吉林四五家子油田下白垩统泉二段储层成岩储集相及储集空间演化

黄述旺; 窦齐丰

吉林四五家子油田下白垩统泉二段储层成岩储集相及储集空间演化

石油大学资源与信息学院, 北京 102249

基金项目: 中国石油天然气集团公司油气储层重点实验室项目

详细信息

作者简介:
黄述旺(1944-), 男, 教授, 1966年毕业于北京地质学院, 主要从事测井地质和油藏描述的教学和科研工作

中图分类号: P618.130.1
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出版历程
- 收稿日期: 2002-08-12
- 刊出日期: 2002-11-25

Characteristics of Diagenesis-Reservoir Facies and Pore Space Evolution of the Second Member of Quantou Formation at Siwujiazi Oilfield, Jilin Province

Resources and Information Institute, University of Petroleum, Beijing 102249, China

摘要

摘要: 利用四五家子油田取心井的岩石铸体薄片鉴定、扫描电镜观察、粘土矿物X衍射分析等资料, 研究了泉二段储层的成岩作用、成岩演化序列, 并划分了成岩作用阶段.泉二段储层可划分为4种成岩储集相类型, 储集物性由好至差依次为, A相: 弱胶结中等压实粒间孔成岩储集相; B相: 胶结物溶解次生孔隙成岩储集相; C相: 杂基充填强压实微孔隙成岩储集相; D相: 早期方解石胶结成岩储集相.详细阐述了各类成岩储集相的特征, 并对其成因进行了分析.最后探讨了泉二段储层的储集空间类型及其演化模式.
- 四五家子油田 /
- 泉二段 /
- 成岩储集相 /
- 储集空间演化
Abstract: Based on the analytic data of casting thin section, scanning electron microscope, X-ray diffraction of clay minerals of well core samples at Siwujiazi oilfield, the diageneses, diagenetic sequences and stages of the Second Member of Quantou Formation of the Lower Cretaceous were studied. The study suggests that its reservoir rocks can be divided into 4 types of diagenetic-reservoir facies, i.e. facies A, which has undergone weak cementation and middle compaction and has interparticle pores; facies B, in which calcite cements have been greatly dissolved and secondary dissolution pores have been developed; facies C, which has undergone strong compaction and has micro pores, showing matrix filled in interparticles; facies D, which has undergone early calcite cementation. The characteristics and origin of each diagenesis-reservoir facies are described in detail. Finally the types and evolution of pore space are discussed.
- Siwujiazi oilfield /
- Jq2 /
- diagenetic-reservoir facies /
- pore space evolution

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图 1 四五家子油田构造位置

Fig. 1. Tectonic location of Siwujiazi oilfield

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图 2 四五家子油田泉二段储层成岩演化序列

Fig. 2. Diagenetic sequences of Jq² at Siwujiazi oilfield

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图 3 四五家子油田泉二段储层成岩作用阶段划分

Fig. 3. Diagenetic stages of Jq² at Siwujiazi oilfield

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图 4 四五家子油田泉二段储层储集空间演化模式

Fig. 4. Pore space evolution of Jq² at Siwujiazi oilfield

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表 1 四五家子油田泉二段储层各类成岩储集相特征

Table 1. Characteristics of each diagenesis-reservoir facies of Jq² at Siwujiazi oilfield

参考文献(3)

[1]	郑浚茂, 庞明. 碎屑储集岩的成岩作用研究[M]. 武汉: 中国地质大学出版社, 1989. ZHENG JM, PANGM. Diagenesis study of clastic rock[M]. Wuhan: China University of Geosciences Press, 1989.
[2]	张守鹏, 蔡进功, 魏魁生. 胜利油气区粒屑碳酸盐岩形成机制与储油气性[J]. 地球科学——中国地质大学学报, 2000, 25(2): 147-151. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200002008.htm ZHANG S P, CAI J G, WEI K S. Sedimentary mechanism and reservoir implication of grained carbonate in Shengli oilfield[J]. Earth Science— Journal of China University of Geosciences, 2000, 25(2): 147-151. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200002008.htm
[3]	彭仕宓, 黄述旺. 油藏开发地质学[M]. 北京: 石油工业出版社, 1998. PENG S M, HUANG S W. Reservoir development geology[M]. Beijing: Petroleum Industry Press, 1998.