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现代地质 ›› 2009, Vol. 23 ›› Issue (6): 1100-1106.

• 石油地质学 • 上一篇    下一篇

川中广安地区须六段储层特征及控制因素分析

 季丽丹, 贾爱林, 何东博, 位云生, 邵辉   

  1. 中国石油勘探开发研究院,北京100083
  • 收稿日期:2009-07-20 修回日期:2009-09-15 出版日期:2009-12-29 发布日期:2012-02-16
  • 作者简介:季丽丹,女,博士研究生,1981年出生,矿产普查与勘探专业,主要从事油气田开发地质研究工作。Email: ji_lidan@163.com.
  • 基金资助:

    国家“973”项目(2007CB2095)。

Analysis on Controlling Factors and Characteristic of Xu-6 Sandstone Reservoir (Upper Triassic) in Guang'an Region, Central Sichuan Basin

 JI  Li-Dan, JIA  Ai-Lin, HE  Dong-Bo, WEI Yun-Sheng, SHAO  Hui   

  1. Research Institute of Petroleum Exploration and Development, PetroChina,Beijing100083,China
  • Received:2009-07-20 Revised:2009-09-15 Online:2009-12-29 Published:2012-02-16

摘要:

广安地区上三叠统须六段为辫状河三角洲平原分流河道的大套砂岩复合体沉积,以中—细粒长石岩屑砂岩、岩屑砂岩为主;孔隙度主要分布在3%~15%之间,渗透率主要分布在之间。主、次分流河道为该区有效储层,复合砂体内渗透层与致密层交互分布形成了复杂的储层分布特征。在此基础上,结合成岩作用分析储层物性的影响因素认为,物源成分的不同影响储层发育富集区的分布,沉积演化特征控制储层发育层段,沉积微相控制层内非均质性。在煤系地层酸性环境下,强烈压实作用是形成普遍低渗的主要原因。主分流河道沉积的中、粗粒长石岩屑砂岩次生孔隙较发育,是主要的储层岩石类型。

关键词: 川中, 须家河组, 低渗砂岩储层, 辫状河三角洲, 储集性能分析, 储层控制因素

Abstract:

 The Xu-6 reservoir of Guang'an gas field is a large scale sandstone complex of distributary channels of braided delta plain sub facies, and the sandstones of reservoir are mainly medium grained feldspar detritus sandstone and detritus sandstone. It has low porosity and ultra low permeability, with a porosity distribution range of 3% to 15% and permeability distribution range of 0. 01×10-3~1×10-3 μm2. Main and sub-main distributary channels are effective reservoirs, and the alternate distribution of permeable zones and compact layers in sand complex lead to complicated reservoir distribution. Based on above results, and combined with diagenesis, the controlling factors of reservoirs are discussed. The reservoir development is controlled by three sedimentary factors of different scales: distinctive rock composition of sandstones from different source regions which affects enrichment areas of reservoirs; sedimentary evolution which controls reservoir distribution sections; sedimentary micro facies which determines the heterogeneity in sandstones of favorable sections. Strong compaction of sandstones in acid environment of coal measures layer is the main cause of general low permeability. Medium and coarse grained feldspar detritus sandstones deposited in main distributary channels, which have relatively high secondary dissolved pores, are the main sandstone type of reservoirs.

Key words:  Central Sichuan, Xujiahe Formation, low permeability sandstone reservoir, braided delta, reservoir quality, controlling factors of reservoir

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