Advanced Search
Volume 32 Issue 5
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2010  >  32(5): 434-441
Ma Hongqiang, Wang Shuyi, Yong Hong, Chen Qianglu, Jiang Haijian, Wang Bin, Li Huili, Sha Xuguang. BURIAL KARST CHARACTERISTICS OF ORDOVICIAN CARBONATE RESERVOIRS IN CENTRAL TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(5): 434-441. doi: 10.11781/sysydz201005434
Citation: Ma Hongqiang, Wang Shuyi, Yong Hong, Chen Qianglu, Jiang Haijian, Wang Bin, Li Huili, Sha Xuguang. BURIAL KARST CHARACTERISTICS OF ORDOVICIAN CARBONATE RESERVOIRS IN CENTRAL TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(5): 434-441. doi: 10.11781/sysydz201005434
shu

BURIAL KARST CHARACTERISTICS OF ORDOVICIAN CARBONATE RESERVOIRS IN CENTRAL TARIM BASIN

doi: 10.11781/sysydz201005434
  • 1.

    Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

  • 2. CNPC International Department, Beijing 100007, China

  • 3. SINOPEC Exploration and Production Research Institute, Beijing 100083, China

  • 4. Research Institute of Petroleum Exploration and Production, Northwest Branch, SINOPEC, Urumqi, Xinjiang 830011, China

  • Received Date: 2010-02-23
  • Rev Recd Date: 2010-08-05
  • Publish Date: 2010-10-28
    Abstract
  • Various types of karstification effects have developed in the Ordovician carbonate reservoirs of the central Tarim Basin.The deep burial and hydrothermal Karstification effects play important roles in favorable reservoir formation.Analyses of well cores,logging data and geological background have indicated that,there are mainly 4 stages of burial Karstification effects in the area.The pores in stages Ⅰ and Ⅱ have been filled.The residual pores in stage Ⅲ and the corrosion pores in stage Ⅳ work as effective reservoir space for present reservoirs.The main fluid medium include organic acid and CO2 generated during organic evolution.H2S may contribute to late reservoir formation.Hydrothermal Karstification is effective to Ordovician reservoir transformation.The influence and evaluation still require further research.

     

