Jiang Xia, Zhou Liqing. CHARACTERISTICS OF FORMATION AND DISTRIBUTION OF PROLIFIC SAGS IN THE NORTHERN JIANGSU BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(4): 319-325. doi: 10.11781/sysydz201004319
Citation: Jiang Xia, Zhou Liqing. CHARACTERISTICS OF FORMATION AND DISTRIBUTION OF PROLIFIC SAGS IN THE NORTHERN JIANGSU BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(4): 319-325. doi: 10.11781/sysydz201004319

CHARACTERISTICS OF FORMATION AND DISTRIBUTION OF PROLIFIC SAGS IN THE NORTHERN JIANGSU BASIN

doi: 10.11781/sysydz201004319
  • Received Date: 2010-04-28
  • Rev Recd Date: 2010-06-21
  • Publish Date: 2010-08-28
  • The oil-and-gas fields discovered so far in the Northern Jiangsu Basin mainly distribute in the Gaoyou,Jinhu and Qintong prolific sags locating in the Dongtai Depression which is in the south of the basin.The formation conditions are as follows: 1) During the migration of subsidence center from west to east in the basin,the sustainable and rapid subsidence type of sags such as Jinhu,Gaoyou and Qintong are created with thick source rocks,premium quality organics and high degree of thermal evolution;2) In the west part of Jinhu and Gaoyou sags which locate in the entrance area of big rivers to lakes in the west of the basin,the favorable Funing Formation reservoir facies belt corresponding to Fu2 Formation premium source rocks is generated.While in the east part of Qintong and Gaoyou sags which locate in the center of the basin,in addition to many favorable combinations of source-reservoir-seal rocks formed with primary oil and gas in the lower part,the vertical migration of oil and gas is fairly dynamic,and the upper secondary oil-and-gas pools have conducive reservoir-forming conditions;3) In the resi-dual depression area of the Wubao movement,namely the Gaoyou,Jinhu and Qintong sags,source rocks are buried with great depth,resulting in high degree of thermal evolution,rich abundance of oil and gas,and good development of secondary oil and gas reservoirs;4) In the central and west sags such as Jinhu,Gaoyou and Qintong,sedimentary volcanism is significant for major hydrocarbon source rocks of Fu2 Formation.Surface thermal environment and abundant inorganic nutrients help grow rich lower hydrobiont in this area and develope premium hydrocarbon source rocks.Meanwhile,magmatism stages for the 3 sags are 3-4,with high geothermal gradient,which is conducive to high degree of thermal evolution and conversion yield.

     

  • loading
  • [1]
    张渝昌,卫自立.苏北—南黄海盆地[G]/朱夏.中国含油气盆地.北京:人民出版社,1989:100-123.
    [2]
    周荔青,刘池阳.深大断裂与中国东部新生代盆地油气资源分布[M].北京:石油工业出版社,2006.
    [3]
    马立桥,陈汉林,董庸,等.苏北—南黄海南部叠合盆地构造演化与海相油气勘探潜力[J].石油与天然气地质,2007,28(1):35-42.
    [4]
    吴向阳,夏连军,陈晶.苏北盆地高邮凹陷构造再认识及对油气勘探的意义[J].石油实验地质,2009,31(6):570-575.
    [5]
    刘玉瑞,刘启东,杨小兰.苏北盆地走滑断层特征与油气聚集关系[J].石油与天然气地质,2004,25(3):279-283.
    [6]
    张国栋,王慧中.中国东部早第三纪海侵和沉积环境:以苏北盆地为例[M].北京:地质出版社,1987.
    [7]
    任红民,陈丽琼.苏北盆地晚白垩世泰州期原型盆地恢复[J].石油实验地质,2008,30(1):52-57.
    [8]
    周荔青,吴聿元.苏北盆地浅层油气藏类型及分布特征[J].石油实验地质,2007,29(4):334-339.
    [9]
    李贤庆,包建平,王文军.苏北盆地下第三系烃源岩热演化研究[J].石油实验地质,1996,18(1):96-105.
    [10]
    陈安定.苏北盆地第三系烃源岩排烃范围及油气运移边界[J].石油与天然气地质,2006,27(5):630-636.
  • 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 (1968) PDF downloads(1295) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return