He Mingxi, Du Jianbo, Wang Rongxin, Guo Shangting, Yan Yongxin, Wu Minghui, Xie Qifeng, Li Fengxun. THE STUDY OF EXPLORATION PROSPECT OF MARINE NATURAL GAS IN THE NEOPROTEROZOIC-LOWER PALEOZOIC ON THE SOUTH MARGIN OF THE NORTH CHINA PLATFORM[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(2): 154-159. doi: 10.11781/sysydz200902154
Citation: He Mingxi, Du Jianbo, Wang Rongxin, Guo Shangting, Yan Yongxin, Wu Minghui, Xie Qifeng, Li Fengxun. THE STUDY OF EXPLORATION PROSPECT OF MARINE NATURAL GAS IN THE NEOPROTEROZOIC-LOWER PALEOZOIC ON THE SOUTH MARGIN OF THE NORTH CHINA PLATFORM[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(2): 154-159. doi: 10.11781/sysydz200902154

THE STUDY OF EXPLORATION PROSPECT OF MARINE NATURAL GAS IN THE NEOPROTEROZOIC-LOWER PALEOZOIC ON THE SOUTH MARGIN OF THE NORTH CHINA PLATFORM

doi: 10.11781/sysydz200902154
  • Received Date: 2008-12-12
  • Rev Recd Date: 2009-03-02
  • Publish Date: 2009-04-28
  • According to the field investigation results on the northern edge of the Qingling-Dabie Orogenic Belt,it was showed that the black mudstone and shale containing phosphor in the Lower Cambrian Yutaishan/Dongpo formation on the south margin of the North China Platform was the high quality source rocks,and the dark grey shale in Cuizhuang/Liulaobei formation of the Qingbaikou System was the potential source rocks.The Neoproterozoic-Lower Paleozoic sandstones and dolomites were the main reservoirs,with favorable pore space developed on several karst erosional surfaces internal the Neoproterozoic-Lower Paleozoic sequences.And the shale and the carbonate rocks with gypsum in the Neoproterozoic-Lower Paleozoic were the cap rocks.There were basic conditions for hydrocarbon ge-neration and accumulation although the thermal maturity was higher in the area.Therefore,it is probably the new formation and new domain for exploration of the marine natural gas in the Neoproterozoic-Lower Paleozoic on the south margin of the North China Platform.

     

  • loading
  • [1]
    戴金星,刘德良,曹高社.华北陆块南部下寒武统海相泥质烃源岩的发现对天然气勘探的意义[J].地质论评,2003,49(3):322~329
    [2]
    戴金星.华北盆地南缘寒武系烃源岩[M].北京:石油工业出版社,2005
    [3]
    河南省地质矿产局.河南省区域地质志[M].北京:地质出版社,1989
    [4]
    安徽省地质矿产局.安徽省区域地质志[M].北京:地质出版社,1989
    [5]
    汪啸风,陈孝红.中国各时代地层划分与对比[M].北京:地质出版社,2005
    [6]
    秦建中,刘宝泉,国建英等.关于碳酸盐烃源岩的评价标准[J].石油实验地质,2004.26(3):281~285
    [7]
    陈安定.海相"有效烃源岩"定义及丰度下限问题讨论[J].石油勘探与开发,2005,32(2):23~25
    [8]
    秦建中,刘宝泉,郑伦举等.海相碳酸盐岩排烃下限值研究[J].石油实验地质,2007,29(4):391~396
    [9]
    陈践发,张水昌,孙省利等.海相碳酸盐岩优质烃源岩发育的主要影响因素[J].地质学报,2006,80(3):467~472
    [10]
    郝石生,王飞宇,高岗等.下古生界高过成熟烃源岩特征和评价[J].勘探家,1996,1(2):25~32
    [11]
    张渝昌.中国含油气盆地原型分析[M].南京:南京大学出版社,1997.333~355
    [12]
    熊永强,耿安松,张海祖等.油型气的形成机理及其源岩生烃潜力恢复[J].天然气工业,2004,24(2):11~13
    [13]
    王传刚,胡宗全,许化政等.叠合盆地老烃源岩系油气勘探前景评价方法[J].石油学报,2008,29(1):10~22
    [14]
    刘小平,孙冬胜,吴欣松.古岩溶地貌及其对岩溶储层的控制[J].石油实验地质,2007,29(3):265~268
    [15]
    付晓飞,宋岩,吕延防等.塔里木盆地库车坳陷膏盐质盖层特征与天然气保存[J].石油实验地质,2006,28(1):25~29
  • 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 (1521) PDF downloads(961) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return