油气藏评价与开发
油氣藏評價與開髮
유기장평개여개발
2013年
1期
15-18
,共4页
程秀梅%章雄冬%王平%刘莉
程秀梅%章雄鼕%王平%劉莉
정수매%장웅동%왕평%류리
储层物性%孔隙结构%阜三段储层%苏北盆地
儲層物性%孔隙結構%阜三段儲層%囌北盆地
저층물성%공극결구%부삼단저층%소북분지
reservoir physical properties%pore structure%Fu-3 reservoir%North Jiangsu basin
对苏北盆地A区块阜三段储层物性及孔隙结构特征进行了分析研究,结果表明,孔隙度与渗透率、岩石密度间具有较好的相关性,纵向上出现三个孔隙发育带,分别为<2100 m,孔隙度主要为35%左右;2100~2600 m,孔隙度主要为25%左右;2600~3100 m,孔隙度主要为20%左右。储层以中小孔微细喉为主,具单孔隙结构,且孔隙结构与物性间具有一定的对应关系,Ⅰ类优质储层主要位于第Ⅰ孔隙发育带和第Ⅱ孔隙发育带上部,约占15%;Ⅱ类主力储层主要位于第Ⅱ孔隙发育带和第Ⅲ孔隙发育带,约占55%;Ⅲ类较差储层主要位于第Ⅲ孔隙发育带,约占30%。
對囌北盆地A區塊阜三段儲層物性及孔隙結構特徵進行瞭分析研究,結果錶明,孔隙度與滲透率、巖石密度間具有較好的相關性,縱嚮上齣現三箇孔隙髮育帶,分彆為<2100 m,孔隙度主要為35%左右;2100~2600 m,孔隙度主要為25%左右;2600~3100 m,孔隙度主要為20%左右。儲層以中小孔微細喉為主,具單孔隙結構,且孔隙結構與物性間具有一定的對應關繫,Ⅰ類優質儲層主要位于第Ⅰ孔隙髮育帶和第Ⅱ孔隙髮育帶上部,約佔15%;Ⅱ類主力儲層主要位于第Ⅱ孔隙髮育帶和第Ⅲ孔隙髮育帶,約佔55%;Ⅲ類較差儲層主要位于第Ⅲ孔隙髮育帶,約佔30%。
대소북분지A구괴부삼단저층물성급공극결구특정진행료분석연구,결과표명,공극도여삼투솔、암석밀도간구유교호적상관성,종향상출현삼개공극발육대,분별위<2100 m,공극도주요위35%좌우;2100~2600 m,공극도주요위25%좌우;2600~3100 m,공극도주요위20%좌우。저층이중소공미세후위주,구단공극결구,차공극결구여물성간구유일정적대응관계,Ⅰ류우질저층주요위우제Ⅰ공극발육대화제Ⅱ공극발육대상부,약점15%;Ⅱ류주력저층주요위우제Ⅱ공극발육대화제Ⅲ공극발육대,약점55%;Ⅲ류교차저층주요위우제Ⅲ공극발육대,약점30%。
This paper analyzed on physical properties and pore structure characteristics of Fu-3 reservoir in block-A of North Ji-angsu basin. The results showed that the porosity is closely related to permeability and rock density. There are three pore develop-ment areas in longitudinal zones. The porosity is about 35%while blow 2 100 meters. The porosity is about 25%while between 2 100 and 2 600 meters. The porosity is about 20%while between 2 600 and 3 100 meters. Reservoirs based on mid-small pores minute throat have single pore structure. The pore structures are related to the physical properties. Quality reservoir I is mainly lo-cated in the first area and the top of the second area, about 15%. Main reservoir II is mainly located in the second area and the third area, about 55%. Poor reservoir III is mainly located in the third area, about 30%.