Main Control Factors and Analysis of Reservoir Space Evolution of Reef-Beach Facies in Changxing - Feixianguan Formation of northeastern Sichuan Area

Expand
  •  
    (1.Lanzhou Library of Chinese Academy of Sciences,Lanz hou 730000,China;2.Key Laboratory of Petroleum Resources Research,Gansu Province/ Key Laboratory of Petroleum Resources Research,
    Institute of Geology and Geophysics,Chinese Academy of Sciences,Lanzhou 730000,China;
    3.Graduate University of Chinese Academy of Sciences,Beijing 100049,China;
    4.Research Institute of Shaanxi Yanchang Petoroleum(Group)CO.,LTD,xi′an 710075,China)

Received date: 2014-03-16

  Revised date: 2014-05-16

  Online published: 2014-10-10

Abstract

The Platform margin reef-beach facies and shoals facies were the foundation for high-quality reservoir development in Changxing-Feixianguan Formation of Northeastern Sichuan Area.Today's reservoir pore type is dominated by secondary porosity,including intergranular pore,interquartz pore,biological visceral pore,various types of dissolved pore,and cracks.Primary porosity has basically been transformed by diagenesis.Among them,interquartz pore,corrosion pore and cracks are the main reservoir space in the study area.In geological history,the study area has experienced seven kinds of main diagenesis,which have different effects on the reef-beach and shoals depositional system,especially the dolomitization,dissolution and fracturing.These effect results provide conditions for the development of high-quality reservoir:dolomitization transformed the reservoir pore structure of reef-beach facies,dissolution expanded solution pore types further,fracturing interconnected pores and provide migration pathways.Based on the SEM analyses and identification of core and flakes,reservoir space development features,diagenetic environment,rock characteristics and reservoir developmental conditions,the development of high quality reservoir system of reef-beach facies of different rock types in the study area is mainly controlled by three factors:reef-beach sedimentary microfacies,diagenesis,tectonic disruption.Under these three controlling factors,reef-beach facies reservoir porosity of Changxing Formation and Feixianguan Formation has a similar developmental process.They all experienced four-stage evolution process,and the slight difference is its pore types.The Changxing Formation porosity evolution process can be divided into original hole,intergranular hole,early burial dissolution hole and late burial dissolution|The Feixianguan Formation porosity evolution process can be divided into primary hole,oolitic die hole/grains dissolved pores,shallow holes and deep holes.In summary,dolomitization,fracturing,and dissolution are the key factors for reef-beach facies to develop into high quality reservoir.

 

 

 

 

 
 

Cite this article

LI Xiao-yan,WANG Qi,HAN Yuan-hong,TIAN Bing,XU Yong,WANG Fei-fei . Main Control Factors and Analysis of Reservoir Space Evolution of Reef-Beach Facies in Changxing - Feixianguan Formation of northeastern Sichuan Area[J]. Natural Gas Geoscience, 2014 , 25(10) : 1594 -1602 . DOI: 10.11764/j.issn.1672-1926.2014.10.1594

