Advanced Search
Volume 35 Issue 4
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2013  >  35(4): 378-383
Ma Haiyong, Zhou Lifa, Zhang Xiaogang, Han Tianyou, Li Jihong, Liu Guanglin. Diagenesis and favorable diagenetic facies of Chang8 reservoir in Jiyuan area of Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(4): 378-383. doi: 10.11781/sysydz201304378
Citation: Ma Haiyong, Zhou Lifa, Zhang Xiaogang, Han Tianyou, Li Jihong, Liu Guanglin. Diagenesis and favorable diagenetic facies of Chang8 reservoir in Jiyuan area of Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(4): 378-383. doi: 10.11781/sysydz201304378
shu

Diagenesis and favorable diagenetic facies of Chang8 reservoir in Jiyuan area of Ordos Basin

doi: 10.11781/sysydz201304378
  • 1.

    Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China

  • 2. Exploration and Development Research Institution/National Engineering Laboratory for Exploration and Development of Low-Permeability Oil & Gas Fields, Changqing Oilfield Company, Xi'an, Shaanxi 710018, China

  • 3. Exploration Department, Changqing Oilfield Company, Xi'an, Shaanxi 710018, China

  • Received Date: 2012-11-11
  • Rev Recd Date: 2013-06-04
  • Publish Date: 2013-07-28
    Abstract
  • The diagenesis and favorable diagenetic facies of Chang8 reservoir in Jiyuan area of the Ordos Basin were studied by means of cast thin section, SEM and reservoir comprehensive evaluation. The Chang8 sandstones were during the subphase A of late diagenesis. Compaction effect caused the disappearance of primary pores. Influenced by acidic diagenetic environment, feldspars were corroded, improving pore connectivity and permeability. In the well-developed chlorite film which generated during early stage, a large quantity of primary pores was preserved, showing good reservoir physical property. According to diagenetic and sedimentary features, 4 diagenetic facies belts were classified. The diagenetic facies belts of feldspar corrosion and chlorite film-intergranular pore were most favorable, mainly distributing in sandbody zones in subaqueous distributary channel of delta front in Liumaoyuan and Baoziwan areas, and in distributary channel of delta in Xiaojianzi area.

     

