Natural Gas Geoscience

Previous Articles     Next Articles

Carbonate diagenesis in high frequency sequence:A case study of Serpukhovian of Lower Carboniferous in Marsel block,Kazakhastan

Wang Yuan,Lin Chang-song,Li Hao,Sun Yan-da,He Hai-quan,Wang Qing-long,Ji Mu-ye,Zhang Man-li   

  1. 1.School of Energy Resources,China University of Geosciences (Beijing),Beijing 100083,China;
    2.School of Ocean sciences,China University of Geosciences(Beijing),Beijing 100083,China;
    3.Geo-jade Petroleum Corporation,Beijing 100016,China
  • Received:2017-07-08 Revised:2017-12-20 Online:2018-01-10 Published:2018-01-10

Abstract:

Based on thin sections,cathodoluminescence(CL),scanning electron microscope(SEM),X-diffraction and imaging logging data analysis,Serpukhovian carbonate reservoir space types and properties,together with its diagenetic types,environments and evolution both in the Lower Carboniferous high frequency sequences and in the sequence boundaries were studied in Marsel block of southern Kazakhastan.The results show that in middle-lower part of Serpukhovian high frequency sequences (the 1st to 3rdforth-order sequences),penecontemporaneous and burial dolomitization combined with tectonic processes made great contribution to early-middle Serpukhovian carbonate reservoirs.While in middle-upper part of Serpukhovian high frequency sequences (the 4thto 6th forth-order sequences),penecontemporaneous and seepage-reflux dolomitization combined with strong penecontemporaneous and meteoric water dissolution at early diagenetic stage had significant impact on late Serpukhovian carbonate reservoirs quality.However,strong cementation and compaction with weak dissolution in burial diagenetic environment of middle Serpukhovian high frequency sequence (the third forth-order sequence) are key factors leading to poor reservoir properties.

Key words: Kazakhastan, Lower Carboniferous, Carbonate rocks, High frequency sequence framework, Reservoir diagenesis

CLC Number: 

