Zhou Jiangyu, Lü Haitao, Lin Zhongmin, Wu Chonglong. KARSTIFICATION MODELS OF THE ORDOVICIAN CARBONATES AND THEIR INFLUETIAL FACTORS IN THE TAHE OILFIELD, THE TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(6): 547-550. doi: 10.11781/sysydz200906547
Citation: Zhou Jiangyu, Lü Haitao, Lin Zhongmin, Wu Chonglong. KARSTIFICATION MODELS OF THE ORDOVICIAN CARBONATES AND THEIR INFLUETIAL FACTORS IN THE TAHE OILFIELD, THE TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(6): 547-550. doi: 10.11781/sysydz200906547

KARSTIFICATION MODELS OF THE ORDOVICIAN CARBONATES AND THEIR INFLUETIAL FACTORS IN THE TAHE OILFIELD, THE TARIM BASIN

doi: 10.11781/sysydz200906547
  • Received Date: 2009-06-05
  • Rev Recd Date: 2009-11-08
  • Publish Date: 2009-12-28
  • Karstification research of a complicated anisotrophic carbonate reservoir is presently an important leading field for reservoir sedimenology and geochemistry.Akekule convex included Tahe Oilfield is a long-term developed paleo-uplift based on the pre-Sinian metamorphic basement,which affected by multi-period of Caledonian and Hercynian tectonic uplift and sea-level changes,and superposing reformed by late tectonic movement.A set of Cambrian-Ordovician carbonate karst-fracture-hole reservoirs were developed in Akekule convex.Combined with the karstification and exploration in Tahe Oilfield,three karstification models were established in the area and the key controling factors of karst development were analyzed.

     

  • loading
  • [1]
    康玉柱.塔里木盆地古生代海相碳酸盐岩储集岩特征[J].石油实验地质,2007,29(3):217-223
    [2]
    杨宁,吕修祥.塔里木盆地轮南、塔河油田碳酸盐岩储层特征研究——以沙107井和轮古40井为例[J].石油实验地质,2008,30(3):247-251
    [3]
    金强,王端平.潜山型碳酸盐岩储集空间成因模式[J].油气地质与采收率,2003,10(5):12-15
    [4]
    饶丹,马绪杰.塔河油田主体区奥陶系缝洞系统与油气分布[J].石油实验地质,2007,29(6):589-592
    [5]
    宋美虹.塔河油田4区奥陶系碳酸盐岩潜山油藏储层预测[J].油气地质与采收率,2005,12(4):23-25
    [6]
    刘小平,孙冬胜,吴欣松.古岩溶地貌及其对岩溶储层的控制——以塔里木盆地轮古西地区奥陶系为例[J].石油实验地质,2007,29(3):265-268
    [7]
    顾乔元,潘文庆.轮南地区奥陶系油气成藏特征[J].新疆石油地质,1999,20(3):210-212
    [8]
    吕修祥,杨宁,解启来等.塔中地区深部流体对碳酸盐岩储层的改造作用[J].石油与天然气地质,2005,26(3):284-289,296
    [9]
    刘显风,蔡忠贤,云露等.塔河油田岩溶作用元素地球化学的特征响应[J].石油实验地质,2009,31(3):270-274
    [10]
    林忠民.塔河油田奥陶系碳酸盐岩储层特征及成藏条件[J].石油学报,2002,23(3):23-27
    [11]
    康志江,李江龙,张冬丽等.塔河缝洞型碳酸盐岩油藏渗流特征[J].石油与天然气地质,2005,26(5):634-640,673
    [12]
    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
    [13]
    Mazzullo S J,Harris P M.Mesogenetic dissolution:Its role in porosity development in carbonate reservoirs[J].AAPG Bulletin,1992,76(5):607-620
    [14]
    Carles K.Karst-controlled reservoir heterogeneity in Ellenburger group carbonates of West Taxes[J].AAPG Bulletin,1988,72 (10):1160-1183
    [15]
    Cao H,Yang J,Wang D.Paleokarsts in late Precambrian and Ordovician carbonates,Kepin-Shaya uplift zone,Tarim basin,China[J].Carbonates Evaporites,1999,14(2):200-208
    [16]
    阎相宾.塔河油田下奥陶统古岩溶作用及储层特征[J].江汉石油学院学报,2002,24(4):23-25
    [17]
    张涛,闫相宾.塔里木盆地深层碳酸盐岩储层主控因素探讨[J].石油与天然气地质,2007,28(6):745-754
    [18]
    闫相宾,李铁军,张涛等.塔中与塔河地区奥陶系岩溶储层形成条件的差异[J].石油与天然气地质,2005,26(2):201-207
    [19]
    刘忠宝,于柄松,李廷艳等.塔里木盆地塔中地区中上奥陶统碳酸盐岩层序发育对同生期岩溶作用的控制[J].沉积学报,2004,22(1):103-109
  • 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

    Article Metrics

    Article views (1759) PDF downloads(1183) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return