References

[1]Zhao Wenguang,Guo Tonglou,Cai Zhongxian ,et al.The controlling factors and types of carbonate reef of Permian Changxing Formation in northeast of Sichuan Basin[J].Geoscience,2010,24(5):951-956.[赵文光,郭彤楼,蔡忠贤,等.川东北地区二叠系长兴组生物礁类型及控制因素[J].现代地质,2010,24(5):951-956.]
[2]Zheng Rongcai,Dang Lurui,Wen Huaguo,et al.Diagenesis characteristics and system for dolostone in Feixianguan Formation of northeast Sichuan[J].Earth Science:Journal of China University of Geosciences,2011,36(4):659-669.[郑荣才,党录瑞,文华国,等.川东北地区飞仙关组白云岩成岩作用与系统划分[J].地球科学:中国地质大学学报,2011,36(4):659-669.]
[3]Ma Yongsheng,Guo Xusheng,Guo Tonglou,et al.Discovery of the large-scale Puguang Gas Field in the Sichuan Basin and its enlightenment for hydrocarbon prospecting[J].Geological Review,2005,51(4):477-480.[马永生,郭旭升,郭彤楼,等.四川盆地普光大型气田的发现与勘探启示[J].地质论评,2005,51(4):477-480.]
[4]Chen Qi,Hu Wenxuan,Li Qing ,et al.Characteristics and genesis of dolomitization in Changxing and Feixianguan Formations in Panlongdong,northeastern Sichuan Basin[J].Oil & Gas Geology,2012,33(1):84-93.[陈琪,胡文瑄,李庆,等.川东北盘龙洞长兴组—飞仙关组白云岩化特征及成因[J].石油与天然气地质,2012,33(1):84-93.]
[5]Li Baohua,Fu Shaohong,Gu Xuexiang,et al.Fluid inclusion characteristics of the Later Permain reservoir in the northeastern Sichuan and implications for petroleum accumulation[J].Bulletion of Mineralogy,Petrology and Geochemistry,2012,31(2):105-113.[李保华,付绍洪,顾雪祥,等.川东北地区上二叠统油气储层中流体包裹体特征及成藏期研究[J].矿物岩石地球化学通报,2012,31(2):105-113.]
[6]Wei Guoqi,Yang Wei,Li Jian,et al.Geological characteristics and exploration fields of subaerial natural gas in China[J].Natural Gas Geoscience,2014,25(7):957-970.[魏国齐,杨威,李剑,等.中国陆上天然气地质特征与勘探领域[J].天然气地球科学,2014,25(7):957-970.]
[7]Zhang Jianyong,Zhou Jinggao,Pan Liyin ,et al.The main origins of high quality reservoir in Feixianguan Formation in northeast Sichuan Basin:Atmospheric water eluviation and seepage-reflux dolomitization[J].Natural Gas Geoscience,2013,24(1):9-18.[张建勇,周进高,潘立银,等,川东北地区孤立台地飞仙关组优质储层形成主控因素——大气淡水淋滤及渗透回流白云石化[J].天然气地球科学,2013,24(1):9-18.]
[8]Ni Xinfeng,Chen Hongde,Wei Dongxiao.Distr ibution and accumulation of materials in shoal-reef compound gas deposits and reservoir characteristics:A case study of the Changxing-Feixian Formation in the Puguang Gasfield,northeastern Sichuan[J].Geology in China,2007,34(6):1045-1054[倪新锋,陈洪德,韦东晓.礁滩复合型气藏物质聚集分布及储层特征研究——以川东北地区普光气田长兴组飞仙关组为例[J].中国地质,2007,34(6):1045-1054.]
[9]Cheng Jinxiang,Guo Tonglou,Tan Qinyin,et al.Characteristics and controlling factors of the reef shoal reservoirs from the Changxing Formation-Feixianguan Formation in the Xuanhan-Daxian zone,northeastern Sichuan[J].Sedimentary Geology and Tethyan Geology,2011,31(3):64-70.[程锦翔,郭彤楼,谭钦银,等.川东北宣汉—达县地区长兴组—飞仙关组礁滩储层特征及其控制因素[J].沉积与特提斯地质,2011,31(3):64-70.]
[10]Ma Yongsheng,Mou Chuanlong,Tan Qinyin,et al.Reef- bank features of Permian Changxing Formation and Triassic Feixianguan Formation in the Daxian-Xuanhan area,Sichuan Province,south China and constraint for the reservoirs of natural gas[J].Earth Science Frontiers,2007,14(1):182-193.[马永生,牟传龙,谭钦银,等.达县—宣汉地区长兴组—飞仙关组礁滩相特征及其对储层的制约[J].地学前缘,2007,14(1):182-193.]
[11]Li Xiaoyan,Wang Qi,Zhang Rui,et al.Reservoir characteristics and main controlling factors of Upper Permian Panlongdong organic reefs in northeastern Sichuan[J].Natural Gas Geoscience,2009,20(1):63-69.[李小燕,王琪,张瑞,等.川东北地区上二叠统盘龙洞生物礁储层特征及其主控因素分析[J].天然气地球科学,2009,20(1):63-69.]
[12]Gao Mei sheng,Zheng Rongcai,Wen Huaguo ,et al.Lithological characteristics of dolomite in the Lower Triassic Feixianguan Formation of the NE Sichuan Basin,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2007,34(3):297-304.[高梅生,郑荣才,文华国,等.川东北下三叠统飞仙关组白云岩成因—来自岩石结构的证据[J].成都理工大学学报:自然科学版,2007,34(3):297-304.]
[13]He Ying,Guo Xusheng,Zhang Keyin,et al.Diagenesis of excellent reservoirs in Feixianguan Formation in northeastern Sichuan Basin[J].Natural Gas Industry,2007,27(1):21-61.[何莹,郭旭升,张克银,等.川东北飞仙关组优质储层形成研究[J].天然气工业,2007,27(1):21-61.]
[14]Chu Zhaohong.The Studies of Carbonate Resercoir in the Changxing and the Feixianguan Formations in the northeastern Sichuan Basin in China[D].Beijing:China University of Geosciences,2006.[储昭宏.川东北长兴组—飞仙关组碳酸盐岩储层研究[D].北京:中国地质大学,2006.]
 
Outlines

/