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Effects of the matrix on the oil production of supertight limestone in a lacustrine mixed sedimentary environment: The case of the Jurassic Da'anzhai member in the central Sichuan Basin, China

机译:矩阵对湖泊中超信石油生产石油生产的影响:中国中部侏罗纪大安寨成员的案例

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摘要

Lacustrine limestone always develops multiple matrices, and the matrices characteristics and effects on oil production have not been carried out effectively. Although the lacustrine limestone of the Jurassic Da'anzhai Member in the central Sichuan Basin is considered supertight, it still produces relatively large amounts of oil. To explain this yield characteristic, typical matrix samples were analyzed to determine the classification and effects on tight oil production, and identify the geological causes of different matrices. (1) The matrix types can be divided into calcareous matrix, argillaceous matrix, siliceous matrix and mixed matrix, and their micro pore-crack systems are well developed. (2) The argillaceous matrix samples are not as tight as the calcareous matrix samples with relatively low discharge pressure and high maximum mercury saturation. The mercury withdrawal efficiency and NMR mobile water saturation of the calcareous matrix samples are higher than those of the argillaceous matrix samples. The isotherms of the nitrogen adsorption and the adsorption loop indicate a wedge-shaped pore type and a slit-shaped pore type. The nanoscale storage space gradually increases from the calcareous matrix to the siliceous matrix to the mixed matrix and finally the argillaceous matrix. (3) The matrix pore-crack system effectively controls tight oil production. The simultaneous development of multiscale pores and cracks in the limestone matrix is the key factor in tight oil production. (4) Different matrix types are finally formed by the original sediments determined by the lacustrine mixed sedimentary after diagenetic evolution processes. Calcareous, siliceous, argillaceous and mixed matrices are mainly formed in the shell beach core, sandy shoal, shell beach slope, and shell beach edge, respectively. The shell beach edge and shell beach slope are associated with favorable matrix types.
机译:Lapustrine LimeStone总是开发多个矩阵,并且矩阵特性和对石油生产的影响尚未有效地进行。虽然四川盆地中侏罗纪大南海成员的湖泊石灰岩被认为是超信,但它仍然产生相对大量的油。为了解释该产量特征,分析典型的基质样品以确定对稀土的分类和影响,并确定不同矩阵的地质原因。 (1)基质类型可分为钙质血管基质,骨质基质,硅质基质和混合基质,它们的微孔裂纹系统均发育良好。 (2)骨质基质样品不如具有相对低的放电压力和高最大汞饱和度的钙质基质样品紧张。钙质基质样品的汞取出效率和NMR移动水饱和度高于骨质基质样品的含量。氮吸附和吸附环的等温线表示楔形孔型和狭缝形孔型。纳米级存储空间从钙质基质到混合基质的钙质基质逐渐增加,最后是骨质基质。 (3)基质孔隙裂纹系统有效地控制了稀疏的石油生产。多尺度孔隙和石灰石基质中的裂缝的同时发展是油生产紧密的关键因素。 (4)最终通过曲线进化过程后由湖泊混合沉积物确定的原始沉积物最终形成不同的基质类型。钙质,硅质,骨质和混合矩阵主要形成在壳滩核心,沙质浅滩,壳滩坡和壳滩边缘。 Shell Beach Edge和Shell Beach斜率与有利的矩阵类型相关联。

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