新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2014年
4期
509-513
,共5页
邢蓝田%徐丽%段毅%刘晔
邢藍田%徐麗%段毅%劉曄
형람전%서려%단의%류엽
鄂尔多斯盆地%林镇%延8油层组%孔隙演化%成岩作用
鄂爾多斯盆地%林鎮%延8油層組%孔隙縯化%成巖作用
악이다사분지%림진%연8유층조%공극연화%성암작용
Ordos Basin%Linzhen area%Yan8 reservoir%Porosity Evolution%Diagenesis
近年来林镇地区延安组延8油层组中不断发现新油气。利用岩心观察、薄片鉴定等分析手段,对储层特征及成岩作用进行研究,定量分析成岩过程中储层孔隙演化特征。结果表明:研究区东北部一带砂体连续,厚度普遍在14 m以上,为该区优势储集体;储层砂岩矿物成熟度较低,结构成熟度中等,沉积时环境相对稳定;孔隙类型以溶蚀孔为主,残余粒间孔次之;该储层目前达晚成岩阶段A期。储层原始孔隙度为33.6%,其演化过程主要受压实作用、胶结作用和溶蚀作用控制,压实及胶结作用导致原始孔隙度丧失16.7%与10.7%,后期溶蚀作用形成6.8%次生孔隙,有效地提升了延8油层组储层的孔隙度。
近年來林鎮地區延安組延8油層組中不斷髮現新油氣。利用巖心觀察、薄片鑒定等分析手段,對儲層特徵及成巖作用進行研究,定量分析成巖過程中儲層孔隙縯化特徵。結果錶明:研究區東北部一帶砂體連續,厚度普遍在14 m以上,為該區優勢儲集體;儲層砂巖礦物成熟度較低,結構成熟度中等,沉積時環境相對穩定;孔隙類型以溶蝕孔為主,殘餘粒間孔次之;該儲層目前達晚成巖階段A期。儲層原始孔隙度為33.6%,其縯化過程主要受壓實作用、膠結作用和溶蝕作用控製,壓實及膠結作用導緻原始孔隙度喪失16.7%與10.7%,後期溶蝕作用形成6.8%次生孔隙,有效地提升瞭延8油層組儲層的孔隙度。
근년래림진지구연안조연8유층조중불단발현신유기。이용암심관찰、박편감정등분석수단,대저층특정급성암작용진행연구,정량분석성암과정중저층공극연화특정。결과표명:연구구동북부일대사체련속,후도보편재14 m이상,위해구우세저집체;저층사암광물성숙도교저,결구성숙도중등,침적시배경상대은정;공극류형이용식공위주,잔여립간공차지;해저층목전체만성암계단A기。저층원시공극도위33.6%,기연화과정주요수압실작용、효결작용화용식작용공제,압실급효결작용도치원시공극도상실16.7%여10.7%,후기용식작용형성6.8%차생공극,유효지제승료연8유층조저층적공극도。
In recent years, new oil reservoirs have been discovered gradually in yan8 subsection of Yanan Formation in Linzhen area, Ordos basin. It is important to understand the reservoir characteristics of yan8 subsection for further explo-ration and exploitation. On the basis of drill-core samples observation and study on rock thin section, the reservoir charac-teristics and Porosity evolution of Yan8 subsection of Yanan formation were analyzed. The results showed that:The sand body in the northeast side of the study area is rather thick, which is high-quality reservoir in the study area. The maturity of composition is on low side and structural maturity is middling;The main type of pore is residual intergranular porosi-ty,dissolved pores between grains and dissolved pores in grains;The author holds that the diagenesis is in the A substage of late diagenesis period;Original porosity of reservior is 33.6%in the stage of sedimentation, and the lithogenesis of compaction, cementation and dissolution are main factors affecting reservoir properties in this area;The compaction and carbonate-cementation destroy the primary-texture of pore intensively, which contribute 16.7%and 10.7%to the loss of original pores, respectively. The dissolution plays an important role in improving the properties by producing secondary porosity and has increased the 6.8%secondary pores.