当代化工
噹代化工
당대화공
CONTEMPORARY CHEMICAL INDUSTRY
2014年
9期
1816-1819
,共4页
张庆国%富会%田得光%王宏旭%代春明
張慶國%富會%田得光%王宏旭%代春明
장경국%부회%전득광%왕굉욱%대춘명
长岭凹陷%葡萄花油层%低孔低渗储层%有效厚度
長嶺凹陷%葡萄花油層%低孔低滲儲層%有效厚度
장령요함%포도화유층%저공저삼저층%유효후도
Changling depression%Putaohua reservoir%Low porosity and low permeability reservoir%Effective thickness
以长岭凹陷葡萄花油层为例,以储层地质学理论为指导,利用岩心分析、测井、录井、分析化验、薄片、扫描电镜、X衍射分析等手段资料,建立姚家组一段基础资料库,确定储层的岩性特征、沉积特征、成岩作用、孔隙结构和物性特征。姚家组一段主要为三角洲前缘相的水下分支河道。岩石类型主要为岩屑质长石砂岩和长石质岩屑砂岩,岩石粒度相对较粗,主要以粉砂、细砂为主。储层孔隙主要以原生孔隙次生溶蚀扩边为主。储层孔隙度主要分布在10%~20%之间,渗透率主要分布在0.01×10-3~20×10-3μm2之间。通过测井与地质及试油资料综合对比研究,确定岩性、物性、含油性、电性下限标准。经过该区域储层68口井442个层测试验证,解释符合率提高10%,使得今后在该类油气层解释评价中具有一定的指导和借鉴意义。
以長嶺凹陷葡萄花油層為例,以儲層地質學理論為指導,利用巖心分析、測井、錄井、分析化驗、薄片、掃描電鏡、X衍射分析等手段資料,建立姚傢組一段基礎資料庫,確定儲層的巖性特徵、沉積特徵、成巖作用、孔隙結構和物性特徵。姚傢組一段主要為三角洲前緣相的水下分支河道。巖石類型主要為巖屑質長石砂巖和長石質巖屑砂巖,巖石粒度相對較粗,主要以粉砂、細砂為主。儲層孔隙主要以原生孔隙次生溶蝕擴邊為主。儲層孔隙度主要分佈在10%~20%之間,滲透率主要分佈在0.01×10-3~20×10-3μm2之間。通過測井與地質及試油資料綜閤對比研究,確定巖性、物性、含油性、電性下限標準。經過該區域儲層68口井442箇層測試驗證,解釋符閤率提高10%,使得今後在該類油氣層解釋評價中具有一定的指導和藉鑒意義。
이장령요함포도화유층위례,이저층지질학이론위지도,이용암심분석、측정、록정、분석화험、박편、소묘전경、X연사분석등수단자료,건립요가조일단기출자료고,학정저층적암성특정、침적특정、성암작용、공극결구화물성특정。요가조일단주요위삼각주전연상적수하분지하도。암석류형주요위암설질장석사암화장석질암설사암,암석립도상대교조,주요이분사、세사위주。저층공극주요이원생공극차생용식확변위주。저층공극도주요분포재10%~20%지간,삼투솔주요분포재0.01×10-3~20×10-3μm2지간。통과측정여지질급시유자료종합대비연구,학정암성、물성、함유성、전성하한표준。경과해구역저층68구정442개층측시험증,해석부합솔제고10%,사득금후재해류유기층해석평개중구유일정적지도화차감의의。
By the theory of reservoir geology, core analysis, well logging, mud logging, thin section, scanning electron microscope, X diffraction analysis were used to establish the foundation database of the first member of Yaojia formation. Then the lithologic characteristics, reservoir sedimentary characteristics, reservoir diagenesis, pore structure and physical characteristics were determined. The results show that the first member of Yaojia formation is mainly subaqueous distributary channel of delta front facies;the rock types are mainly lithic feldspar sandstone and feldspathic lithic sandstone, rock grain size are relatively coarse, mainly composed of silt and fine sand; reservoir porosity is mainly primary pores and secondary dissolution extension;reservoir porosity is mainly distributed between 10%and 20%, permeability is mainly distributed between 0.01×10-3 and 20×10-3μm2. The limit of the lithology, physical property, oiliness, and electrical standards were determined by logging and geological comprehensive comparative study and test data. Interpretation coincidence rate was increased by 10%by 442 layer test validation of 68 Wells in the regional reservoir.