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Diagenesis of Paleogene formation in Lenghu region and its impact on porosity evolution
Chen Bo,Sun Guoqiang,Shi Ji'an,Hao Yuanyuan,Shi Haixin,Chen Fenjun
Reservoir Evaluation and Development    2018, 8 (2): 7-13.   DOI: null
Abstract   (258 HTML8 PDF(pc) (2755KB)(300)  

By using the drilling coring data, rock thin section, cast thin section, scanning electron microscope and logging data, and combined with the analysis of the test data, the diagenesis characteristics and its impact on reservoir porosity of Lenghu region of Paleogene has been carried on by the detailed study. The results showed that the maturity of the Lenghu region is low, the primary pore, secondary pore and micro cracks are both developed in the reservoir. The diagenesis types are complex, including compaction, cementation and dissolution. The compaction is the most fundamental reason for failure of reservoir. The porosity loss of the reservoirs in the study area caused of the compaction is 21.65 % in average. The cementation is an important factor for further reducing the reservoir pore loss, causing an average of 3.34 %. The dissolution of the reservoir is an important way to increase the hole, but due to the lack of dissolution fluid, its contribution is limited, increasing pores about 2.26 %. There is a positive correlation between the reservoir properties and maturity, and a negative correlation between the properties and depth, which show that the low maturity and deep buried Lulehe formation (E1+2) has the strongest compaction and cementation, and the worst reservoir property. The property of lower Ganchaigou formation (E3 1) was medium, and the upper of lower Ganchaigou formation(E3 2), which has the highest maturity and is the most shallow buried has the optimal reservoir property.


Fig. 1 Location of research area
Extracts from the Article
柴达木盆地为一典型的中新生代含油气盆地[10],油气勘探显示最重要含油层系位于中生界的三叠系,侏罗系和白垩系,及新生界的古近系,新近系和第四系.冷湖地区(冷湖构造带)位于东祁连山和阿尔金山交汇处,属于柴北缘赛昆断陷的一个二级背斜构造,为第三纪晚期形成的褶皱断裂构造(图1).根据钻井及地面露头揭示,柴北缘冷湖地区古近系地层自下而上发育三套地层,分别为路乐河组(E1+2),下干柴沟组下段(E31)和下干柴沟组上段(E32),古近系与下侏罗系呈不整合接触,中上侏罗系和白垩系缺失,侏罗系是柴北缘的生烃油源.古近系储层发育良好,油储配置关系较好,但研究区古沉积环境多变复杂,沉积相带演变快,主要发育冲积扇—辫状河—辫状河三角洲—滨浅湖沉积体系[9,11-12],储层岩石类型多样,成分及组构特征复杂,储层非均质性强.
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