  • TE122

[1]Fan Aiping,Yang Renchao,Han Zuozhen,et al.Carbonate diagenetic system of  Zhangxia Formation in west Shandong Province[J].Acta Sedimentologica Sinica,2015,33(1):67-78.
樊爱萍,杨仁超,韩作振,等.鲁西地区张夏组碳酸盐岩成岩系统[J].沉积学报,2015,33(1):67-78.
[2]Zhao Guoxiang,Wang Qingbin,Jin Xiaoyan,et al.Diagenesis of the Ordovician carbonates in Bozhong Depression,Bohai sea area[J].Geological Science and Technology Information,2015,34(5):1-7.
赵国祥,王清斌,金小燕,等.渤海海域渤中凹陷奥陶系碳酸盐岩成岩作用[J].地质科技情报,2015,34(5):1-7.
[3]Qian Zheng,Huang Xianxiong.Carbonate Diagenesis and Reservoirs of the Carboniferous in the Eastern Part of Sichuan Basin,China[M].Beijing:Petroleum Industry Press,2000:23-34.
钱峥,黄先雄.碳酸盐岩成岩作用及储层——以中国四川东部石炭系为例[M].北京:石油工业出版社,2000:23-34.
[4]Huang Sijing.Carbonate Diagenesis[M].Bejing:Geological Publishing House,2010:54-58.
黄思静.碳酸盐岩的成岩作用[M].北京:地质出版,2010:54-58.
[5]Qiu Guiqiang.Analysis on Lower Tertiary diagenetic sequence characteristics and their difference of reservoir in Dongying Sag[J].Acta Sedimentologica Sinica,2007,25(6):915-922.
邱桂强.东营凹陷古近系成岩层序特征与储集差异性分析[J].沉积学报,2007,25(6):915-922.
[6]Han Denglin,Zhang Changmin,Yin Taiju.Diagenetic reaction pattern of the sequence boundary and its impacts on reservoir quality[J].Oil & Gas Geology,2010,31(4):449-454.
韩登林,张昌民,尹太举.层序界面成岩反应规律及其对储层储集物性的影响[J].石油与天然气地质,2010,31(4):449-454.
[7]Lai Jin,Wang Guiwen,Chai Yu,et al.Diagenetic sequence stratigraphy characteristics of Lower Cretaceous Bashijiqike Formation in Kuqa Depression[J].Acta Sedimentologica Sinica,2015,33(2):394-407.
赖锦,王贵文,柴毓,等.库车坳陷白垩系巴什基奇克组成岩层序地层特征[J].沉积学报,2015,33(2):394-407.
[8]Read J F,Horbury A D.Eustasy and tectonic controls on porosity evolution beneath sequence-bounding unconformities and parasequence disconformities on carbonate platforms[J].Computers IEEE Transactions on,1993,65(3):677-678.
[9]He Zhiliang,Gao Zhiqian,Zhang Juntao,et al.Types of sequence boundaries and their control over formation and distribution of quality carbonate reservoirs[J].Oil & Gas Geology,2014,35(6):853-859.
何治亮,高志前,张军涛,等.层序界面类型及其对优质碳酸盐岩储层形成与分布的控制[J].石油与天然气地质,2014,35(6):853-859.
[10]Xu Guifen,Lin Changsong,Li Zhentao.Lithofacies paleogeopraphy and favorable reservoir of Lower Carboniferous in southern Kazakhstan[J].Journal of Northeast Petroleum University,2014,38(6):1-11.
徐桂芬,林畅松,李振涛.南哈萨克区块下石炭统层序岩相古地理及其对有利储层的控制[J].东北石油大学学报,2014,38(6):1-11.
[11]Zhen Junzhang,Zhou Haiyan,Huang Xianxiong.Basic characteristics of petroleum geology and exploration potential analysis in Kazakhstan[J].China Petroleum Exploration,2009,14(2):80-86.
郑俊章,周海燕,黄先雄.哈萨克斯坦地区石油地质基本特征及勘探潜力分析[J].中国石油勘探,2009,14(2):80-86.
[12]Pang Xiongqi,Huang Handong,Lin Changsong,et al.Formation,distribution,exploration,and resource/reserve assessment of superimposed continuous gas field in Marsel exploration area,Kazakhstan[J].Acta Petrolei Sinica,2014,35(6):1012-1056.庞雄奇,黄捍东,林畅松,等.哈萨克斯坦Marsel探区叠复连续气田形成、分布与探测及资源储量评价[J].石油学报,2014,35(6):1012-1056.
[13]Haq B U,Schutter S R.A chronology of Paleozoic sea-level changes[J].Science,2008,322 (5898):64-68.
[14]Li Li,Li Guorong,Yuan Shaomin,et al.Application of natural gamma energy spectrum logging curve in stratigraphic sequence division:A case study of Changxing Formation in northeastern Sichuan Basin[J].Computing Techniques for Geophysical and Geochemical Exploration,2012,34(6):691-695.
李丽,李国蓉,袁少民,等.自然伽玛能谱测井曲线在地层层序划分中的应用——以川东北地区长兴组碳酸盐岩地层为例[J].物探化探计算技术,2012,34(6):691-695.
[15]Scholle P A,Ulmerscholle D S.A Color Guide to the Petrography of Carbonate Rocks:Grains,Textures,Porosity,Diagenesis[M].Beijing:Petroleum Industry Press,2010:408-409.
彼得·A.肖勒,达娜·S.厄尔默-肖勒.姚根顺,等译.碳酸盐岩岩石学:颗粒、结构、孔隙及成岩作用[M].北京:石油工业出版社,2010:408-409.
[16]Wang Yinghua.Carbonate diagenesis and porosity evolution[J].Acta Sedimentologica Sinica,1992,10(3):85-95.
王英华.碳酸盐岩成岩作用与孔隙演化[J].沉积学报,1992,10(3):85-95.
[17]Wu Shiqiang,Zhu Jingquan,Wang Guoxue,et al.Types and origin of Cambrian-Ordovician dolomites in Tarim Basin[J].Acta Petrologica Sinica,24(6):1390-1400.
吴仕强,朱井泉,王国学,等.塔里木盆地寒武—奥陶系白云岩结构构造类型及其形成机理[J].岩石学报,2008,24(6):1390-1400.
[18]Hendry J P,Gregg J M,Shelton K L,et al.Origin,characteristics and distribution of fault-related and fracture-related dolomitization:Insights from Mississippian carbonates,Isle of Man[J].Sedimentology,2015,62(3):717-752.
[19]Sibley D F,Gregg J M.Classification of dolomite rock texture[J].Journal of Sedimentary Research,1987, 57(6):967-975.
[20]Warren J.Dolomite:occurrence,evolution and economically important associations[J].Earth-Science Reviews,2000,52(1-3):1-81.
[21]Ji Mingming,Zhao Junxing,Li Fengjie,et al.Diagenesis and pore evolution of carbonate rock in Ordovician Mawu5 submember,eastern Sulige area[J].Natrual Gas Exploration and Development,2013,36(4):12-16.
季明明,赵俊兴,李凤杰,等.苏东奥陶系马五5亚段碳酸盐岩成岩作用与孔隙演化[J].天然气勘探与开发,2013,36(4):12-16.
[22]Fan Ming.Mechanism of Carbonate Reservoir Pores-Geological and Experimental Research on Dissolution and Dolomitization[C].Qingdao:Symposium of the 4th National Sedimentary Congress,2009:181-182.
范明.碳酸盐岩储层孔隙形成机理—溶蚀与白云岩化作用实验地质学研究[C].青岛:第四届全国沉积学大会论文集,2009:181-182.
[23]Kong Jinxiang,Li Guorong.SY/T5478-2003 the Division of Diagenetic Stages in Carbonate Rocks[S].Beijing:Petroleum Industry Press,2003.
孔金详,李国蓉.SY/T5478-2003碳酸盐岩成岩阶段划分[S].北京:石油工业出版社,2003.

