[1]郭军,陈洪德,赵俊兴,等.镇泾探区长9成岩作用及对储层物性的影响[J].复杂油气藏,2014,(02):21.
　Guo Jun,Chen Hongde,Zhao Junxing,et al.Diagenesis and its influence on the reservoir quality of Chang 9 oil layer in Zhenjing area[J].Complex Hydrocarbon Reservoirs,2014,(02):21.
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镇泾探区长9成岩作用及对储层物性的影响
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《复杂油气藏》[ISSN:1674-4667/CN:31-2019/TQ]

卷:
期数:
2014年02期
页码:
21
栏目:
油气勘探
出版日期:
2014-06-25

文章信息/Info

Title:
Diagenesis and its influence on the reservoir quality of Chang 9 oil layer in Zhenjing area
作者:
郭军1; 2; 陈洪德2; 3; 赵俊兴2; 3; 向芳2; 3; 李婕2; 孔祥超2
1.湖南省煤炭地质勘查院，湖南长沙410014;2.成都理工大学沉积地质研究院，四川成都610059； 3.成都理工大学油气藏地质及开发工程国家重点实验室，四川成都
Author(s):
Guo Jun1; Chen Hongde2; 3; Zhao Junxing2; 3; Xiang Fang2; 3; Li Jie2; Kong Xiangchao2
1.Hunan Institute of Coal Geology and Exploration，Changsha,Hunan 410014; 2.Institute of Sedimentary Geology，Chengdu University of Technology，Chengdu,Sichuan 610059; 3.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation，Chengdu University of Technology，Chengdu，Sichuan 610059
关键词:
长９储层　储层物性　成岩作用　镇泾探区　鄂尔多斯盆地
Keywords:
Chang 9 reservoir; reservoir property; diagenesis; Zhenjing area; the Ordos Basin
分类号:
TE122.12
文献标志码:
A
摘要:
利用岩心描述、铸体薄片、扫描电镜和岩矿分析等手段，对鄂尔多斯盆地镇泾探区长9储层砂岩的成岩作用及其对储层物性发育的影响进行了分析研究。结果表明：研究区储层砂岩经历了压实、胶结、溶蚀、交代和重结晶五种成岩作用类型，其中压实作用使得塑性岩屑发生弯曲变形、刚性岩屑碎裂，导致原生孔隙大幅度减少；方解石胶结物在某些井位和层段中含量可达25%，并形成连生胶结，造成砂岩的孔隙度损失严重；溶蚀作用形成的次生粒内溶孔（包括少量粒间溶孔）增加了研究区储层砂岩平均值为287%的面孔率。长9储层砂岩处于晚成岩阶段A期的晚期至B期的早期。
Abstract:
With the use of core description，casting thin sections，scanning electrom microscopy and rock ore analysis etc.，the diagenesis and its influence on the reservoir quality of Chang 9 reservoir sandstone in Zhenjing exploratory area，Ordos Basin，was analyzed and researched.The results showed that the sandstone reservoir in the study area experienced five types of diageneses: compaction，cementation，dissolution，metasomatism，and recrystallization.The compaction made the plastic debris bending deformation and rigid rock splintering，leading to the great reduction of primary pores.In some locations and intervals，calcite cement content can reach 25% and form cementation，making serious loss of sandstone porosity.The secondary solution pores，generated by dissolution，including a small amount of intergranular dissolved pores，increased the face rate of rock by 2.87%.Chang 9 reservoir sandstone was at the late A stage to the early B stage of the late diagenetic period.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期：2013-12-09；改回日期：2014-02-11
作者简介：郭军(1983—)，助理工程师，硕士，沉积地质学方面研究。电话：0731-85648630，E-mail：gj2010lj@163.com。
更新日期/Last Update: 2014-06-25