鄂尔多斯盆地代家坪地区延长组8段低孔渗砂岩成岩作用及成岩相

doi:10.11743/ogg20160202

石油与天然气地质 ›› 2016, Vol. 37 ›› Issue (2): 155-164.doi: 10.11743/ogg20160202

鄂尔多斯盆地代家坪地区延长组8段低孔渗砂岩成岩作用及成岩相

周翔¹, 何生¹, 陈召佑², 王芙蓉¹, 周思宾², 刘萍¹

1. 中国地质大学(武汉)构造与油气资源教育部重点实验室, 湖北武汉 430074;
2. 中国石化华北油气分公司勘探开发研究院, 河南郑州 450006

收稿日期:2015-06-08 修回日期:2015-12-10 出版日期:2016-04-08 发布日期:2016-04-29
通讯作者: 何生(1956-),男,教授、博士生导师,油气地质。E-mail:shenghe@cug.edu.cn。 E-mail:shenghe@cug.edu.cn
作者简介:周翔(1988-),男,博士研究生,储层地质与有机地球化学。E-mail:zhouxiang2206@163.com。
基金资助:
国家科技重大专项(2016ZX05005-001);高等学校学科创新引智计划资助项目(B14031)。

Diagenesis and diagenetic facies of low porosity and permeability sandstone in Member 8 of the Yanchang Formation in Daijiaping area, Ordos Basin

Zhou Xiang¹, He Sheng¹, Chen Zhaoyou², Wang Furong¹, Zhou Sibin², Liu Ping¹

1. Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China;
2. Exploration and Production Research Institute, SINOPEC North China Company, Zhengzhou, Henan 450006, China

Received:2015-06-08 Revised:2015-12-10 Online:2016-04-08 Published:2016-04-29

摘要/Abstract

摘要： 上三叠统延长组长8段砂岩是鄂尔多斯盆地代家坪地区重要的勘探目的层，以长石岩屑细砂岩和岩屑长石细砂岩为主，目前处于中成岩A期，属典型低孔特低渗储层。强烈的成岩作用是储层致密化的主要原因，其中压实作用和碳酸盐岩胶结作用造成储层原生孔隙大量丧失，绿泥石胶结和长石溶蚀对储层物性改善起到了积极作用，碱-酸-碱交替的成岩介质环境变化控制了粘土矿物形成、碳酸盐胶结物沉淀以及长石溶蚀作用。综合多项定性和定量参数，将长8段砂岩划分为5种成岩相类型，定量计算不同成岩相埋藏过程中孔隙演化表明，由沉积作用形成的不同成岩相中砂岩原始组分差异是导致胶结类型和溶蚀程度差异的物质基础，不同成岩相中成岩作用类型及强度是造成砂岩孔隙演化及物性差异的主要原因。优质砂岩储层分布与成岩相密切相关，其中分布于水下分流河道砂体中的弱压实绿泥石胶结相和中压实次生溶蚀相砂岩物性最好，是研究区长8段砂岩储层中最有利的成岩相带。

关键词: 成岩作用, 成岩相, 致密砂岩, 延长组, 鄂尔多斯盆地

Abstract: Member 8 sandstone of the Upper Triassic Yanchang Formation is the major exploration target in Daijiaping area, Ordos Basin.Member 8 sandstone of the Yanchang Formation mainly consists of feldspathic litharenite and lithic arkose, currently is at the A phase of middle diagenesis stage, and is categorized into low-porosity and extremely low-permeability reservoir.The intensive diagenesis is main cause of reservoir densification.Compaction and carbonate cementation largely reduce the primary porosity, while chlorite cementation and feldspar dissolution improve the reservoir quality, and the alkaline-acidic-alkaline change of digenetic environment control the formation of clay mineral, the precipitation of carbonate cements, and the dissolution of feldspar.Five types of diagenetic facies are identified in the Member 8 sandstone of the Yanchang Formation according to multiple qualitative and quantitative parameters.Quantitative calculation of porosity evolution in different digenesis facies shows that the differences of primitive compositions among different diagenetic facies as a result of sedimentation is the material basis of the cementation types and the dissolution strength, while the differences of diagenesis types and intensity is the main cause of the differences in porosity evolution and reservoir quality.The distribution of high quality reservoirs is closely related to the diagenesis facies.The weakly-compacted chlorite cement facies and modera-tely-compacted secondary dissolution facies in subaqueous distributary channel sandstone show the best reservoir quality, thus are the most favorable diagenesis facies in the Member 8 sandstone of the Yanchang Formation reservoir.