[1] Lü Zheng-xiang,Wang Xian-dong,Wu Jia-yang, Qing Yuan-hua. Diagenetic evolution characteristics of Paleogene lacustrinecarbonate reservoirs in the central Bohai Sea area [J]. Natural Gas Geoscience, 2018, 29(7): 921-931.
[2] Du Yang,Fan Tai-liang,Gao Zhi-qian. Geochemical characteristics and their implications to diagenetic environment of Lower-Middle Ordovician carbonate rocks,Tarim Basin,China:A case study of Bachu Dabantage outcrop and Aksu Penglaiba outcrop [J]. Natural Gas Geoscience, 2016, 27(8): 1509-1523.
[3] Zhao Guo-xiang,Wang Qing-bin,Yang Bo,Wang Xiao-gang,Bai Bing,Wan Lin. Dissolution mechanism analysis of Ordovician carbonates under burial environment of Bozhong Sag,Bohai Sea area [J]. Natural Gas Geoscience, 2016, 27(1): 111-120.
[4] LIU Jie,ZHANG Zhong-tao,LIU Dao-li,WANG Xiu-ling,XU Hui,YAN Hui. Development Characteristics of Limestone upon Sandstone Reservoir Identification by Pre-stack Simultaneous Inversion:Taking C16-Field in Pearl River Mouth Basin as an Example [J]. Natural Gas Geoscience, 2015, 26(4): 718-724.
[5] LI Da-qi,KANG Yi-li,YOU Li-jun. Experimental Study on Permeability Stress Sensitivity of Carbonate Rocks [J]. Natural Gas Geoscience, 2014, 25(3): 409-413.
[6] LI Ke-peng,CHEN Hong-han,FENG Yong. Characteristics of Homogenization Temperatures of Fluid Inclusions  and Application in Deeply Buried Carbonate Rocks [J]. Natural Gas Geoscience, 2012, 23(4): 756-763.
[7] YANG Hua, WANG Bao-Qing, SUN Liu-Yi, REN Jun-Feng, HUANG Zheng-Liang, WU Chun-Ying. Characteristics of Oxygen and Carbon Stable Isotopes for Middle Ordovician Majiagou Formation Carbonate Rocks in the Ordos Basin [J]. Natural Gas Geoscience, 2012, 23(4): 616-625.
[8] LI Da-Qi, KANG Yi-Li, ZHANG Hao. New Evaluation Method of Permeability Stress Sensitivity Based on Visual Fracture Aperture Measurement [J]. Natural Gas Geoscience, 2011, 22(3): 494-500.
[9] LI Zhen-Sheng, ZHANG Wen-Jun, WU Xiao-Qi, LIU De-Liang. Gas Source of Carbon Dioxide and Its Degassing Model in Songliao Basin [J]. Natural Gas Geoscience, 2011, 22(1): 29-37.
[10] TANG You-jun,WEN Zhi-gang,BIE Xu-wei. DISCUSSION OF THE PERSPECTIVE OF OIL EXPLORATION IN MIDDLE YANGTZE AREA FROM THE HYDROCARBON GENERATION OF MARINE CARBONATE ROCKS [J]. Natural Gas Geoscience, 2006, 17(4): 590-592.
[11] .
RESTORATION ON ORGANIC MATTER ABUNDANCE OF CARBONATE SOURCE ROCKS: A CASE OF MIDDLE-UPPER PROTERZOICCARBONATE ROCKS IN NORTH CHINA
[J]. Natural Gas Geoscience, 2004, 15(3): 306-310.
[12] . RESERVOIR EVALUATION MEASURE FOR CONDENSATED GAS RESERVOIR OF CARBONATE ROCKS IN QIANMIQIAO BURIED HILL [J]. Natural Gas Geoscience, 2003, 14(4): 267-270.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!