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含油气盆地中热液流体对油气成藏的影响已经成为油气地质研究的热点。基于钻井岩心观察、岩石薄片鉴定、流体包裹体测温、碳氧同位素、元素地球化学及地层水分析等实验技术方法,分析鄂尔多斯盆地靖边气田马家沟组五段(马五段)碳酸盐岩储层中热液活动特征,探讨热液活动对油气的地质意义。结果表明：靖边气田马家沟组热液活动特征主要体现在热液黄铁矿充填溶孔、流体包裹体的均一温度异常增高、脉体方解石的碳氧同位素和天然气中H2S硫同位素均指示了高温热液异常、白云岩稀土元素显示明显的δEu正异常和δCe负异常,且样品全部分布在Ya/La—Yb/Ca交会图的热液成因区域,部分主量元素和微量元素因热液作用显著增加。地层水特征显示出多种地质因素综合作用的结果。因此推断深部热液流体通过基底断裂和古断裂上升,沿着马五段顶部不整合面和古断裂进入马家沟组。前期可对岩石中的不稳定组分进行溶蚀,形成大量的次生溶蚀孔洞,对储层起建设性作用。后期随着热液流体温度的降低及压力系统的改变,热液流体形成的黄铁矿、石英和方解石开始大量沉淀,充填溶蚀孔洞和裂缝,对储层起破坏性作用。 相似文献
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The transport of liquid plugs in microchannels is very important for many applications such as in medical treatments in airways and in extraction of oil from porous rocks. A plug of wetting and non-wetting liquids driven by a constant pressure difference through a T-shaped microchannel is studied numerically with lattice Boltzmann (LB) method. A two-phase flow LB model based on field mediators is built. Three typical flow patterns (blocking, rupture and splitting flow) of plug flow are obtained with different driving pressures. It is found that it becomes difficult for a plug with short initial plug length to leave the microchannel; the flow pattern of plug transport varies with the contact angle, especially from wetting to nonwetting; with the increase of interfacial tension, the front interface of plug moves faster; the front and rear interfaces of the plug with small viscosity ratio move faster in the microchannel than those of the plug with large viscosity ratio. The study is helpful to provide theoretical data for the design and scale-up of liquid-liquid reactors and separators. 相似文献
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