石油与天然气地质 ›› 2017, Vol. 38 ›› Issue (1): 71-78.doi: 10.11743/ogg20170108

• 油气地质 • 上一篇    下一篇

渤海A油田扇三角洲相低渗储层特征及物性控制因素

周军良, 胡勇, 李超, 付蓉, 来又春   

  1. 中海石油(中国)有限公司 天津分公司 渤海石油研究院, 天津 300459
  • 收稿日期:2016-01-15 修回日期:2016-12-28 出版日期:2017-02-28 发布日期:2017-02-27
  • 第一作者简介:周军良(1983-),男,工程师,油气田开发地质。E-mail:zhoujl4@cnooc.com.cn。
  • 基金项目:

    国家科技重大专项(2011ZX05023-002);中国海洋石油总公司科技攻关项目(CNOOC-KJ125ZDXM07LTDTJ02)。

Characteristics and controlling factors of fan delta facies low permeability reservoirs in Bohai A oilfield, the Bohai Bay Basin

Zhou Junliang, Hu Yong, Li Chao, Fu Rong, Lai Youchun   

  1. Bohai Oilfield Research Institute, CNOOC China Limited, Tianjin Branch, Tianjin 300459, China
  • Received:2016-01-15 Revised:2016-12-28 Online:2017-02-28 Published:2017-02-27

摘要:

为弄清渤海A油田沙三下亚段的储层特征及物性控制因素,利用薄片、扫描电镜、压汞及常规物性等分析化验资料,分析了储层的岩石成分、孔隙类型及结构、物性特征,并从沉积、成岩和构造作用等方面探讨了储层物性的控制因素。研究表明,沙三下亚段扇三角洲储层主要由成分成熟度低的岩屑长石砂岩组成,孔隙类型主要为原生粒间孔、溶蚀孔及残余原生孔组成的混合孔,孔喉结构表现为微细-细特征,属于低、特低孔-特低渗储层。储层物性主要受控于沉积作用、溶蚀作用及构造活动等。扇三角洲前缘分流河道及河口砂坝沉积环境控制了砂岩碎屑颗粒的粒度和分选,物性较好。压实和胶结作用是储层低渗的主要原因,有机酸对长石、岩屑的溶蚀造成了储层次生孔隙的发育,异常高压的形成减弱了压实作用的强度,促进了原生粒间孔的保存。构造活动形成的断层附近裂缝发育,有助于改善储层物性。综合分析认为,水动力较强的原始沉积环境、后期溶蚀改造及裂缝发育是相对高孔渗储层发育的主控因素。

关键词: 成岩作用, 储层物性, 沙河街组, 扇三角洲, 渤海湾盆地

Abstract:

In order to understand reservoir characteristics and controlling factors of the lower 3rd Member of Shahejie Formation(E2s3L) in Bohai A oilfield,we studied the lithological composition,pore types and structure,porosity and permeability distribution and discussed the controlling factors of petrophysical properties of the reservoirs from sedimentary,diagenetic and tectonic perspectives based on thin section,scanning electron microscopy (SEM),mercury injection and other conventional lab test data.The results show that the reservoirs of fan delta facies in E2s3L have low to ultra-low poro-sity and ultra-low permeability.They are composed of lithic arkosic sandstone with low compositional maturity,their main pore throat types are primary intergranular pore,dissolution pore and residual pore,and the pore throat structure is fine to micro.The reservoir properties were controlled by various factors,including sedimentation,dissolution and tectonic movements etc.Sedimentary environment of distributary channel and mouth bar at fan delta front controlled the grain size and sorting of the reservoir,resulting in relatively good reservoir properties.Compaction and cementation were the main factors causing the low permeability,however,dissolution of feldspar and detritus components by organic acids formed secondary pores,and the abnormal high pressure in the reservoir weakened compaction and helped the preservation of primary intergranular pores.Fractures are well developed near the faults formed by various tectonic movements,which also helped to improve the physical properity of the reservoirs.Through comprehensive analysis of all available data,we can conclude that strong hydrodynamic depositional environment,later dissolution and well-developed fracture network are the main factors that control the formation of the reservoirs with relatively high porosity and permeability.

Key words: diagenesis, physical properity, Shahejie Formation, fan delta, Bohai Bay Basin

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