吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (5): 1235-1246.doi: 10.13278/j.cnki.jjuese.20180094

• 地质与资源 • 上一篇    下一篇

渤中凹陷CFD18-2油田高岭石胶结作用及其对储层物性的影响

陈思芮1, 曲希玉1, 王冠民1, 王清斌2, 曹英权1   

  1. 1. 中国石油大学(华东)地球科学与技术学院, 山东 青岛 266580;
    2. 中海石油(中国)有限公司天津分公司, 天津 300459
  • 收稿日期:2018-05-05 发布日期:2019-10-10
  • 通讯作者: 曲希玉(1977-),男,副教授,博士,主要从事流体-岩石相互作用、储层及沉积方面的研究,E-mail:quxiyu@upc.edu.cn E-mail:quxiyu@upc.edu.cn
  • 作者简介:陈思芮(1994-),男,硕士研究生,主要从事储层地质学方面的研究,E-mail:393960958@qq.com
  • 基金资助:
    国家科技重大专项(2016ZX05024-003-006);中央高校基本科研业务费专项资金(12CX04004A)

Kaolinite Cementation and Its Influences on Reservoir Properties in CFD18-2 Oilfield in Bozhong Sag

Chen Sirui1, Qu Xiyu1, Wang Guanmin1, Wang Qingbin2, Cao Yingquan1   

  1. 1. College of Geoscience, China University of Petroleum, Qingdao 266580, Shandong, China;
    2. Tianjin Branch of CNOOC, Tianjin 300459, China
  • Received:2018-05-05 Published:2019-10-10
  • Supported by:
    Supported by National Science and Technology Major Project (2016ZX05024-003-006) and Fundamental Research Funds for the Central University (12CX04004A)

摘要: 为探究成岩作用过程中所形成的次生黏土矿物对储层物性的影响,借助偏光显微镜及扫描电镜的镜下分析,并结合储层物性等数据,对渤中凹陷附近沙垒田凸起东南部CFD18-2油田东三段高岭石的特征、类型、成因及其对储层物性的影响进行了研究。研究结果表明:1)研究区高岭石为有机酸溶蚀长石形成的自生高岭石,呈现典型的"手风琴状"及"蠕虫状",常充填于粒间孔、长石次生溶孔及碳酸盐胶结物溶孔中并形成良好的晶间孔隙。2)研究区主要发育两期高岭石,第一期主要充填于早期碳酸盐胶结物溶孔中,呈微小"蠕虫状";第二期充填于铁方解石与铁白云石胶结物溶孔中,部分高岭石具碱性溶蚀特征,且第二期高岭石与晚期伊利石共生。3)研究区东三段储层具备一定的渗流能力,使长石溶蚀形成的"副产物"被流体带走;但在破坏性成岩作用下,储层渗流能力会逐渐变差,最终使得"副产物"堆积于孔隙,降低储层物性。4)高岭石及同期硅质胶结物对储层物性的影响是一把"双刃剑",当高岭石及硅质的体积分数低于6.81%时,长石溶蚀有利于改善储层物性;当高岭石及硅质的体积分数高于6.81%时,则不利于储层物性的改善。

关键词: 高岭石, 储层物性, 溶蚀作用, 形成期次, CFD18-2油田

Abstract: Kaolinite is a common aluminum-rich silicate clay mineral in sandstone reservoirs. It usually fills in the pore-throat of reservoirs. Its appearance generally indicates the dissolution of feldspars and the formation of secondary pores. The authors studied the characteristics, types, origin of the kaolinite through analyzing the data of polarizing microscope, scanning electron microscope, and the physical properties of the reservoir in the third member of Dongying Formation (Ed3) of CFD18-2 oil field in the southeastern part of Shaleitian uplift in Bozhong Sag. The results reveal that:1) The kaolinite of the study area is authigenic kaolinite formed by feldspar dissolution by organic acid. The authigenic kaolinite shows typical "accordion" and "worm" shapes, and is often filled in intergranular pores, feldspar secondary dissolution pores, and carbonate cement dissolution pores, forming good inter-crystalline pores. 2) Two phases of kaolinite are developed in the study area. The first phase of kaolinite is mainly filled in the dissolution pores of early carbonate cement, showing a tiny "worm" shape; the second phase of kaolinite is filled in the dissolution pores of ferrocalcite and ankerite cements, some kaolinite have the characteristics of alkaline dissolution, and the second phase of kaolinite is symbiotic with late illite. 3) The reservoir in the third member of Dongying Formation has a certain ability to seep, so that the "byproducts" formed by feldspar dissolution can be taken away by the fluid. However, under the action of destructive diagenesis, the seepage ability of the reservoir will gradually deteriorate, eventually causing "byproducts" to accumulate in the pores and reduce the physical properties of the reservoir. 4) The effect of kaolinite and siliceous cement on reservoir properties are "double-edged sword". When the content of kaolinite and siliceous material is low, dissolution of feldspar is beneficial to improving the physical properties of reservoirs; while the high content of kaolinite and siliceous is not conducive to the improvement of reservoir quality.

