低频次叠加的同生溶蚀作用对滩相储层发育的控制——以川中栖霞组为例  

The control of syngenetic dissolution of low-frequency superposition on the development of shoal facies reservoir:a case study of Qixia Formation in central Sichuan

作　　者：韩心奕 伏美燕[1,3] 邓虎成[1,3] 吴冬 胥旺 何溥为 陈培 郭恒玮 HAN Xinyi;FU Meiyan;DENG Hucheng;WU Dong;XU Wang;HE Puwei;CHEN Pei;GUO Hengwei(College of Energy Resources,Chengdu University of Technology,Chengdu 610059,China;Southwest Geophysical Research Institute,BGP Inc.,CNPC,Chengdu 610213,China;State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China;Research Institute of Petroleum Exploration and Development,Southwest Oil&Gas Field Company,PetroChina,Chengdu 610051,China)

机构地区：[1]成都理工大学能源学院,四川成都610059 [2]中国石油东方地球物理公司西南物探研究院,四川成都610213 [3]油气藏地质及开发工程国家重点实验室(成都理工大学),四川成都610059 [4]中国石油西南油气田公司勘探开发研究院,四川成都610051

出　　处：《断块油气田》2022年第2期239-244,255,共7页Fault-Block Oil & Gas Field

基　　金：西南油气田公司项目“高石梯地区栖霞组、长兴组储层综合评价研究”(2020-56205)。

摘　　要：川中地区栖霞组油气勘探已获得突破,但栖霞组优质储层类型及其形成机理尚不明确。文中综合利用川中高石梯-磨溪地区的岩心、录井、测井等资料及各类白云岩样品的地球化学测试数据,结合构造背景和沉积演化特征,对该地区栖霞组储层特征及其形成机理进行了研究。结果表明:该地区栖霞组储层发育晶粒白云岩、颗粒白云岩、斑状白云岩、砂屑灰岩、微亮晶球粒灰岩。储集空间以晶间孔、晶间溶孔和溶洞为主。储层类型包括溶洞型、溶孔-溶洞型和溶孔型。溶洞发育的白云岩、亮晶砂屑灰岩和微亮晶球粒灰岩储层对产能贡献明显,为该地区的优质储层。栖霞组优质储层发育于开阔台地的颗粒滩微相,主要受到古地貌缓坡部位的低频次叠加的同生溶蚀作用控制。根据储层演化过程建立了川中地区栖霞组优质储层发育模式。研究成果对于下一步分析川中地区储层分布规律提供了地质依据。A breakthrough has been made in the exploration of the Qixia Formation in the central Sichuan Basin,but the type and formation mechanism of the Qixia formation reservoir with high quality are not clear yet.In this paper,the reservoir characteristics and formation mechanism of the Qixia Formation in Gaoshiti-Moxi area of central Sichuan basin are studied by using core,logging data and geochemical test data of various dolomite samples,combined with tectonic background and sedimentary evolution characteristics.The results show that the lithologies of the Qixia Formation in this area include crystalline dolostone,grain dolostone,dolomitic limestone,intraclastic limestone,bioclastic limestone and microsparite pelletoid limestone.The void spaces are mainly composed of intercrystalline pore,intercrystalline dissolved pore and karst cave.The reservoir types include cave,dissolved pore-cave and pore.Dolomite,intraclastic limestone and microsparry pelletoid limestone reservoirs with karst caves contribute significantly to productivity and are the high-quality reservoirs in this area.The high quality reservoir of Qixia Formation was developed in the shoal microfacies of the open platform,which was mainly controlled by syngenetic dissolution of low-frequency superposition of the shoal located on the high position of paleogeomorphology.Based on the reservoir evolution process,the development model of Qixia Formation reservoir in central Sichuan Basin was established.This study provides geological basis for further study of reservoir distribution in central Sichuan Basin.

关 键 词：滩相 储层形成机理 同生溶蚀作用 热液作用 

分 类 号：TE122.2[石油与天然气工程—油气勘探]