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首页> 外文期刊>Journal of Natural Gas Geoscience >Reservoir characteristics and forming conditions for the Middle Triassic Leikoupo Formation in the western Sichuan Basin, China
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Reservoir characteristics and forming conditions for the Middle Triassic Leikoupo Formation in the western Sichuan Basin, China

机译:四川盆地西部中三叠统雷口坡组储层特征及形成条件

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In the past few years, petroleum exploration in the Leikoupo Formation in the western Sichuan Basin of China has obtained fruitful achievements, but composite research on the carbonate rock reservoir and its control factors are lagging behind, which constrains further exploration in the Leikoupo Formation based on field outcrop, core and logging data, while the laboratory analysis, reservoir characteristics and forming conditions of the Leikoupo Formation in the western Sichuan Basin are systematically summarized. The results show: (1) the Leikoupo Formation reservoir mainly involves algae dolomite, grain dolomite and fine powder crystal dolomite with intergranular, intercrystalline and biotrellis pores, and the reservoir generally has low porosity and low permeability; (2) both sedimentary facies and karstification control the development of the Leikoupo Formation reservoir, in which the sedimentary facies is essential to the reservoir, and penecontemporaneous dolomitization and karstification act as a controlling factor to maintain the pore size and secondary pore development, while supergene karstification at the end of the Middle Triassic improved the pores, and the dissolution of organic acid in the burial stage preserved the pores.
机译:近年来,川西地区雷口坡组的石油勘探取得了丰硕的成果,但碳酸盐岩储层及其控制因素的综合研究滞后,制约了雷口坡组在该基础上的进一步勘探。野外露头,岩心和测井资料,系统地总结了川西盆地雷口坡组的室内分析,储层特征和形成条件。结果表明:(1)雷口坡组储层主要为藻类白云岩,粒状白云岩和细晶状白云岩,具有粒间,晶间和生物格状孔隙,普遍具有低孔隙度,低渗透率; (2)沉积相和岩溶作用都控制着雷口坡组储集层的发育,其中沉积相对储集层是必不可少的,同时期白云石化和岩溶作用是维持孔隙大小和次生孔隙发育的控制因素,而表生作用中三叠世末期的岩溶作用改善了孔隙,而有机酸在埋葬阶段的溶解保留了孔隙。

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