CAJ | 학술논문

通过对苏里格气田北部盒_8、山_1段24口钻井572块样品的成岩作用研究表明,苏里格气田北部盒_8和山_1段主要经历了压实作用、胶结作用、次生加大作用、自生矿物的生成、交代和蚀变作用、溶蚀作用、破裂作用等.根据它们对孔隙发育的贡献分为建设性成岩作用、破坏性成岩作用、保持性成岩作用3种类型.其中,约80%的砂岩粒间孔具有溶蚀现象,溶蚀作用使储集层孔隙结构得到有效的改善,以次生粒间孔最为常见,粒内溶孔较少见,粘土质微孔发育,并与岩石中保存下来的剩余原生粒间孔组合构成溶孔一原生粒间孔组合、溶孔-粘土质微孔组合及溶孔-微孔-(裂缝、粒缘缝)组合.保持性成岩作用所生成的环边绿泥石包膜使部分孔隙得以保存,对储层的发育具有积极意义.根据铸体薄片、扫描电镜下所观察到的自生矿物类型以及X衍射等测试手段所揭示的I/S混层粘土矿物的演变、粘土矿物组合及矿物中的混层比,这些成岩作用被划分为早成岩A期、早成岩B期、中成岩A期、中成岩B期和晚成岩期3个阶段5个期次;成岩作用研究认为S4井,S5井,S6井和T5井区为有利储层分布区.
통과대소리격기전북부합_8、산_1단24구찬정572괴양품적성암작용연구표명,소리격기전북부합_8화산_1단주요경력료압실작용、효결작용、차생가대작용、자생광물적생성、교대화식변작용、용식작용、파렬작용등.근거타문대공극발육적공헌분위건설성성암작용、파배성성암작용、보지성성암작용3충류형.기중,약80%적사암립간공구유용식현상,용식작용사저집층공극결구득도유효적개선,이차생립간공최위상견,립내용공교소견,점토질미공발육,병여암석중보존하래적잉여원생립간공조합구성용공일원생립간공조합、용공-점토질미공조합급용공-미공-(렬봉、립연봉)조합.보지성성암작용소생성적배변록니석포막사부분공극득이보존,대저층적발육구유적겁의의.근거주체박편、소묘전경하소관찰도적자생광물류형이급X연사등측시수단소게시적I/S혼층점토광물적연변、점토광물조합급광물중적혼층비,저사성암작용피화분위조성암A기、조성암B기、중성암A기、중성암B기화만성암기3개계단5개기차;성암작용연구인위S4정,S5정,S6정화T5정구위유리저층분포구.
Study on the characteristics of diagenesis shows that He8 and Shanl Member in the north of Sulige gas field has undergone compaction, cementation, secondary enlargement, authi-genic mineral-producing, metasomatic alteration, dissolution, as well as fracturing processes re-spectively. According to their contribution to pores, diagenesis can be divided into three types, constructive,destructive and retention processes. Compaction process resulted in sharp reduction of 20%～25% in pore. Corrosion occurred in about 80% sand pore,which is the most important factor for the improvement of reservoir pore structure. Secondary intergranular pore is common, but intergranular corrosive pore is seldom. The well-developed clay micropore and residual inter-granular pore form several combinations. In retention processes, the grain-coating of lining chlo-rite resulted in the preservation of some pores and has positive meanings for reservoir develop-ment. Based on the observation of cores and slices and application of SEM/CL and X ray diffrac-tion technology,combined with the types of authigenic mineral, formation temperature, producing order, relative order of the diagenetic evolution of various minerals, the structure and texture char-acteristics of the clastic and interstitial material,and I/S clay mineral evolution, these diagenesis were divided into 3 stages and 5 phases,including A and B the second phase of early diagenesis,A and B the second phase of middle diagenesis,and late diagenesis. The area of S4,S5, S6 and T5 are considered to be favorable reservoir position according to the diagenetic study.