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Characteristics and controlling factors of deep buried-hill reservoirs in the BZ19-6 structural belt, Bohai sea area

机译:渤海地区BZ19-6构造带深层潜山油藏特征及控制因素

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The BZ19-6 deep buried-hill structural belt in the southwest of Bozhong Sag, Bohai Bay Basin, is a newly discovered super-giant oil and gas bearing area. The study on its reservoirs is still in the early stage, and the characteristics and control factors of reservoir development are not understood deeply. In this paper, cores, sidewall cores, rock sections were analyzed and described. Then, based on regional structural setting, mud logging and logging data, the buried-hill reservoirs in this area were analyzed from the aspects of petrological characteristics, reservoir space types and physical properties, the inherent factors influencing the development of the reservoirs were discussed, and distribution laws of the reservoirs were investigated. And the following research results were obtained. First, the deep buried-hill reservoirs of this belt are a pan-buried hill reservoir system composed of the Palaeocene–Eocene Kongdian Fm glutenite in the upper part and the Archean buried-hill metamorphic granite in the lower part. A multi-layer reservoir structure of glutenite pore zone, weathering crust dissolution fracture zone and inner fracture zone is formed. These reservoirs are complex in genesis and diverse in type. Second, the Archean buried-hill metamorphic granite reservoir can be vertically divided into weathering crust, inner fracture zone and tight zone, and it presents the dual characteristics of porous and fractured media. Third, the buried-hill weathering crust is mainly affected by strong dissolution and leaching superimposed with fracturing, forming fractured-porous reservoir space. The reservoir of inner fracture zone is mainly controlled by the superimposition of three-phrase fractures, which forms the main development period of buried-hill fractures since the Yanshanian. Fourth, the glutenite of Kongdian Fm is a typical sieve deposit and it is mainly controlled by the late dissolution. Fifth, migmatization and supercritical fluid cryptoexplosion play a constructive role in the development of the reservoirs. In conclusion, the understanding of buried-hill glutenite and metamorphic reservoir system developed in this belt is conductive to determining the target and direction of next oil and gas exploration in this area.
机译:渤海湾盆地渤中凹陷西南部的BZ19-6深潜山构造带是一个新发现的超大型含油气区。其储层研究仍处于早期阶段,对储层发育的特征和控制因素还没有深入了解。在本文中,对岩心,侧壁岩心,岩石剖面进行了分析和描述。然后,根据区域构造背景,泥浆测井和测井资料,从岩石学特征,储层空间类型和物性等方面分析了该地区的潜山储层,探讨了影响储层发育的内在因素,研究了储层的分布规律。并获得了以下研究结果。首先,该带的深层潜山储层是由上新世—始新世孔店Fm胶体和下部的太古宙潜山变质花岗岩组成的埋藏式丘陵储层系统。形成了砂砾岩孔隙带,风化壳溶解断裂带和内断裂带的多层储层结构。这些储层成因复杂,类型多样。其次,太古宙潜山变质花岗岩储层可垂直划分为风化壳,内部裂缝带和致密带,表现出多孔介质和裂缝介质的双重特征。第三,潜山风化壳主要受强烈的溶蚀作用和淋溶作用的叠加,形成裂缝-多孔储集空间。内裂缝带的储集层主要由三阶段裂缝的叠加控制,形成了燕山期以来潜山裂缝的主要发育时期。第四,孔店组砂砾岩是典型的筛床沉积物,主要受后期溶蚀作用控制。第五,迁移和超临界流体隐爆在油藏开发中起建设性作用。综上所述,对该带发育的潜山砂砾岩和变质油藏系统的认识有助于确定该地区下一次油气勘探的目标和方向。

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