石油与天然气地质 ›› 2002, Vol. 23 ›› Issue (2): 179-182.doi: 10.11743/ogg20020217

• 油气空间 • 上一篇    下一篇

轮南-巴楚地区奥陶系生物礁储层特征

胡明毅1,2, 朱忠德2, 贺萍2, 张俊1, 王青春2   

  1. 1. 中国地质大学, 北京, 100083;
    2. 江汉石油学院地质系, 湖北荆州, 434023
  • 收稿日期:2002-03-10 出版日期:2002-06-25 发布日期:2012-01-16

ORDOVICION REEF IN LUNAN-BACHU AREA AND THEIR RESERVOIR CHARACTERISTICS

Hu Minyi1,2, Zhu Zhongde2, He Ping2, Zhang Jun1, Wang Qingchun 2   

  1. 1. China University of Geosciences, Beijing;
    2. Jianghan Petroleum University, Jingzhou, Hubei
  • Received:2002-03-10 Online:2002-06-25 Published:2012-01-16

PDF (PC)

671

被引次数

36

摘要：

塔里木盆地轮南巴楚地区奥陶系生物礁赋存于中奥陶统一间房组和上奥陶统桑塔木组,主要造礁生物为瓶筐石,其次为海绵类、苔藓虫类和有柄棘皮动物类。礁体规模较小,形态多样,礁体一般由礁基、礁核和礁盖三部分组成。含礁层系储层物性总体比较差,以低孔低渗或低孔中渗为特征,但是礁基、礁盖储层物性明显好于礁体本身。礁体储层类型为裂缝型或孔隙裂缝型储层,储层性能主要受沉积相和成岩作用控制。

关键词: 生物礁, 储层, 奥陶系, 塔里木盆地

Abstract:

Ordovicion reef in Lunan-Bachu area of Tarim basin have been discovered recently in Middle Ordovicion Yi Jianfang Formation and Upper Ordovicion Sang Tama Formation.The reef-build-up organism are mainly composed of Calathium,Lithistida,Batostoma and Archaeoscyphia etc.The reef body,small in size and variety in type,is generally made up of reef base,reef core and reef cap.Characterized by low-porosity-low permeability or low porosity-middle permeability based on the analysis of porosity and permeability,rocks of reef reservoir are not good in general,but the porosity of reef base and reef cap is higher than that of reef core.The reservoirs,controlled by sedimentary structure and diagenesis,are mainly in types of fracture and pore-fracture.

Key words: reef, reservoir, Ordovicion system, Tarim

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