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1.Presented in this study are the characteristics of aromatic hydrocarbon biomarkers in the Lower Palaeozoic marine carbonate rocks in North China, including phenanthrene, biphengl, benznuorene,benzfhiore tri-fluorene, fluoranthene series pyrene, benz fluoranthene series beamperylene, chrysene and triaromatic sterane. The content of naphthalene is relatively low.
本文详细总结了华北地区下古生界海相烃源岩中芳烃生物标志物特征，主要包括菲系列、联苯系列、苯并芴系列，三芴系列、荧蒽系列、芘系列、苯并荧蒽和苯并芘系列、　系列和三芳甾烷系列，而萘系列含量较低。收藏指正
2.Occurrence of High Mature Organic Matter in Marine Black Shale Source Rocks of Lower Cambrian from Northern Tarim Basin,China
塔里木盆地下寒武统底部高熟海相烃源岩中有机质的赋存状态收藏指正
3.VITRINITE-LIKE MACERALS IN CHINESE EARLY PALAEOZOIC SOURCE ROCKS
下古生界高过成熟烃源岩中的镜状体收藏指正
4.Taking the Dongying Sag source rocks in Eogene as the example, the main task of this article is to discuss the accumulation mechanisms of fractured mudstone reservoirs by researching on the characters of source rocks and the evolution of hydrocarbons;
本文以东营凹陷下第三系的烃源岩为例，在对烃源岩的特征、分布及成烃过程、裂缝的特征、成因及分布、油气在烃源岩中的运移聚集机理研究基础上，探讨泥质岩裂缝油气藏的成藏机理。 得到的主要认识有：收藏指正
5.The geochemical characteristics of extract from the source rocks,such as organic matter composition of saturation hydrocarbon(based on gas chromatogram),composition and configuration characteris tics of steroid and triterpane(based on GC/MS),and carbon isotopes composition of chloroform bitumen A and group composition have been presented too. According to the geochemical characteristics of organic matter in source rocks,the parent matter type,geochemistry en-viron ment and maturity of organic matter were analyzed.
介绍了长岭地区主要烃源岩的分布特征、有机质丰度、类型及热演化程度,描述了烃源岩中有机质族组成特征、饱和烃气相色谱特征、甾烷、三萜烷系列化合物分布特征及稳定碳同位素组成特征等,并根据这些地球化学特征分析了不同层位烃源岩的母质类型、生烃环境及有机质演化规律。收藏指正
6.Biomarkers from Cretaceous Source Rocks in Jiaolai Basin
胶莱盆地白垩系烃源岩生物标志物收藏指正
7.GEOCHEMICAL METHODS AND RESEARCH STATUS QUO ON LOWER PALAEOZOIC MARINE CARBONATE HYDROCARBON-GENERATING ROCKS
下古生界海相碳酸盐烃源岩地球化学的研究现状收藏指正
8.According to the differences of sedimentary facies and environment, the source rock are divided into four types such as lime-mud reef in platform margin, platform inner sag, deep-water flat slope or continental shelf, abyssal basin, the lime-mud reef type is distributed in platform margin of Upper Ordovician, the remained three types are widely distributed in Cambrian-Ordovician system.
根据沉积相带与沉积环境的不同，可将烃源岩划分为在不同沉积环境中的4种类型烃源岩；台地边缘灰泥丘型烃源岩、台地内凹陷型烃源岩、深水缓坡与陆棚型烃源岩、深海盆地型烃源岩。收藏指正
9.Major hydrocarbon source rocks are in the Cambrian and Ordovician.
寒武-奥陶系烃源岩是该区主力烃源岩;收藏指正
10.H/C CONTENT VARIATION OF ORGANIC MATTER IN SOURCE ROCKS DURING THERMAL EVOLUTION
烃源岩有机质热演化过程中碳氢含量的变化收藏指正