Liu Xiaoping, Sun Dongsheng, Wu Xinsong. ORDOVICIAN PALAEOKARST LANDFORM AND ITS CONTROL ON RESERVOIRS IN WEST LUNGU REGION, THE TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(3): 265-268. doi: 10.11781/sysydz200703265
Citation: Liu Xiaoping, Sun Dongsheng, Wu Xinsong. ORDOVICIAN PALAEOKARST LANDFORM AND ITS CONTROL ON RESERVOIRS IN WEST LUNGU REGION, THE TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(3): 265-268. doi: 10.11781/sysydz200703265

ORDOVICIAN PALAEOKARST LANDFORM AND ITS CONTROL ON RESERVOIRS IN WEST LUNGU REGION, THE TARIM BASIN

doi: 10.11781/sysydz200703265
  • Received Date: 2006-10-30
  • Rev Recd Date: 2007-04-01
  • Publish Date: 2007-05-28
  • Karst landform is the result of the compositive process of karst and various geology.And various shapes of karst landforms also control the karst reservoir development.The palaeokarst landform in west Lungu region was restored by using seismic horizon flattening technique.The results show that the surface of the karst is undulate greatly,and develops the landform combination of peak cluster depression,peak forest valley and peak forest plain from east to west.The vertical karst facies belts in different landform was divided according to the data of well logging,drilling and geological log.Then,the development characteristics of reservoirs in different landforms are discussed.Research results indicate that the great differences of cavern development and filling status exist among various palaeokarst landforms and karst facies belts,which reflect that the palaeokarst landforms control the spatial development of karst facies belt and reservoirs.

     

  • loading
  • [1]
    陈学时,易万霞,卢文忠.中国油气田古岩溶与油气储层[J].沉积学报,2004,22(2):244~253
    [2]
    顾忆.塔里木盆地北部塔河油田油气藏成藏机制[J].石油实验地质,2002,22(4):307~312
    [3]
    周玉琦,黎玉战,侯鸿斌.塔里木盆地塔河油田的勘探实践与认识[J].石油实验地质,2001,23(4):363~367
    [4]
    夏日元,唐健生,关碧珠等.鄂尔多斯盆地奥陶系古岩溶地貌及天然气富集特征[J].石油与天然气地质,1999,20(2):133~136
    [5]
    肖玉茹,何峰煜,孙义梅.古洞穴型碳酸盐岩储层特征研究:以塔河油田奥陶系古洞穴为例[J].石油与天然气地质,2003,24(1):75~86
    [6]
    王敦则,黎玉战,俞仁连.塔里木盆地塔河油田下奥陶统油藏特征及成藏条件分析[J].石油实验地质,2003,25(2):122~128
    [7]
    闫相宾.塔河油田奥陶系碳酸盐岩储层特征[J].石油与天然气地质,2002,23(3):262~265
    [8]
    刘金荣,黄国彬,黄学灵等.广西区域热带岩溶地貌不同类型的演化浅议[J].中国岩溶,2001,20(1):247~258
    [9]
    杨景春,李有利.地貌学原理[M].北京:北京大学出版社,2005.1~246
    [10]
    任美锷,刘振中.岩溶学概论[M].北京:商务印书馆,1983.1~331
    [11]
    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):202~207
    [12]
    顾家裕,周兴熙.塔里木盆地轮南潜山岩溶及油气分布规律[M].北京:石油工业出版社,2001.1~268
    [13]
    王良俊,李桂卿.塔河油田奥陶系岩溶地貌形成机制[J].新疆石油地质,2001,22(6):480~482
  • 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 (640) PDF downloads(334) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return