石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2014年
6期
684-691
,共8页
郭智%贾爱林%薄亚杰%唐海发%郭本晓
郭智%賈愛林%薄亞傑%唐海髮%郭本曉
곽지%가애림%박아걸%당해발%곽본효
有效砂体%沉积%砂体分布%成岩作用%主控因素%苏里格气田
有效砂體%沉積%砂體分佈%成巖作用%主控因素%囌裏格氣田
유효사체%침적%사체분포%성암작용%주공인소%소리격기전
effective sand body%sedimentation%sand body distribution%diagenesis%mainly controlling factors%Sulige Gas Field
苏里格气田南区是苏里格气田主体向南的延伸,距离物源区远,储层埋深大,成岩作用强。落实有效砂体分布及主控因素,是苏南等气田边部地区高效开发的基础。以苏南盒8、山1段储层为目标,结合构造、沉积、储层、成岩分析,研究了有效砂体的空间展布特征,总结了有效砂体的主控因素。苏南有效砂体多分布在心滩和分流河道底部等粗砂岩相,垂向上发育孤立型、垂向叠置型、侧向搭接型3种模式,平面上分布在中、东部2条主砂带内。在有效储层形成过程中,宽缓的构造坡降是沉积、成藏的背景,强水动力条件下的浅水辫状河三角洲平原沉积控制了储层的分布格局,而成藏前的压实、胶结、溶蚀等成岩作用深刻改造了储层,塑造了有效砂体的形态。
囌裏格氣田南區是囌裏格氣田主體嚮南的延伸,距離物源區遠,儲層埋深大,成巖作用彊。落實有效砂體分佈及主控因素,是囌南等氣田邊部地區高效開髮的基礎。以囌南盒8、山1段儲層為目標,結閤構造、沉積、儲層、成巖分析,研究瞭有效砂體的空間展佈特徵,總結瞭有效砂體的主控因素。囌南有效砂體多分佈在心灘和分流河道底部等粗砂巖相,垂嚮上髮育孤立型、垂嚮疊置型、側嚮搭接型3種模式,平麵上分佈在中、東部2條主砂帶內。在有效儲層形成過程中,寬緩的構造坡降是沉積、成藏的揹景,彊水動力條件下的淺水辮狀河三角洲平原沉積控製瞭儲層的分佈格跼,而成藏前的壓實、膠結、溶蝕等成巖作用深刻改造瞭儲層,塑造瞭有效砂體的形態。
소리격기전남구시소리격기전주체향남적연신,거리물원구원,저층매심대,성암작용강。락실유효사체분포급주공인소,시소남등기전변부지구고효개발적기출。이소남합8、산1단저층위목표,결합구조、침적、저층、성암분석,연구료유효사체적공간전포특정,총결료유효사체적주공인소。소남유효사체다분포재심탄화분류하도저부등조사암상,수향상발육고립형、수향첩치형、측향탑접형3충모식,평면상분포재중、동부2조주사대내。재유효저층형성과정중,관완적구조파강시침적、성장적배경,강수동력조건하적천수변상하삼각주평원침적공제료저층적분포격국,이성장전적압실、효결、용식등성암작용심각개조료저층,소조료유효사체적형태。
The southern Sulige area is the southward extension of the main part of the Sulige Gas Field, where is far from sediment provenance, buried deep and has a strong diagenesis. Understanding the distribution character?istics and main controlling factors of effective sand body is the basis of the efficient development of the edge re?gions of the Sulige Gas Field, such as the southern Sulige area. Focusing on the reservoirs of He8 member and Shan1 member, the areas of tectonic, sedimentation, reservoir and diagenesis were studied, and the distribution characteristics and main controlling factors of effective sand body were concluded. The effective sand bodies in the southern Sulige area mainly distribute in point bars and the bottom of distributary channels, and can be verti?cally classified into three types:isolated, vertically stacking, and laterally shiplap ones. Horizontally, they locate in the central and eastern sand belts of the study area. During the formation of effective reservoirs, a gentle struc?ture background is necessary for the sedimentation and formation of gas reservoirs. The shallow braided?river delta plain deposits in the strong hydrodynamic environment determined the distribution pattern of reservoir, whereas the compaction, cementation and dissolution diagenesis before the formation progress of gas reservoirs greatly re?formed the reservoirs and controlled the distribution of effective sand body.