    • FullText(HTML)
  • loading
    • References(37)
  • [1]
    何自新.鄂尔多斯盆地演化与油气[M].北京:石油工业出版社,2003.
    [2]
    陈朝兵,朱玉双,谢辉,等.姬塬油田红井子地区延长组长9油层组石油富集规律[J].石油与天然气地质,2012,33(5):758-765.
    [3]
    胡作维,黄思静,马永坤,等.鄂尔多斯盆地姬塬地区长2油层组储层孔隙结构特征[J].断块油气田,2012,19(5):588-591.
    [4]
    郑荣才,牛小兵,梁晓伟,等.鄂尔多斯盆地姬塬油田延长组原油性质与来源分析[J].地球科学与环境学报,2011,33(2):142-145.
    [5]
    唐俊,王琪,马晓峰,等.Q型聚类分析和判别分析法在储层评价中的应用:以鄂尔多斯盆地姬塬地区长81储层为例[J].特种油气藏,2012,19(6):28-31
    [6]
    张文正,杨华,李剑锋,等.论鄂尔多斯盆地长7段优质烃源岩在低渗透油气成藏富集中的主导作用:强生排烃特征及机理分析[J].石油勘探与开发,2006,33(3):289-293.
    [7]
    肖晖,吴小斌,何丹,等.鄂尔多斯盆地镇川地区长3低渗储层特征及其控制因素[J].断块油气田,2011,18(6):701-704.
    [8]
    侯瑞云,刘忠群.鄂尔多斯盆地大牛地气田致密低渗储层评价与开发对策[J].石油与天然气地质,2012,33(1):118-128.
    [9]
    白玉彬,张乾.鄂尔多斯盆地定边油田长2低渗砂岩储层特征及评价[J].特种油气藏,2011,18(5):56-59.
    [10]
    李荣西,段立志,张少妮,等.鄂尔多斯盆地低渗透油气藏形成研究现状与展望[J].地球科学与环境学报,2011,33(4):364-372.
    [11]
    罗顺社,银晓.鄂尔多斯盆地姬塬地区延长组长 8 沉积相的研究[J].石油天然气学报,2008,30(4):5-9.
    [12]
    聂永生,田景春,夏青松.鄂尔多斯盆地白豹—姬塬地区上三叠统延长组物源分析[J].油气地质与采收率,2004,11(5):4-7.
    [13]
    王纹婷,郑荣才,王成玉,等.鄂尔多斯盆地姬塬地区长8油层组物源分析[J].岩性油气藏,2009,21(4):41-46.
    [14]
    韩永林,王成玉,王海红,等.姬塬地区长8油层组浅水三角洲沉积特征[J].沉积学报,2009,27(6):1057-1064.
    [15]
    李元昊,刘池洋,独育国,等.鄂尔多斯盆地西北部上三叠统延长组长8油层组浅水三角洲沉积特征及湖岸线控砂[J].古地理学报,2009,11(3):265-274.
    [16]
    银晓,罗顺社,李鑫,等.鄂尔多斯盆地姬塬地区延长组长8时期物源分析[J].岩性油气藏,2008,20(3):59-63.
    [17]
    罗静兰,刘小洪,林潼,等.成岩作用与油气侵位对鄂尔多斯盆地延长组砂岩储层物性的影响[J].地质学报,2006,80(5):664-673.
    [18]
    杨希濮,孙卫.鄂尔多斯盆地低渗透油藏孔隙结构特征及影响因素分析[J].特种油气藏,2011,18(6):44-47.
    [19]
    薛永超,程林松.靖安油田长4+5油藏储集空间及成岩作用演化[J].特种油气藏,2011,18(5):25-28.
    [20]
    黄思静,黄培培,王庆东,等.胶结作用在深埋藏砂岩孔隙保存中的意义[J].岩性油气藏,2007,19(3):7-13.
    [21]
    思玉琥,郝世彦, 张林森, 等.延安地区上三叠统长6期储层成岩作用及孔隙演化[J].特种油气藏,2011,18(6):36-39.
    [22]
    柳益群,李文厚.陕甘宁盆地上三叠统含油长石砂岩的成岩特点及孔隙演化[J].沉积学报,1996,14(3):87-96.
    [23]
    罗静兰,张晓莉,张云翔,等.成岩作用对河流—三角洲相砂岩储层物性演化的影响:以延长油区上三叠统延长组长2砂岩为例[J].沉积学报,2001,19(4):541-547.
    [24]
    刘小洪,罗静兰,郭彦如,等.鄂尔多斯盆地陕北地区上三叠统延长组长6油层组的成岩相与储层分布[J].地质通报,2008,27(5):626-632.
    [25]
    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.
    [26]
    郑荣才,耿威,周刚,等.鄂尔多斯盆地白豹地区长6砂岩成岩作用与成岩相研究[J].岩性油气藏,2007,19(2):1-8.
    [27]
    Surdam R C,Jiao Z S,MacGowen D B.Redox rreaction involving hydrocarbons and mineral oxidants:A mechanism for significant porosity enhancement in sandstones[J].AAPG Bulletin,1993,77(9):1509-1518.
    [28]
    张磊,龚福华,任瑞清,等.鄂尔多斯盆地胡尖山—王洼子地区长4+5储层成岩作用及成岩相研究[J].特种油气藏,2009,16(5):40-47.
    [29]
    刘宝珺,张锦泉.沉积成岩作用[M].北京:科学出版社,1992:65-92.
    [30]
    裘怿楠,薛叔浩.油气储层评价技术[M].北京:石油工业出版社,1994:59-64,290.
    [31]
    邹才能,陶士振,薛叔浩."相控论"的内涵及其勘探意义[J].石油勘探与开发,2005,32(6):7-12.
    [32]
    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.
    [33]
    成志刚,宋子齐,景成,等.苏里格东区致密气储层成岩储集相分类及特征[J].断块油气田,2012,19(5):577-582.
    [34]
    张伟,刘建朝,高志亮,等.鄂尔多斯盆地吴堡地区长6段浊积特征及其石油地质意义[J].地球科学与环境学报,2012,34(2):64-71.
    [35]
    杜业波,季汉成,吴因业,等.前陆层序致密储层的单因素成岩相分析[J].石油学报,2006,27(2):48-52.
    [36]
    Hillier S.Pore-lining chlorites in siliciclastic reservoir sandstones: Electron microprobe, SEM and XRD data,and implications for their rigin[J].Clay Minerals,1994,29(4):665-679.
    [37]
    王琪,禚喜准,陈国俊,等.鄂尔多斯西部长6砂岩成岩演化与优质储层[J].石油学报,2005,26(5):17-23.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (1572) PDF downloads(860) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return