鄂尔多斯盆地姬塬地区长6 储层成岩作用研究
网络出版日期: 2013-02-20
基金资助
国家自然科学基金项目“中国中西部地质历史时期湖相白云岩类比研究及实验模拟”(编号:41272115)资助
Diagenesis of Chang 6 reservoir of Upper Triassic in Jiyuan area,Ordos Basin
Online published: 2013-02-20
李标 , 唐海 , 吕栋梁 . 鄂尔多斯盆地姬塬地区长6 储层成岩作用研究[J]. 岩性油气藏, 2013 , 25(1) : 69 -74 . DOI: 10.3969/j.issn.1673-8926.2013.01.014
The Chang 6 reservoir of Upper Jurassic in Jiyuan area is characterized by poor physical properties, complicated diagenesis, strong heterogeneity and low permeability. Based on the analysis of cast thin section, cathode luminescence and scanning electronic microscope, the diagenesis of Chang 6 reservoir was studied. The result shows that sandstone reservoirs in this area are mainly composed of fine lithic arkose and feldspathic sandstone, mainly developed intergranular pores and intragranular dissolved pores, mainly experienced compaction, cementation, dissolution and metasomatism, and the diagenetic evolution reached the middle diagenetic stage A. The diagenesis of Chang 6 reservoir is the main controlling factor for reservoir properties. This study can provide basic data and guidance for the oil and gas exploration and development in this area.
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