獻好于微孔。根據現有資料認為,延長組富有機質泥頁巖塑性礦物含量高,成巖作用弱,對儲層後期改造提齣瞭嚴峻挑戰。
부유궤질니혈암저층특정연구대인식혈암유기감탐잠력구유중요의의。위학정연장조부유궤질니혈암저층특정,개전료암석박편、소묘전경、X-사선연사、물성、비표면적공경분석화유궤탄함량등분석측시공작,게시료니혈암암상、광물함량、성암작용、공극류형、물성화공극결구등특정。연장조니혈암가화분위니암암상、함분사니암암상화분사질니암암상3충암상류형。니암암상적유궤탄함량최고,점토광물함량고(>50%),성암작용교약;립간공화립내공시중생계니혈암저층주요적공극류형;미공주요집중재0.4~1 nm,중공주요집중재3~5 nm,중공대공극체적화비표면적적공헌호우미공。근거현유자료인위,연장조부유궤질니혈암소성광물함량고,성암작용약,대저층후기개조제출료엄준도전。
Reservoir characteristics study is very important to understand the hydrocarbon potential of organic -rich shales . A series of analyses and tests,including thin sections,SEM,XRD,physical property,total organic carbon(TOC),specific surface area and pore size distribution ,were made to reveal the reservoir characteristics of the organic-rich shales of the Triassic Yanchang Formation(Fm)in Ordos Basin.This paper also defined the lithofacies,mineral types,diagenesis,pore types and physical properties .Three types of lithofacies are identified in the organic-rich shales ,including muddy shale , silt-bearing shale and silty shale .The muddy shale has the highest TOC content,clay content of more than 50%and rela-tively weak diagenesis .The dominant pore types of the organinc-rich shales in the Yanchang Fm are intragranular and intergranular pores.The pore sizes of micropores are mainly within 0.4 to 1 nm and those of mesopores are mainly within 3 to 5 nm.The contribution of the mesopores to pore volume and specific surface area is larger than that of the micro -pores.The high content of ductile minerals and weak diagenesis of the organic shales in the the Yanchang Fm make the reservoir stimulation more challenging .