    • FullText(HTML)
  • loading
    • References(36)
  • [1]
    叶德胜,王恕一,张希明,等.新疆塔里木盆地北部储层沉积、成岩特征及储层评价[M].成都:成都科技大学出版社,1995.
    [2]
    陈景山,李忠,王振宇,等.塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布[J].沉积学报,2007,25(6):858-868.
    [3]
    钱一雄,陈跃,陈强路,等.塔中西北部奥陶系碳酸盐岩埋藏溶蚀作用[J].石油学报,2006,27(3):47-52.
    [4]
    钱一雄,TABERNER C,邹森林,等.碳酸盐岩表生岩溶与埋藏溶蚀比较:以塔北和塔中地区为例[J].海相油气地质,2007,12(2):1-7.
    [5]
    钱一雄,邹远荣,陈强路,等.塔里木盆地塔中西北部多期、多成因岩溶作用地质-地球化学表征:以中1井为例[J].沉积学报,2005,23(4):596-602.
    [6]
    朱东亚,胡文,张学丰,等.塔河油田奥陶系灰岩埋藏溶蚀作用特征[J].石油学报,2007,28(5):57-62.
    [7]
    郑和荣,刘春燕,吴茂炳,等.塔里木盆地奥陶系颗粒石灰岩埋藏溶蚀作用[J].石油学报,2009,30(1):9-15.
    [8]
    陈强路,周凌方,张根法,等.塔里木盆地巴楚-麦盖提地区油气勘探领域评价[J].石油实验地质,2009,31(4):343-349.
    [9]
    陈强路,何治亮,李思田.塔中地区奥陶系碳酸盐岩储层与油气聚集带[J].石油实验地质,2007,29(4):367-372.
    [10]
    克莱德 H 莫尔.碳酸盐岩储层:层序地层格架中的成岩作用和孔隙演化[M].姚根顺,沈安江,潘文庆,等译.北京:石油工业出版社,2007:265-270.
    [11]
    范明,胡凯,蒋小琼,等.酸性流体对碳酸盐岩储层的改造作用[J].地球化学,2009,38(1):20-26.
    [12]
    范明,蒋小琼,刘伟新,等.不同温度条件下CO2水溶液对碳酸盐岩的溶蚀作用[J].沉积学报,2007,25(6):825-830.
    [13]
    蒋小琼,王恕一,范明,等.埋藏成岩环境碳酸盐岩溶蚀作用模拟实验研究[J].石油实验地质,2008,30(6):643-646.
    [14]
    朱光有,张水昌,马永生,等.TSR(H2S)对石油天然气工业的积极性研究:H2S的形成过程促进储层次生孔隙的发育[J].地学前缘,2006,13(3):141-149.
    [15]
    曾伟,黄先平,杨雨,等.川东北地区飞仙关组储层中的埋藏溶蚀作用[J].天然气工业,2006,26(11):4-7.
    [16]
    马永生,郭彤楼,赵雪凤,等.普光气田深部优质白云岩储层形成机制[J].中国科学(D辑:地球科学),2007,(S2):43-52.
    [17]
    马永生,郭彤楼,朱光有,等.硫化氢对碳酸盐储层溶蚀改造作用的模拟实验证据:以川东飞仙关组为例[J].科学通报,2007,52(S1):136-141.
    [18]
    赵雪凤,朱光有,张水昌,等.川东北普光地区与塔中地区深部礁滩体优质储层的对比研究[J].沉积学报,2009,27(3):390-403.
    [19]
    张建勇,刘文汇,范明,等.TSR产物对碳酸盐岩储层是否具有改良作用:实验地质学的依据[J].海相油气地质,2008,13(2):57-61.
    [20]
    黄思静,QING HAIRUO,胡作维,等.四川盆地东北部三叠系飞仙关组硫酸盐还原作用对碳酸盐成岩作用的影响[J].沉积学报,2007,25(6):815-914.
    [21]
    韩剑发,梅廉夫,杨海军,等.塔里木盆地塔中奥陶系天然气的非烃成因及其成藏意义[J].地学前缘,2009,16(1):314-325.
    [22]
    蔡春芳,邬光辉,李开开,等.塔中地区古生界热化学硫酸盐还原作用与原油中硫的成因[J].矿物岩石地球化学通报,2007,26(1):44-48.
    [23]
    陈利新,杨海军,邬光辉,等.塔中Ⅰ号坡折带奥陶系礁滩体油气藏的成藏特点[J].新疆石油地质,2008,29(3):327-330.
    [24]
    张兴阳,顾家裕,罗平,等.塔里木盆地奥陶系萤石成因及其油气地质意义[J].岩石学报,2006,22(8):2220-2247.
    [25]
    张兴阳,顾家裕,罗平.TZ45井萤石成因与油气成藏[J].新疆石油地质,2004,25(5):479-482.
    [26]
    王嗣敏,吕修祥.塔中地区奥陶系碳酸盐岩储层特征及其油气意义[J].西安石油大学学报(自然科学版),2004,19(4):72-77.
    [27]
    王嗣敏,金之钧,解启来.塔里木盆地塔中井区碳酸盐岩储层的深部流体改造作用[J].地质论评,2004,50(5):543-546.
    [28]
    赵霞.塔里木盆地TZ45 井及柯坪西克尔萤石成因的讨论[J].西北地质,2000,33(3):5-8.
    [29]
    金之钧,朱东亚,胡文瑄,等.塔里木盆地热液活动地质地球化学特征及其对储层影响[J].地质学报,2006,80(2):245-254.
    [30]
    朱东亚,胡文瑄,宋玉才,等.塔里木盆地TZ45 井油藏萤石化特征及其对储层的影响[J].石油学报,2005,24(3):205-215.
    [31]
    林青,王培荣,金晓辉,等.塔中北斜坡TZ45井奥陶系油藏成藏史浅析[J].石油勘探与开发,2002,29(3):5-7.
    [32]
    钟广法,马在田,刘瑞林,等.塔里木盆地奥陶系萤石脉-油气叠合成藏作用:高分辨率成像测井资料提供的证据[J].高校地质学报,2000,6(4):576-582.
    [33]
    潘文庆,刘永福,DICKSON J A D,等.塔里木盆地下古生界碳酸盐岩热液岩溶的特征及地质模型[J].沉积学报,2009,27(5):983-992.
    [34]
    朱毅秀,金之钧,林畅松,等.塔里木盆地塔中地区早二叠世岩浆岩及油气成藏关系[J].石油实验地质,2005,27(1):50-54.
    [35]
    康玉柱.新疆两大盆地石炭-二叠系火山岩特征与油气[J].石油实验地质,2008,30(4):321-327.
    [36]
    吕修祥,解启来,杨宁,等.塔里木盆地深部流体改造型碳酸盐岩油气聚集[J].科学通报,2007,52(S):142-148.
    • 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 (2172) PDF downloads(1000) 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