石油与天然气地质 ›› 2015, Vol. 36 ›› Issue (6): 873-879.doi: 10.11743/ogg20150601

• 油气地质 • 上一篇    下一篇

致密碎屑岩储层“甜点”形成及保持机理——以鄂尔多斯盆地西南部镇泾地区延长组长8油层组为例

刘春燕   

  1. 中国石化 石油勘探开发研究院构造与沉积储层实验室, 北京 100083
  • 收稿日期:2015-01-29 修回日期:2015-10-16 出版日期:2015-12-08 发布日期:2016-01-08
  • 作者简介:刘春燕(1965—),女,高级工程师,沉积储层与成岩作用。E-mail:liuchunyan.syky@sinopec.com。
  • 基金资助:
    国家科技重大专项(2016ZX05002-006,2016ZX05002-006-003)。

Formation and preservation mechanism of sweet spot in tight clastic reservoirs —A case study of Chang 8 oil layer of Yanchang Formation in Zhenjing area, southwest Ordos Basin

Liu Chunyan   

  1. Laboratory of Structure & Sedimentary Reservoir, Petroleum Exploration & Production Research Institute, SINOPEC, Beijing 100083, China
  • Received:2015-01-29 Revised:2015-10-16 Online:2015-12-08 Published:2016-01-08

摘要: 中西部盆地碎屑岩普遍致密化、储层“甜点”预测难度大是制约油气发现的重要因素。为探索储层致密化及“甜点”形成和保持机理,通过岩心观察、铸体、荧光、包裹体、阴极发光等薄片鉴定、粒度分析、压汞和覆压孔渗测试、扫描电镜和能谱分析等沉积、岩石和地球化学综合研究,根据成因类型,将鄂尔多斯盆地西南部镇泾地区延长组长8油层组“甜点”划分为原生型、次生型两大类,认为早期绿泥石膜的发育适度抑制了后期的成岩改造,是原生型“甜点”得以形成、保持的重要因素。对于次生型“甜点”,各类溶蚀孔和微裂缝为其主要孔隙空间,可进一步划分为溶蚀型“甜点”和裂缝型“甜点”,并证实了各类溶蚀、破裂等建设性成岩作用是形成次生型“甜点”的关键因素。研究认为,早期油气充注可有效地抑制后期胶结作用的发生,多期次的成岩交替过程使“甜点”形成-保持(或失效)。纵向上,单砂体的去致密化作用始自原生孔隙保存相对较好的高渗层或裂缝与溶蚀作用较强的叠合部位,并逐渐向外推进。平面上,砂体的去致密化有着类似的特点,顺沿砂体,储层“甜点”呈现“竹节状”分布的特点。

关键词: “甜点”发育模型, 成岩作用, 碎屑岩, 致密储层, 延长组, 鄂尔多斯盆地

Abstract: Densification of clastic reservoirs and difficulties in predicting their sweet spots constrain petroleum discovery in basins in central and western China.In order to investigate the mechanisms of reservoir densification and formation and preservation of sweet spots,a comprehensive study of sedimentology,petrology,and geochemstry were performed by using various methods,including core observation,microscopic observation of casting thin section and under fluorescence and cathode luminescence,fluid inclusion analysis,particle size analysis,mercury injection and permeability tests under overburden pressure,scanning electron microscopic analysis and so on.According to the generic types,sweet spots of the Chang 8 oil layer of Yanchang Formation in Zhenjing area, southwest Ordos Basin,are divided into a primary type and a secondary type.Early developments of chlorite films moderately inhibited later diagenesis processes,which is the main factor contributing to the formation and preservation of the primary sweet spot.The secondary type can be subdivided into a dissolution-type and a fracture-type according to their major pore space being dissolution pores or microfractures.The key factor determining the formation of the secondary sweet spot is constructive diagenesis.It can be concluded that the early charging of hydrocarbons effectively inhibited later cementation,and the multiphase diagenesis resulted the formation and preservation(or lost)of sweet spots.In vertical sections,individual sand body de-densification started from layers of relative high permeability,or areas of fracture and dissolution superimposing,and propagated outwards progressively.In planar view,sand body de-densification shows similar features,the sweet spots distribute in “bamboo-like” shape along the sand body.

Key words: sweet spot development model, diagenesis, clastic rock, tight reservoin, Yanchang Formation, Ordos Basin

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