Key words: kaolinite, reservoir properties, dissolution, formation stage, CFD18-2 oil field

中图分类号: 

  • P59
[1] 赵明,季俊峰,陈振岩,等. 大民屯凹陷古近系高岭石亚族和伊/蒙混层矿物特征与盆地古温度[J]. 中国科学:地球科学,2011,41(2):169-180. Zhao Ming, Ji Junfeng, Chen Zhenyan,et al. Evolution of Kaolinite Subgroup Minerals and Mixed-Layer Illite/Smectite in the Paleogene Damintun Depression in Liaohe Basin of China and Its Implication for Paleotemperature[J]. Scientia Sinica:Terrae, 2011,41(2):169-180.
[2] 张关龙,陈世悦,鄢继华,等. 郑家、王庄地区沙三段高岭石矿物特征及对储层物性的影响[C]//第三届全国沉积学大会论文摘要汇编. 成都:[s.n.],2004:221-223. Zhang Guanlong, Chen Shiyue, Yan Jihua,et al. Characteristics of Kaolinite Minerals in the Third Member of Shahejie Formation in Zhengjia and Wangzhuang Area and their Influence on Reservoir Properties[C]//The 3rd National Conference on Sedimentology Abstract Compendium. Chengdu:[s.n.], 2004:221-223.
[3] Hassan B, Mervat M H. Kaolinite in the Upper Cretaceous-Paleogene Sedimentary Facies of Bahariya Oasis, Egypt:Nature and Origin[J]. Neues Jahrbuch für Geologie und Paläontologie-Abhandlungen, 2009, 253(2/3):313-325.
[4] Jiménez-Millán J, Velilla N, Vázquez M. Two-Stage Formation of Kaolinite in Shear-Zone Slates, Southern Iberian Massif, SE Spain[J]. Clay Minerals, 2007, 42(3):273-286.
[5] Katarzyna G. The Role of Diagenesis in the Formation of Kaolinite Raw Materials in the Santonian Sediments of the North-Sudetic Trough (Lower Silesia, Poland)[J]. Applied Clay Science,1997,12(4):313-328.
[6] 韩信.苏里格气田东北部召30井区盒8段自生高岭石的微观特征及其对储层的影响[D]. 成都:成都理工大学,2016. Han Xin. Microscopic Characteristics and Its Effect on the Reservoir of the Authigenic Kaolinite of the Eighth Member of Shihezi Formation in the Zhao 30 Well Block of the Northeastern Section of the Surig Gas Field[D].Chengdu:Chengdu University of Technology, 2016.
[7] 邹华耀,郝芳,柳广弟,等. 库车冲断带巴什基奇克组砂岩自生高岭石成因与油气成藏[J]. 石油与天然气地质,2005,26(6):786-791. Zou Huayao, Hao Fang, Liu Guangdi,et al. Genesis of Authigenic Kaolinite and Gas Accumulation in Bashijiqike Fm Sandstone in Kuqa Thrust Belt[J]. Oil & Gas Geology, 2005, 26(6):786-791.
[8] 庞小军,王清斌,杜晓峰,等. 渤中凹陷西北缘古近系物源演化及其对储层的影响[J].大庆石油地质与开发,2016,35(5):34-41. Pang Xiaojun, Wang Qingbin, Du Xiaofeng,et al. Matter Provenance Evolution and Its Influence on Palaeogene Reservoirs in the Northwestern Margin of the Bozhong Sag[J]. Petroleum Geology & Oilfield Development in Daqing, 2016, 35(5):34-41.
