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黄骅坳陷二氧化碳气成因类型及分布规律

机译:黄骅坳陷二氧化碳气成因类型及分布规律

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CO2 gas is a nonhydrocarbon gas, with a high economic value and a broad prospect for application. In the Huanghua Depression, there exist many genetic types of CO2 gases, i.e. organic CO2, thermal metamorphic CO2 and crust-mantle mixed CO2. The distribution of different types of CO2 gases is controlled by different factors. Organic CO2 that occurs mainly around the oil-generating center is associated with hydrocarbon gases as a secondary product and commonly far away from large faults. Thermal metamorphic CO2 occurs mainly in areas where carbonate strata are developed and igneous activity is strong, and tends to accumulate near large faults. CO2 of such an origin is higher in concentration than organic CO2, but lower than crust-mantle mixed CO2. Crust-mantle mixed CO2 occurs mainly along large faults. Its distribution is limited, but its purity is the highest.
机译:CO2气体是一种非烃类气体,具有高经济价值和应用的广阔前景。在黄花凹陷中,存在许多遗传类型的CO 2气体,即有机二氧化碳,热变形二氧化碳和壳体混合CO2。不同类型的二氧化碳气体的分布由不同的因素控制。主要周围发生的有机二氧化碳与油生成中心周围发生的烃类气体与二级产品相关,并且常见远离大故障。热性变质二氧化碳主要发生在碳酸盐层的开发和火火活性强度的区域中,并且倾向于积累近大断层。这种原点的CO 2浓度高于有机二氧化碳,但低于壳体裂缝混合CO 2。 Crust-Mantle混合Co2主要发生在大故障。其分配有限,但其纯度最高。

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