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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. 2 Characteristics of rock types in different strata of Paleogene in Lenghu area
Extracts from the Article
柴北缘冷湖地区古近系岩性类型多样,发育有砂岩,泥岩和少量的砾岩,砂岩以细砂岩,砂岩,粉砂岩为主,但不同层位岩石类型及组构特征差异较大.其中E1+2层位以长石岩屑砂岩和岩屑长石砂岩为主(图2a),石英含量较低,长石和岩屑含量高,砂岩的矿物成分成熟度指数Q/F+R值低,均值为0.89;E31层位以岩屑长石砂岩和长石石英砂岩为主(图2b),石英,长石及岩屑三者含量相当,成熟度指数Q/F+R均值为1.38;E32层位以岩屑长石石英砂岩,长石砂岩为主(图2c),石英含量相对较长石,岩屑含量高,成分成熟度指数Q/F+R均值位1.58,整体而言,E32层位成熟度最高,E31层位次之,E1+2层位成熟度最低(表1).研究区储层填隙物以胶结物和泥质杂基为主,碎屑颗粒分选性整体中等—偏差,磨圆度也欠佳,多为次棱状,颗粒接触方式以点—线接触为主,整体表现为较低的结构成熟度.发育于冲积扇—辫状河—辫状河三角洲—湖泊沉积体系下的研究区储层具有近源快速沉积的特点,成分成熟度和结构成熟度均较低.
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