Study on the genesis of carbonate cements in tight and non-tight sandstone reservoirs in Fukang Sag

Li Na , Wang Zi'ang , Liu Gang , Wang Guozhi , Huang Sheng , Liu Jinlong , Jing Yang , Chen Haixia
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Abstract

Carbonate cements characterization and reservoir genesis mechanism are the key geological issues constraining the current deep oil and gas exploration. The relationship between carbonate cementation and oil and gas filling time can affect reservoir reserves. In this paper, the tight and non-tight sandstone reservoirs of the Middle Jurassic in Fukang Sag of Junggar Basin are taken as the research object. The petrology, sedimentary microfacies, diagenesis, porosity and carbonate cements of tight and non-tight reservoirs are compared by means of casting thin sections, scanning electron microscope (SEM) and carbon and oxygen isotopes. The research shows that the tight reservoirs and non-tight reservoirs of deep sandstone in Fukang sag are similar in rock type and sedimentary microfacies, they are all feldspar lithic sandstone. The reservoirs are mainly developed in underwater distributary channels and estuary sand dams. There are obvious differences in the strength of compaction and pore types. Although they all contain carbonate cements, their genesis and formation time are obviously different. The results show that the carbonate cements in the non-tight sandstone reservoirs of the Toutunhe Formation are mainly of Microbial sulfate reduction (BSR) origin, which are formed in the process of reservoir failure. The formation of carbonate mineral cements in tight sandstone reservoirs of the Badaowan Formation and Sangonghe Formation is mainly related to the decarboxylation of organic acids, which are mainly formed in the process of hydrocarbon accumulation. The research in this paper can provide theoretical guidance for exploration and development in the future of the 4th Block of central Junggar Basin and similar research areas.
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阜康凹陷致密与非致密砂岩储层碳酸盐胶结物成因研究
碳酸盐胶结物表征及成藏机理是制约当前深部油气勘探的关键地质问题。碳酸盐岩胶结作用与油气充填时间的关系影响储层储量。本文以准噶尔盆地阜康凹陷中侏罗统致密和非致密砂岩储层为研究对象。采用浇铸薄片、扫描电镜(SEM)和碳氧同位素等方法,对致密储层和非致密储层的岩石学、沉积微相、成岩作用、孔隙度和碳酸盐胶结物进行了比较。研究表明,阜康凹陷深部砂岩致密储层与非致密储层在岩石类型和沉积微相上相似,均为长石岩屑砂岩。储层主要发育在水下分流河道和河口沙坝中。压实强度和孔隙类型存在明显差异。虽然均含有碳酸盐胶结物,但其成因和形成时间明显不同。结果表明,头屯河组非致密砂岩储层中的碳酸盐胶结物主要为微生物硫酸盐还原物(BSR)成因,是在储层破坏过程中形成的。八道湾组和三工河组致密砂岩储层碳酸盐矿物胶结物的形成主要与有机酸的脱羧作用有关,主要是在油气成藏过程中形成的。本文的研究可为准噶尔盆地中部四区块及类似研究区今后的勘探开发提供理论指导。
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