Key words: diagenesis, diagenetic facies, tight sandstone, Yanchang Formation, Ordos Basin

中图分类号:

TE122.2

周翔,何生,陈召佑,等. 鄂尔多斯盆地代家坪地区延长组8段低孔渗砂岩成岩作用及成岩相[J]. 石油与天然气地质, 2016, 37(2): 155-164. doi: 10.11743/ogg20160202 Zhou Xiang,He Sheng,Chen Zhaoyou,et al. Diagenesis and diagenetic facies of low porosity and permeability sandstone in Member 8 of the Yanchang Formation in Daijiaping area, Ordos Basin[J]. Oil & Gas Geology, 2016, 37(2): 155-164. doi: 10.11743/ogg20160202

参考文献

[1] 高辉,李天太,解永刚,等.三角洲前缘亚相致密砂岩储层的成岩作用与有利成岩相带:以鄂尔多斯盆地子洲气田山23段砂岩为例[J].现代地质,2013,27(2):373-388. Gao Hui,Li Tiantai,Xie Yonggang,et al.Diagenesis and favorable diagenetic facies of tight sandstone reservoir in delta front subfacies:a case study on the shan₂² sandstone of Zizhuo gas field in Ordos Basin[J].Geoscience,2013,27(2):373-388.
[2] 王峰,陈蓉,田景春,等.鄂尔多斯盆地陇东地区长4+5油层组致密砂岩储层成岩作用及成岩相[J].石油与天然气地质,2014,35(2):199-206. Wang Feng,Chen Rong,Tian Jingchun,et al.Diagenesis and diagenetic facies ofthe Chang 4+5 tight sandstone reservoirs in Longdong area,Ordos Basin[J].Oil & Gas Geology,2014,35(2):199-206.
[3] 张海涛,时卓,石玉江,等.低渗透致密砂岩储层成岩相类型及测井识别方法——以鄂尔多斯盆地苏里格气田下石盒子组8段为例[J].石油与天然气地质,2012,33(2):256-264. Zhang Haitao,Shi Zhuo,Shi Yujiang,et al.Diagenetic facies types and logging identification methods for low-permeability tight sandstone reservoir:a case study on the 8^th member of Xiashihezi Formation in Sulige gasfield,Ordos Basin[J].Oil & Gas Geology,2012,33(2):256-264.
[4] 张哨楠,胡江柰,沙文武,等.鄂尔多斯盆地南部镇泾地区延长组的沉积特征[J].矿物岩石,2000,20(4):25-30. Zhang Shaonan,Hu Jiangnai,Sha Wenwu,et al.The sedimentary characteristics of Yanchang Formation in Zhenyuan and Jingchuan districts,southern part of Ordos Basin[J].Journal of Mineralogy and Petrology,2000,20(4):25-30.
[5] 罗静兰,李忠兴,史成恩,等.鄂尔多斯盆地西南部上三叠统延长组长8、长6油层组的沉积体系与物源方向[J].地质通报,2008,27(1):101-111. Luo Jinglan,Li Zhongxing,Shi Chengen,et al.Depositional systems and provenance directions for the Chang 6 and Chang 8 reservoir groups of the Upper Triassic Yanchang Formation in the southwestern Ordos Basin,China[J].Geological Bulletin of China,2008,27(1):101-111.
[6] 黄思静,谢连文,张萌,等.中国三叠系陆相砂岩中自生绿泥石的形成机制及其与储层孔隙保存的关系[J].成都理工大学学报(自然科学版),2004,31(3):273-281. Huang Sijing,Xie Lianwen.Zhang Meng,et al.Formation mechanism of authigenic chlorite and relation to preservation of porosity in nonmarine Triassic reservoir sandstones,Ordos Basin and Sichuan Basin,China[J].Journal of Chengdu University of Technology(Science & Technology Edition),2004,31(3):273-281.
[7] Jeffry D G.Origin and growth mechanism of authigenic chlorite in sandstones of the lower Vicksburg formation,South Texas[J].Journal of Sedimentary Research,2001,71(1):27-36.
[8] 刘春燕.致密碎屑岩储层"甜点"形成及保持机理——以鄂尔多斯盆地西南部镇泾地区延长组长8油层组为例[J].石油与天然气地质,2015,36(6):873-879. Liu Chunyan.Formation and preservation mechanism of sweet spot in tight clastic reservoirs-A case study of Chang 8 oil layer of Yanchang Formation in Zhenjing area,southwest Ordos Basin[J].Oil & Gas Geology,2015,36(6):873-879.
