石油与天然气地质
石油與天然氣地質
석유여천연기지질
OIL & GAS GEOLOGY
2014年
5期
712-719
,共8页
卢炳雄%郑荣才%华国%徐文礼
盧炳雄%鄭榮纔%華國%徐文禮
로병웅%정영재%화국%서문례
沉积相%热演化%构造运动%页岩气%皖南地区
沉積相%熱縯化%構造運動%頁巖氣%皖南地區
침적상%열연화%구조운동%혈암기%환남지구
sedimentary facies%thermal evolution%tectonic movement%shale gas%southern Anhui%province
以野外剖面观测和室内薄片及扫描电镜分析为基础,结合地质与钻井等资料,提出皖南地区下寒武统沉积相的具体划分方案。认为盆地相的深水还原环境是形成页岩气藏的最佳相带,而碳酸盐缓坡不利于页岩气勘探;对储层贡献最大的储集空间类型为裂缝,其次为次生溶蚀微孔,而晶间孔相对不发育,对储层的贡献则十分有限。从富含有机质页岩的空间展布、地化特征、保存条件等方面出发,采用页岩气目标优选评价综合分析方法,对皖南地区下寒武统页岩气成藏条件进行了研究,着重定量评价了页岩厚度、有机碳含量、镜质体反射率、脆性矿物含量等指标。皖南地区下寒武统页岩平均厚度大于50 m,石台县-南陵县一带达页岩厚度最大值为200~600 m;有机碳含量较高,平均值达2.37%;镜质体反射率平均值大于2%,页岩气藏处于干酪根裂解气的成熟-高熟阶段;脆性矿物含量较高,平均值为46.89%,有利于压裂形成网络裂缝。通过与美国主要页岩气藏的地化参数进行对比分析,认为皖南地区下寒武统页岩具备非常优越的页岩气成藏条件,可选为我国非常规能源首选的有利区之一。
以野外剖麵觀測和室內薄片及掃描電鏡分析為基礎,結閤地質與鑽井等資料,提齣皖南地區下寒武統沉積相的具體劃分方案。認為盆地相的深水還原環境是形成頁巖氣藏的最佳相帶,而碳痠鹽緩坡不利于頁巖氣勘探;對儲層貢獻最大的儲集空間類型為裂縫,其次為次生溶蝕微孔,而晶間孔相對不髮育,對儲層的貢獻則十分有限。從富含有機質頁巖的空間展佈、地化特徵、保存條件等方麵齣髮,採用頁巖氣目標優選評價綜閤分析方法,對皖南地區下寒武統頁巖氣成藏條件進行瞭研究,著重定量評價瞭頁巖厚度、有機碳含量、鏡質體反射率、脆性礦物含量等指標。皖南地區下寒武統頁巖平均厚度大于50 m,石檯縣-南陵縣一帶達頁巖厚度最大值為200~600 m;有機碳含量較高,平均值達2.37%;鏡質體反射率平均值大于2%,頁巖氣藏處于榦酪根裂解氣的成熟-高熟階段;脆性礦物含量較高,平均值為46.89%,有利于壓裂形成網絡裂縫。通過與美國主要頁巖氣藏的地化參數進行對比分析,認為皖南地區下寒武統頁巖具備非常優越的頁巖氣成藏條件,可選為我國非常規能源首選的有利區之一。
이야외부면관측화실내박편급소묘전경분석위기출,결합지질여찬정등자료,제출환남지구하한무통침적상적구체화분방안。인위분지상적심수환원배경시형성혈암기장적최가상대,이탄산염완파불리우혈암기감탐;대저층공헌최대적저집공간류형위렬봉,기차위차생용식미공,이정간공상대불발육,대저층적공헌칙십분유한。종부함유궤질혈암적공간전포、지화특정、보존조건등방면출발,채용혈암기목표우선평개종합분석방법,대환남지구하한무통혈암기성장조건진행료연구,착중정량평개료혈암후도、유궤탄함량、경질체반사솔、취성광물함량등지표。환남지구하한무통혈암평균후도대우50 m,석태현-남릉현일대체혈암후도최대치위200~600 m;유궤탄함량교고,평균치체2.37%;경질체반사솔평균치대우2%,혈암기장처우간락근렬해기적성숙-고숙계단;취성광물함량교고,평균치위46.89%,유리우압렬형성망락렬봉。통과여미국주요혈암기장적지화삼수진행대비분석,인위환남지구하한무통혈암구비비상우월적혈암기성장조건,가선위아국비상규능원수선적유리구지일。
Based on outcrop investigation ,thin-section observation and SEM analysis ,a detail division scheme of sedimen-tary facies was proposed for the Lower Cambrian in southern Anhui combining with geology and wellbore data .The most fa-vorable facie belt for shale gas accumulation is deep-water deduction environment in the basin ,while the carbonate ramp is unfavorable for shale gas exploration .Fractures make the greatest contribution to the storage of shale gas reservoir ,followed by the secondary dissolution micro-pores.In contrast ,intercrystalline pores contribute the least due to their relatively poor development .This paper comprehensively studied the geological characteristics of the Lower Cambrian shale gas play in southern Anhui in such aspects as spatial distribution of organic -rich shale ,geochemical behaviors and preservation condi-tions.The study was focused on quantitative evaluation of shale thickness ,TOC content,Ro and brittleness.The Lower Cam-brian shale in southern Anhui is more than 50 meters on average ,with the maximum thickness in the range from 200 to 600 meters occurring in Shitai and Nanling counties .The shale gas play has an average TOC content of 2.37%.The average Ro is more than 2%,indicating that the shale is at mature-high mature stage .The average brittle mineral content is 46.89%, being favorable for the creation of fracture networks through hydraulic fracturing .Based on comparison with the geochemical parameters of the main large shale gas plays in America ,it is indicated that the Lower Cambrian shale in southern Anhui has favorable accumulation conditions for shale gas ,thus can be selected as one of the play fairways in China .