岩性油气藏
巖性油氣藏
암성유기장
LITHOLOGIC RESERVOIRS
2011年
6期
13-17
,共5页
李文龙%牟中海%屈信忠%滕贤清%黄婧
李文龍%牟中海%屈信忠%滕賢清%黃婧
리문룡%모중해%굴신충%등현청%황청
成岩作用%成岩演化%储层物性%切6井区%昆北油田%柴达木盆地
成巖作用%成巖縯化%儲層物性%切6井區%昆北油田%柴達木盆地
성암작용%성암연화%저층물성%절6정구%곤북유전%시체목분지
diagenesis%diagenetic evolution%reservoir properties%Qie 6 well area%Kunbei Oilfield%Qaidam Basin
通过普通薄片、铸体薄片、扫描电镜、X-射线衍射分析,对昆北油田切6井区E1+2和E31砂岩储层成岩作用类型、演化阶段、演化序列及储层物性的影响因素进行了研究。结果表明:E1+2和E31砂岩处于中成岩阶段A亚期的末期,成岩作用类型主要有压实作用、胶结作用、溶蚀作用、交代作用、破裂作用;较强的压实作用、石英次生加大、方解石及硬石膏等矿物的胶结作用是使储层物性变差的重要因素;长石、岩屑和方解石胶结物的溶蚀作用以及砂岩破裂作用使储层物性得到改善。
通過普通薄片、鑄體薄片、掃描電鏡、X-射線衍射分析,對昆北油田切6井區E1+2和E31砂巖儲層成巖作用類型、縯化階段、縯化序列及儲層物性的影響因素進行瞭研究。結果錶明:E1+2和E31砂巖處于中成巖階段A亞期的末期,成巖作用類型主要有壓實作用、膠結作用、溶蝕作用、交代作用、破裂作用;較彊的壓實作用、石英次生加大、方解石及硬石膏等礦物的膠結作用是使儲層物性變差的重要因素;長石、巖屑和方解石膠結物的溶蝕作用以及砂巖破裂作用使儲層物性得到改善。
통과보통박편、주체박편、소묘전경、X-사선연사분석,대곤북유전절6정구E1+2화E31사암저층성암작용류형、연화계단、연화서렬급저층물성적영향인소진행료연구。결과표명:E1+2화E31사암처우중성암계단A아기적말기,성암작용류형주요유압실작용、효결작용、용식작용、교대작용、파렬작용;교강적압실작용、석영차생가대、방해석급경석고등광물적효결작용시사저층물성변차적중요인소;장석、암설화방해석효결물적용식작용이급사암파렬작용사저층물성득도개선。
Based on the analysis of ordinary thin sections, cast thin sections, scanning electron microscope and X-ray diffraction, this paper studied the diagenesis types, evolutionary phase, evolutionary series and influencing factors of reservoir properties of E1+2 and E31 in Qie 6 well area of Kunbei Oilfield. The result shows that the sandstone of E1+2 and E31 is in the late stage of middle diagenetic stage A, and the main diagenesis types are compaction, cementation, dissolution, metasomatism and cataclasis. The experienced compaction, quartz secondary enlargement and cementation of calcite and anhydrite are the main destructive factors of reservoir properties, while the dissolution of feldspar, detritus and calcite and cataclasis are the constructive factors of reservoir properties.