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本文以系统的野外和室内分析测试为基础，系统地描述了抚顺盆地第三纪富氢煤的岩石学、有机地球化学和加氢液化特征，并对富氢煤的形成条件进行了初步探讨。抚顺煤岩石类型非常丰富，根据煤的宏观岩石组成和结构已划分出１９种岩性相类型。抚顺煤的显微组分总体以富镜质体和贫惰性体和壳质体为特征，但在一些特殊岩石类型分层中，例如：琥珀煤和腐殖－腐泥煤，前者具有丰富树脂体，后者主要由碎块状镜质体和高降解的丝状藻类体组成。抚顺煤的煤级主要为亚烟煤和高挥发分烟煤Ａ。抚顺煤具有限的液化性能，是一种优质的液化煤。抚顺煤形成于温暖潮湿强覆水的富树脂的森林沼泽和比较快速沉降的构造环境。
Based on the systematic field and laboratory tests, the paper systematically described the petrology, organic geochemistry and hydrotreating characteristics of the Tertiary hydrogen-rich coal in the Fushun Basin. The formation conditions of the hydrogen-rich coal were also discussed. Fushun coal rock type is very rich, according to the macro-rock composition and structure of coal has been divided into 19 kinds of lithological facies. The microscopic components of Fushun coal are generally characterized by the presence of vitrinite and lean body and shell bodies, but in some special strata of rock type such as amber coal and humic-rot sap, the former is rich in resin The latter consists mainly of shredded vitrinite and highly degraded filamentous algae. The coal rank of Fushun coal is mainly sub-bituminous coal and high volatile bituminous coal A. Fushun coal liquefaction with limited performance, is a high-quality liquefied coal. Fushun coal is formed in a resin-rich forest swamp that is warm, wet and overwhelmed, and has a relatively rapid subsidence tectonic setting.