[9] 江涛,李慧勇,李新琦,等. 渤西沙垒田凸起走滑断裂背景下油气成藏特征[J].岩性油气藏,2015,27(5):172-175. Jiang Tao, Li Huiyong, Li Xinqi,et al. Hydrocarbon Accumulation Characteristics Under the Background of Strike-Slip Faults in Shaleitian Uplift, West Bohai Sea[J]. Lithologic Reservoirs, 2015, 27(5):172-175.
[10] 朱雯. 渤中凹陷西部东二段沉积体系研究[D]. 荆州:长江大学,2017. Zhu Wen. Study on Depositonal System of the Middle Section of Dongying Formation in Western Bozhong Sag, Bohai Bay[D]. Jingzhou:Yangtze University, 2017.
[11] 江涛,李慧勇,茆利,等. 沙南凹陷沙中构造带油气成藏特征及主控因素分析[J]. 断块油气田,2014,21(6):692-696. Jiang Tao, Li Huiyong, Mao Li,et al. Analysis on Oil and Gas Accumulation Features and Main Controlling Factors of Shazhong Structural Belt in Shanan Depression[J]. Fault-Block Oil & Gas Field, 2014, 21(6):692-696.
[12] 李顺利,朱筱敏,刘强虎,等. 沙垒田凸起古近纪源-汇系统中有利储层评价与预测[J]. 地球科学,2017,42(11):1994-2009. Li Shunli, Zhu Xiaomin, Liu Qianghu,et al. Evaluation and Prediction of Favorable Reservoirs in Source-to-Sink Systems of the Palaeogene, Shaleitian Uplift[J]. Earth Science, 2017, 42(11):1994-2009.
[13] 任拥军,杜雨佳,王冠民,等. 渤中凹陷古近系优质烃源岩特征及分布[J]. 油气地质与采收率,2015,21(6):5-13. Ren Yongjun, Du Yujia, Wang Guanmin,et al. Characteristics and Distribution of Paleogene High-Quality Source Rocks in Bozhong Sag[J]. Petroleum Geology and Recovery Efficiency, 2015, 21(6):5-13.
[14] 石文龙,张志强,彭文绪,等. 渤海西部沙垒田凸起东段构造演化特征与油气成藏[J]. 石油与天然气地质,2013,34(2):242-247. Shi Wenlong, Zhang Zhiqiang, Peng Wenxu,et al. Tectonic Evolution and Hydrocarbon Accumulation in the East Part of Shaleitian Sailent,Western Bohai Sea[J]. Oil & Gas Geology, 2013,34(2):242-247.
[15] 庞小军,王清斌,万琳,等. 沙南凹陷东北缘东三段储层差异及其成因[J]. 中国矿业大学报,2018,47(3):596-612. Pang Xiaojun, Wang Qingbin, Wan Lin, et al. Quality Differences and Its Influence on Glutenite Reservoirs in the Ed3 of the Northeast Margin, Shanan Sag, Bohai Sea[J]. Journal of China University of Mining & Technology, 2018,47(3):596-612.
[16] 于水.曹妃甸18-2油气田凝析气藏探明储量报告[R]. 天津:中海石油(中国)天津分公司,1997. Yu Shui. Report of Proved Reserve of Caofeidian 18-2 Oil and Gas Field[R]. Tianjin:Tianjin Branch of CNOOC(China), 1997.
[17] Stoessell R K. Kaolinite Formation in Clastic Reservoirs:Carbon Dioxide Factor[J]. AAPG Bulletin,1981,65(5):991-998.
[18] 刘涛. 姬塬地区长8油层组砂岩中自生高岭石对储层发育的影响[D]. 成都:成都理工大学,2011. Liu Tao. The Influence of Authigenic Kaolinite on the Reserivor Development in Chang 8 Oil-Bearing Formation Sandstone of Jiyuan Area[D]. Chengdu:Chengdu University of Technology, 2011.
