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作 者:赵虎[1,2] 冯艺丹 王轶 李世临[4] 胥良君 邸志欣 朱彬瑞 ZHAO Hu;FENG Yidan;WANG Yi;LI Shilin;XU Liangjun;DI Zhixin;ZHU Binrui(Sichuan Province University Key Laboratory of Natural Gas Geology,SWPU,Chengdu 610500,China;School of Geoscisence and Technology,Southwest Petroleum University,Chengdu 610500,China;Exploration Division,PetroChina Southwest Oil&Gasfield Company,Chengdu 610041,China;Chongqing Gas District,PetroChina Southwest Oil&Gasfield Company,Chongqing 400707,China;Research Center,SINOPEC Geophysical Corporation,Nanjing 210000,China;Southwest Geophysical Research Institute of CNPC Eastern Geophysical Company,Chengdu 610213,China)
机构地区:[1]西南石油大学天然气地质四川省重点实验室,四川成都610500 [2]西南石油大学地球科学与技术学院,四川成都610500 [3]中国石油西南油气田分公司勘探事业部,四川成都610041 [4]中国石油西南油气田分公司重庆气矿,重庆400707 [5]中国石化石油工程地球物理有限公司科技研发中心,江苏南京210000 [6]中国石油东方地球物理公司西南物探研究院,四川成都610213
出 处:《天然气地球科学》2022年第1期153-167,共15页Natural Gas Geoscience
基 金:中国石油—西南石油大学创新联合体科技合作项目(编号:2020CX010201)资助。
摘 要:近年来随着国家油气需求进一步增加,致密储层逐渐成为研究热点,川东地区凉高山组是典型的致密砂岩储层,具有层系多、河道规模大、砂体厚、生储组合好和烃源丰富等优点,具有较好的勘探前景,但也存在储层岩性致密、孔渗低、勘探程度低等难题。针对这些问题,从地震地质资料入手,详细分析凉高山组纵横向砂岩储层地震地质特征。研究发现:优势砂体发育在凉高山组中上部,中下部烃源岩发育好,水下分流河道及河口坝为主要储集体,河道宽度大,河道沙坝呈块状非连续性分布,油气保存条件较好。储层甜点区受相带控制特征明显,远离通天断层的向斜区、河道中沙坝、裂缝发育区为最有利的勘探区域。In recent years,as the national oil and gas demand has further increased,tight reservoirs have gradually become a research hotspot. The Lianggaoshan Formation in eastern Sichuan Basin is a typical tight sandstone reservoir,which has the advantages of multiple layers,large scale of river channels,thick sand bodies,good source-reservoir assemblage and abundant hydrocarbon sources,and has good prospects for exploration.However,there are also problems such as tight reservoir lithology,low porosity and permeability,and low degree of exploration. In response to these problems,this article starts with seismic geological data and analyzes in detail the seismic geological characteristics of vertical and horizontal sandstone reservoirs in the Lianggaoshan Formation,and the research finds that dominant sand bodies are developed in the middle and upper parts of Lianggaoshan Formation,source rocks are well developed in the middle and lower parts of Lianggaoshan Formation. The underwater distributary channels and estuary dams are the main reservoirs,the channel width is large,and the channel sand dams are distributed in blocky discontinuity,and the oil and gas preservation conditions are good. Reservoir sweet spots are obviously controlled by facies belts,and syncline areas far away from the Tongtian fault,sand bars in river channels,and fracture-developed areas are the most favorable exploration areas.
分 类 号:TE132.14[石油与天然气工程—油气勘探]
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