CAJ | 학술논문

下寒武统龙王庙组是四川盆地安岳特大型气田的主力储层。本文基于盆地周缘露头、钻井岩心和薄片资料，通过龙王庙组地层对比、储层岩石学、物性特征、成岩作用等的研究，探讨了龙王庙组储层形成分布的控制因素。四川盆地龙王庙组整体上具有可对比性，储层岩性主要为粉－细晶（残余）砂屑白云岩、粉－细晶（残余）鲕粒白云岩、粉－细晶白云岩。储层属于中低孔低渗型。孔隙度＞2％的储层厚度多在20～60 m，川中磨溪地区较高石梯地区厚，向西北方向剥蚀，向东南方向厚度减小。龙王庙组储层形成和分布主要受控于3个因素：拉张槽继承性古地貌、同生期喀斯特作用和液态烃充注作用。拉张槽断层下盘形成的古地貌高地控制了龙王庙组颗粒滩的发育；同生期大气淡水溶蚀作用形成粒间溶孔和粒内溶孔，为后期成岩流体的进入和溶蚀孔洞的扩溶奠定了基础；生排烃高峰期的烃类充注作用，既能形成大量孔隙，又能对储层起到积极的保持作用。绵阳—长宁拉张槽东西两侧断阶形成的古地貌高地控制了龙王庙组早期优质储层的形成和分布；中三叠世期间拉张槽内下寒武统供烃中心与川中古隆起重叠地区是龙王庙组晚期优质储层最发育地区。四川盆地内龙王庙组优质储层最发育和天然气大规模成藏最有利地区均是绵阳－长宁拉张槽与川中古隆起相重叠区的东侧，即高石梯—磨溪地区。
하한무통룡왕묘조시사천분지안악특대형기전적주력저층。본문기우분지주연로두、찬정암심화박편자료，통과룡왕묘조지층대비、저층암석학、물성특정、성암작용등적연구，탐토료룡왕묘조저층형성분포적공제인소。사천분지룡왕묘조정체상구유가대비성，저층암성주요위분－세정（잔여）사설백운암、분－세정（잔여）이립백운암、분－세정백운암。저층속우중저공저삼형。공극도＞2％적저층후도다재20～60 m，천중마계지구교고석제지구후，향서북방향박식，향동남방향후도감소。룡왕묘조저층형성화분포주요수공우3개인소：랍장조계승성고지모、동생기객사특작용화액태경충주작용。랍장조단층하반형성적고지모고지공제료룡왕묘조과립탄적발육；동생기대기담수용식작용형성립간용공화립내용공，위후기성암류체적진입화용식공동적확용전정료기출；생배경고봉기적경류충주작용，기능형성대량공극，우능대저층기도적겁적보지작용。면양—장저랍장조동서량측단계형성적고지모고지공제료룡왕묘조조기우질저층적형성화분포；중삼첩세기간랍장조내하한무통공경중심여천중고륭기중첩지구시룡왕묘조만기우질저층최발육지구。사천분지내룡왕묘조우질저층최발육화천연기대규모성장최유리지구균시면양－장저랍장조여천중고륭기상중첩구적동측，즉고석제—마계지구。
The Lower Cambrian Longwangmiao Formation is the play of the Anyue supergiant gas field in Sichuan Basin.Based on the integrated study of the outcrops on the basin margin and the drilling cores in Sichuan Basin,this paper discusses the controlling factors of the formation and distribution of the high-quality reservoirs of the Longwangmiao Formation through the researches on the strata correlation,reservoir petrology,property characteristics and diagenesis etc..The Longwangmiao Formation could be well correlated in the basin scale,and the reservoir rocks are composed of dolarenite dolomite,oolitic dolomite and crystalline dolomite.The reservoir is of the pore-fracture type with low porosity and low permeability.The reservoir thickness with the porosity over 2% is about 20~60 m.The reservoir in the Moxi area is much thicker than that in the Gaoshiti area.The penecontemporaneous selective fresh water dissolution and liquid hydrocarbon filling have been controlled by the Early Cambrian Mianyang-Changning intracratonic sag to a certain extent.Three factors control the formation and distribution of the good-quality reservoir rocks in Longwangmiao Formation,that is,the inherited palaeogeomorphology of the intracratonic sag,the contemporaneous karst and the liquid hydrocarbon filling.The paleohigh formed by the footwall of margin fault of the intracratonic sag controls the distribution of the grain bank of Longwangmiao Formation. The intergranular and intragranular dissolution pores produced by the contemporaneous atmospheric freshwater karstification are important for the upcoming fluid filling and further dissolution.The hydrocarbon filling at the peak period of the generation and expulsion of the source rocks is beneficial to the increase of pores and the protection of the previous pores.The paleohigh formed by the faults along the two sides of the Mianyang-Changning intracratonic sag controls the formation and distribution of the early high-quality reservoirs,and the overlapping areas of the Lower Cambrian hydrocarbon-generating center and the Chuanzhong paleouplift are the most favorable areas of the late good-quality reservoirs.The most profitable areas for the distribution of the high-quality reservoir rocks and natural gas accumulations in Longwangmiao Formation are the eastern part of the overlapping areas of the Mianyang-Changning intracratonic sag and the Chuanzhong paleouplift,that is,the Gaoshiti-Moxi area.