[19] 于兴河. 油气储层地质学基础[M]. 北京:石油工业出版社,2009. Yu Xinghe. Geological Foundation of Oil and Gas Reservoir[M]. Beijing:Petroleum Industry Press, 2009.
[20] 丁晓琪,韩玫梅,张哨楠,等. 大气淡水在碎屑岩次生孔隙中的作用[J]. 地质论评,2014,60(1):145-158. Ding Xiaoqi, Han Meimei, Zhang Shaonan,et al. The Role of Atmospheric Fresh Water in Secondary Pores of Clastic Rock[J]. Geological Review, 2014, 60(1):145-158.
[21] 柳广弟. 石油地质学[M]. 4版. 北京:石油工业出版社,2009. Liu Guangdi. Petroleum Geology[M].4th ed. Beijing:Petroleum Industry Press, 2009.
[22] 戴金星. 中国东部无机成因气及其气藏形成条件[M]. 北京:科学出版社,1995. Dai Jinxing. Inorganic Generating Gas and Formation Conditions of Gas Reservoirs in Eastern China[M]. Beijing:Science Press, 1995.
[23] 肖卫勇,王良书,李华,等. 渤海盆地地温场研究[J]. 中国海上油气,2001,15(2):105-110. Xiao Weiyong, Wang Liangshu, Li Hua,et al. Study on Ground Temperature Field in Bohai Basin[J]. China Offshore Oil and Gas, 2001, 15(2):105-110.
[24] 碎屑岩成岩阶段划分:SY/T5477-2003[S].北京:石油工业出版社, 2003. Division of Diagenetic Stages in Clastic Rocks:SY/T5477-2003[S].Beijing:Petroleum Industry Press, 2003.
[1] 巨银娟, 张小莉, 张永庶, 陈琰. 柴达木盆地昆北地区基岩储层裂缝特征[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1660-1671.
[2] 邱隆伟, 师政, 付大巍, 潘泽浩, 杨生超, 曲长胜. 临南洼陷沙三段孔隙度控制因素分析与定量模型[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1321-1331.
[3] 陈彬滔, 潘树新, 梁苏娟, 张庆石, 刘彩燕, 王革. 陆相湖盆深水块体搬运体优质储层的主控因素以松辽盆地英台地区青山口组为例[J]. 吉林大学学报(地球科学版), 2015, 45(4): 1002-1010.
[4] 田建锋,喻建,张庆洲. 孔隙衬里绿泥石的成因及对储层性能的影响[J]. 吉林大学学报(地球科学版), 2014, 44(3): 741-748.
[5] 张云峰, 王国强, 付宝利, 李晶, 王春香. 长岭断陷深层碎屑岩储层成岩作用及异常高孔带成因[J]. J4, 2011, 41(2): 372-376.
[6] 邓虎成, 周文, 姜文利, 刘岩, 梁峰. 鄂尔多斯盆地麻黄山西区块延长、延安组裂缝成因及期次[J]. J4, 2009, 39(5): 811-817.
[7] 曹瑞成,曲希玉,文 全,鲍春艳,刘剑营,刘 娜,刘 立. 海拉尔盆地贝尔凹陷储层物性特征及控制因素[J]. J4, 2009, 39(1): 23-0030.
[8] 冯娟萍,李文厚,欧阳征健,余 芳,曹红霞,赵 阳. 陕北青化砭油田长2砂岩储层物性的控制因素[J]. J4, 2008, 38(3): 417-0424.
[9] 高有峰,刘万洙,纪学雁,白雪峰,王璞珺,黄玉龙,郑常青,闵飞琼. 松辽盆地营城组火山岩成岩作用类型、特征及其对储层物性的影响[J]. J4, 2007, 37(6): 1251-1258.
[10] 吴颜雄,王璞珺,曲立才,闵飞琼,李喆,任利军. 营城组一段及下段岩性岩相和储层物性的精细刻画--基于标准剖面营一D1井全取心钻孔资料[J]. J4, 2007, 37(6): 1192-1202.
[11] 张莉,朱筱敏,钟大康,崔可平. 惠民凹陷古近系砂岩储层物性控制因素评价[J]. J4, 2007, 37(1): 105-0111.
[12] 张凡芹,王伟锋,王建伟,孙粉锦,刘锐娥. 苏里格庙地区凝灰质溶蚀作用及其对煤成气储层的影响[J]. J4, 2006, 36(03): 365-369.
[13] 王 蛟,姜在兴,操应长,邢焕清,王艳忠,罗文生. 山东东营凹陷永921地区沙四上亚段扇三角洲沉积与油气[J]. J4, 2005, 35(06): 725-0731.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!