【摘要】 随着油气形成的有机—无机相互作用观点的提出和发展,人们不断意识到无机物质在有机质生烃演化中的重要作用。深部流体作为地球内部物质运移的载体,承载着大量来自地下深部的无机物质。深部流体的加入将从外源氢、催化剂2个方面的物质供应促进沉积盆地内部有机质的生烃演化,并通过为无机生烃反应提供必要碳源的方式参与烃类物质的无机形成过程。通过对有关外源氢、催化剂作用下的有机质催化加氢反应和以费托合成为代表的无机生烃反应的模拟实验研究的归纳,系统分析了外源氢和催化剂对有机质成烃演化过程的影响,肯定了深部流体的"增烃"效应。更多还原

【Abstract】 As the formation and development of organic-inorganic interaction,people came to realize the important role of inorganic matter during the process of organic matter maturation and hydrocarbon generation.Deep fluids act as a carrier of inner earth substances,and it carried massive inorganic matter from deep earth.The injection of deep fluids provide sedimentary basin with hydrogen sources and catalyst,which would promote the maturation and evolution of organic matters with basins.By providing essential carbon sources for inorganic reaction,deep fluids also took a part in inorganic hydrocarbon generation reaction.This paper collects recent achievements about organic matter hydrogenation reaction and inorganic hydrocarbon generation reaction such as F-T synthesis.By giving a detailed analysis of the effect extraneous hydrogen sources and catalyst exerted on organic maturation and hydrocarbon-producing process,this paper confirms the"increasing hydrocarbon yield"effect of deep fluid.更多还原