西南石油大学学报(自然科学版) ›› 2013, Vol. 35 ›› Issue (2): 23-28.

• 地质勘探 • 上一篇    下一篇

卡塔尔鲁卜哈利盆地古生界生储盖组合特征

范春花,胡孝林,黄兴文,白海强,尹君   

  1. 中海油研究总院,北京东城100027
  • 收稿日期:1900-01-01 修回日期:1900-01-01 出版日期:2013-04-01 发布日期:2013-04-01

Source-reservoir-cap Assemblages in Paleozoic of the Rub al KhaliBasin,Qatar

Fan Chunhua, Hu Xiaolin, Huang Xingwen, Bai Haiqiang, Yin Jun   

  1. CNOOC Research Institute,Dongcheng,Beijing 100027,China
  • Received:1900-01-01 Revised:1900-01-01 Online:2013-04-01 Published:2013-04-01

摘要: 卡塔尔鲁卜哈利盆地古生界碎屑岩是油气勘探的新领域,在区域地质研究的基础上,利用石油地质学、储层
地质学等理论对古生界的生储盖组合进行研究,并重点分析了盖层发育特征。研究结果表明,卡塔尔鲁卜哈利盆地古
生界发育良好的生储盖组合,志留系Qusaiba 热页岩是主力烃源岩,泥盆系Jauf 组滨岸相砂岩和二叠系Unayzah 组河
流—三角洲相砂岩是主要储层,二叠系Khuff 组膏岩及底部的海侵泥岩为区域盖层,同时还发育多套局部盖层。盖层
的封盖能力是古生界油气勘探的主要风险之一,区域盖层横向分布稳定,且含膏岩,封盖性好,但局部盖层厚度较薄并
且泥岩质不纯,夹薄层白云质泥岩和少量粉砂岩,对封盖能力影响较大,盖层风险不容忽视。

关键词: 生储盖组合, 碎屑岩, 古生界, 鲁卜哈利盆地, 卡塔尔

Abstract: Clastic rock in Paleozoic is a new field for the petroleum exploration in the Rub al Khali Basin,Qatar. Based on
the regional geology study,the source-reservoir-cap assemblage in Paleozoic,especially the development characteristic of cap
rocks,is studied using petroleum geology and reservoir geology theory. The results show that the Palaeozoic group in the Rub
al Khali Basin is well-developed source-reservoir-cap assemblage. The Qusaiba hot shales in Silurian are the major source
rocks. The littoral sandstones of Jauf in Devonian and fluvial-deltaic sandstones of Unayzah in Permian are major reservoirs.
The Gypsum rocks and basal transgressive mudstones of Khuff are the regional cap rocks,with several sets of local cap rocks.
The seal abilities of cap rocks is one of the main risks for the Paleozoic petroleum exploration in this region. The distribution
of the regional cap rocks are stable on plane,which contains gypsum rocks. The seal ability is good as a whole,but local cap
rocks with minor dolomites and a few of siltstone are thin and impurity,which have an adverse effect on sealing abilities. The
cap risks should be taken in consideration in petroleum exploration.

Key words: source-reservoir-cap assemblages, clastic rocks, Paleozoic, the Rub al Khali Basin, Qatar