煤储层流体特征、成藏控制因素及富集模式——以鄂尔多斯盆地中东部上古生界为例

IF 7 Q1 ENERGY & FUELS
Shida CHEN , Dazhen TANG , Wei HOU , Daojun HUANG , Yongzhou LI , Jianling HU , Hao XU , Shu TAO , Song LI , Shuling TANG
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引用次数: 0

摘要

根据鄂尔多斯盆地中东部上古生界探井岩心的测试和实验资料,结合构造、埋藏深度和流体地球化学分析,揭示了上古生界煤储层流体特征、天然气成藏控制因素和成藏模式。该研究表明了两个方面的发现。首先,1 500 ~ 1 800 m段是浅中深开放流体体系与深部封闭流体体系之间的临界过渡带;1 500 m以上储层水侵强度大,压力梯度分布离散,甲烷与不同程度的次生生物气混合存在,普遍表现为高含水饱和度和吸附气欠饱和。深度大于1 800 m的储层为自封闭储层,渗透率极低,含水动力侧向封堵和致密盖层封闭共同形成的封闭流体体系。在这些系统中,地表径流入渗较弱,二次流体转化程度最小,压力梯度相对均匀。大部分煤层吸附气饱和度超过100%,游离气含量主要在1 ~ 8 m3/t之间(部分煤层大于10 m3/t)。②深部煤中天然气成藏主要受煤质、储盖组合、构造位置等因素的控制,受地下温度和压力条件的约束。含灰岩和泥岩盖层的高阶低灰分煤具有较好的成藏潜力。正构造高点和宽缓的负构造低点是天然气富集的有利部位,褶皱分支斜坡带的含气量相对较低。该研究增强了对煤储层成藏机理的认识,为深部资源精准区域化评价和自适应增产技术创新提供了有效的参数参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fluid characteristics, gas accumulation controlling factors and gas enrichment modes in coal reservoirs: A case study of the Upper Paleozoic in the central-eastern Ordos Basin, NW China
Based on the test and experimental data from exploration well cores of the Upper Paleozoic in the central-eastern Ordos Basin, combined with structural, burial depth and fluid geochemistry analyses, this study reveals the fluid characteristics, gas accumulation control factors and accumulation modes in the Upper Paleozoic coal reservoirs. The study indicates findings in two aspects. First, the 1 500–1 800 m interval represents the critical transition zone between open fluid system in shallow–medium depths and closed fluid system in deep depths. The reservoirs above 1 500 m reflect intense water invasion, with discrete pressure gradient distribution, and the presence of methane mixed with varying degrees of secondary biogenic gas, and they generally exhibit high water saturation and adsorbed gas undersaturation. The reservoirs deeper than 1 800 m, with extremely low permeability, are self-sealed, and contains closed fluid systems formed jointly by the hydrodynamic lateral blocking and tight caprock confinement. Within these systems, surface runoff infiltration is weak, the degree of secondary fluid transformation is minimal, and the pressure gradient is relatively uniform. The adsorbed gas saturation exceeds 100% in most seams, and the free gas content primarily ranges from 1 m3/t to 8 m3/t (greater than 10 m3/t in some seams). Second, the gas accumulation in deep coals is primarily controlled by coal quality, reservoir-caprock assemblage, and structural position governed storage, wettability and sealing properties, under the constraints of the underground temperature and pressure conditions. High-rank, low-ash yield coals with limestone and mudstone caprocks show superior gas accumulation potential. Positive structural highs and wide and gentle negative structural lows are favorable sites for gas enrichment, while slope belts of fold limbs exhibit relatively lower gas content. This research enhances understanding of gas accumulation mechanisms in coal reservoirs and provides effective parameter reference for precise zone evaluation and innovation of adaptive stimulation technologies for deep resources.
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CiteScore
11.50
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