Fluid activity characteristics of shallow shale veins in the Wufeng–Longmaxi Formation in the Shixi syncline in northern Guizhou and their significance for shale gas preservation

IF 4.2 3区 工程技术 Q2 ENERGY & FUELS
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Abstract

Preservation conditions are key to enriching shallow shale gas. Therefore, the veins of two typical wells in the Shixi syncline in northern Guizhou as research objects. Based on core observation, vein thin-section observation, cathodoluminescence, calcite in situ U-Pb dating, fluid inclusion microthermometry, Raman spectrum shift, single well basin simulation, and C-O isotope geochemical analysis, the researchers clarified the characteristics of the veins and the differences in paleofluid activity, as well as their significance for shale gas preservation. The results showed that: 1) a small number of high-angle fractures had developed mainly in the Shixi syncline in northern Guizhou. The width of viens is small and filled primarily with early calcite-quartz and late calcite. The inclusions were mainly methane and brine. The proportion of brine inclusions in the SD1 well was greater than that in the SX1 well. The SD1 well has experienced more intense second-stage uplift and denudation, and the consequent gas loss is serious. 2) The results of the C-O isotope analysis showed that most of the vein-forming fluids were derived from marine carbonate rocks. The O3b had obvious negative deviations of δ13C and δ18O, which were modified by exogenous or deep hydrothermal fluid. The C-O isotope difference between the vein bodies and the surrounding rock of the SX1 well was small, and the preservation conditions were better. 3) The difference in gas content in the Shixi syncline depends on the degree of damage to gas reservoir preservation conditions caused by burial depth and other factors. Shixi syncline is a wide and gentle syncline with central retention enrichment mode. Therefore, clarifying the development of shale veins, the characteristics of paleofluid activity, and their significance for shale gas preservation can lay a foundation for studying the enrichment mechanism of shallow shale gas and thus guide further exploration and development.
贵州北部石溪向斜五峰-龙马溪地层浅层页岩脉的流体活动特征及其对页岩气保存的意义
保存条件是浅层页岩气富集的关键。因此,以贵州北部石溪向斜两口典型井的岩脉为研究对象。研究人员通过岩心观察、岩脉薄片观察、阴极发光、方解石原位U-Pb测年、流体包裹体微测温、拉曼光谱移动、单井盆地模拟、C-O同位素地球化学分析等手段,阐明了岩脉特征、古流体活动差异及其对页岩气保存的意义。结果表明1)主要在贵州北部的石溪向斜中发育了少量高角度断裂。裂隙宽度较小,主要由早期方解石-石英和晚期方解石填充。包裹体主要是甲烷和卤水。SD1 井的盐水包裹体比例高于 SX1 井。SD1井经历了更强烈的第二阶段隆升和剥蚀,因此气损严重。2)C-O 同位素分析结果表明,大部分成脉流体来源于海相碳酸盐岩。O3b的δ13C和δ18O有明显的负偏差,这是由外源流体或深部热液改变的。SX1井脉体与围岩的C-O同位素差异较小,保存条件较好。3)石溪向斜含气量的差异取决于埋藏深度等因素对气藏保存条件的破坏程度。石溪向斜是一条宽缓的向斜,具有中心滞留富集模式。因此,弄清页岩脉发育、古流体活动特征及其对页岩气保存的意义,可为研究浅层页岩气富集机理奠定基础,从而指导进一步的勘探开发。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Natural Gas Industry B
Natural Gas Industry B Earth and Planetary Sciences-Geology
CiteScore
5.80
自引率
6.10%
发文量
46
审稿时长
79 days
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