[9] Baker J C,Havord P J,Martin K R,et al.Diagenesis and petrophysics of the Early Permian Moogooloo Sandstone,soutthern Carnarvon Basin,Weatern Australia[J].AAPG Bulletin,2000,84(2):250-265.
[10] 张永旺,曾溅辉,曲正阳,等.东营凹陷砂岩储层自生高岭石发育特征与成因机制[J].石油与天然气地质,2015,36(1):73-79. Zhang Yongwang,Zeng Jianhui,Qu Zhengyang,et al.Development characteristics and genetic mechanism of authigenic kaolinite in sandstone reservoir of the Dongying Sag,Bohai Bay Basin.[J].Oil & Gas Geology,2015,36(1):73-79.
[11] 王琪,禚喜准,陈国俊,等.延长组砂岩中碳酸盐胶结物氧碳同位素组成特征[J].天然气工业,2007,27(10):28-32. Wang Qi,Zhou Xizhun,Chen Guojun,et al.Characterics of carbon and oxygen isotopic compositions of carbonate cements in Triassic Yanchang sandstone in Ordos Basin[J].Natural Gas Industry,2007,27(10):28-32.
[12] 邹才能,陶士振,周慧,等.成岩相的形成、分类与定量评价方法[J].石油勘探与开发,2008,35(5):526-540. Zou Caineng,Tao Shizhen,Zhou Hui,et al.Genesis,classification and evaluation method of diagenetic facies[J].Petroleum Exploration and Development,2008,35(5):526-540.
[13] 王昌勇,王成玉,梁晓伟,等.鄂尔多斯盆地姬塬地区上三叠统延长组长8油层组成岩相[J].石油学报,2011,32(4):596-604. Wang Changyong,Wang Chengyu,Liang Xiaowei,et al.Diagenetic facies ofthe Chang8 oil-bearing layer of the Upper Triassic Yanchang Formation in the Jiyuan area,Ordos Basin[J].Acta Petrolei Sinica,2011,32(4):596-604.
[14] 付晶,吴胜和,付金华,等.鄂尔多斯盆地陇东地区延长组储层定量成岩相研究[J].地学前缘,2013,20(2):86-97. Fu Jing,Wu Shenghe,Fu Jinhua,et al.Research on quantitative diagenetic facies of the Yanchang Formation in Longdong area,Ordos Basin[J].Earch Scinence Frontiers,2013,20(2):86-97.
[15] 罗静兰,张成立,闫世可,等.盆地埋藏史及其对砂岩储层物性演化的影响-以陕北延长油区砂岩储层为例[J].石油与天然气地质,2001,22(2):123-123. Luo Jinglan,Zhang Chengli,Yan Shike,et al.Effect of burial history on physical property of sandstone reservoir:take Yanchang oil region in north Shaanxi as an example.[J].Oil & Gas Geology,2001,22(2):123-123.
[16] 吴小斌,侯加根,孙卫.特低渗砂岩储层微观结构及孔隙演化定量分析[J].中南大学学报:自然科学版,2011,42(11):3438-3445. Wu Xiaobin,Hou Jiagen,Sun Wei.icrostructure characteristics and quantitative analysis on porosity evolution of ultra-low sandstone reservoir[J].Journal of Central South University(Science and Technology),2011,42(11):3438-3445.
[17] Scherer,M.Parameters influencing porosity in sandstones:a model for sandstone porosity prediction[J].AAPG Bulletin,1987,71(5):485-491.
[18] Beard D C,Weyl P K.Influence of texture on porosity and permeability of unconsolidated sand[J].AAPG Bulletin,1973,57(2):349-369.
[19] Ehrenbeg S N.Measuring sandstone compaction from modal analyses of thin section:how to do it and what the result mean[J].Journal of Sediment Research,1995,65(2a):369-379.
[20] Nguyen B T T,Jones S J,Goulty N R,et al.The role of fluid pressure and diagenetic cements for porosity preservation in Triassic fluvial reservoir of the Central Craben,North Sea[J].AAPG Bulletin,2013,97(8):1273-1302.

鄂尔多斯盆地代家坪地区延长组8段低孔渗砂岩成岩作用及成岩相

Diagenesis and diagenetic facies of low porosity and permeability sandstone in Member 8 of the Yanchang Formation in Daijiaping area, Ordos Basin

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