Characteristics and development model of deep-ultra deep reservoirs in the Upper Wuerhe Formation of Permian in the sags of eastern Junggar Basin, China

Qiuyu Wang , Wenqi Yan , Zhiyi Xie , Chaowei Liu , Hui Li
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Abstract

Taking the deep-ultra deep glutenite reservoirs in the Upper Wuerhe Formation of Permian in Fukang Sag and Dongdaohaizi Sag as the research object and representative of the eastern Junggar Basin, its characteristics and main controlling factors are analyzed using various methods, including core analysis, thin section examination, and scanning electron microscope observation. High-pressure mercury injection and logging imaging were also employed to reveal the reservoir that Fukang and Dongdaohaizi sags harbor deep-ultra deep glutenite reservoirs, with Fukang Sag being a typical low porosity to ultra-low permeability reservoir, while Dongdaohaizi Sag is a low porosity to low permeability reservoir. Reservoir space types vary between the two sags, with Fukang Sag characterized by microfractures and corrosion pores, while a large number of corrosion pores with fewer fractures existing in Dongdaohaizi Sag. Both compaction and cementation exhibit a strong destructive effect on the reservoirs in the eastern Junggar Basin. However, the compaction effect in Fukang Sag is very strong, and the dissolution effect is weak. The large number of fractures generated by overpressure becomes an effective channel for ultra-deep oil and gas migration. The cracks in the Dongdaohaizi Sag are underdeveloped, and a large number of intra-particle corrosion pores generated by the dissolution of feldspar and turbidite improve reservoir properties. In addition, its rich turbidite also plays a compressive and pore retention role. There are two types of reservoir models developed in the Upper Wuerhe Formation of Permian in the eastern Junggar Basin: the deep fracture model represented by the Fukang Sag and the solution pore model rich in turbidite in Dongdaohaizi Sag. These models create favorable conditions for oil and gas accumulation in the deep-ultra deep reservoirs in the depression area.

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中国准噶尔盆地东部下陷二叠系上乌尔禾组深-超深储层特征及发育模式
以准噶尔盆地东部具有代表性的二叠系上统乌尔禾地层阜康下陷和东道海子下陷深-超深糯米质储层为研究对象,采用岩心分析、薄片检查、扫描电镜观察等多种方法分析了其特征和主要控制因素,并通过高压注汞和测井成像揭示了阜康下陷和东道海子下陷深-超深糯米质储层,其中阜康下陷为深-超深糯米质储层。通过高压注汞和测井成像,揭示了阜康下陷和东道海子下陷蕴藏深-超深糯质岩储层,其中阜康下陷为典型的低孔隙度-超低渗透储层,东道海子下陷为低孔隙度-低渗透储层。两个下陷的储层空间类型各不相同,阜康下陷以微裂缝和腐蚀孔隙为特征,而东道海子下陷则存在大量腐蚀孔隙,裂缝较少。压实和胶结对准噶尔盆地东部的储层都有很强的破坏作用。但阜康下陷的压实作用很强,溶蚀作用较弱。超压产生的大量裂缝成为超深油气运移的有效通道。东道海子下陷裂缝不发育,长石和浊积岩溶解产生的大量粒内腐蚀孔隙改善了储层性质。此外,其丰富的浊积岩也起到了压缩和滞留孔隙的作用。准噶尔盆地东部二叠系上统乌尔禾地层发育有两种储层模式:以阜康下陷为代表的深部断裂模式和东道海子下陷富含浊积岩的溶蚀孔隙模式。这些模式为凹陷区深-超深储层的油气聚集创造了有利条件。
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