首页> 外文期刊>Australian Journal of Earth Sciences >Diversities in biomarker compositions of Carboniferous-Permian humic coals in the Ordos Basin, China
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Diversities in biomarker compositions of Carboniferous-Permian humic coals in the Ordos Basin, China

机译:中国鄂尔多斯盆地石炭系 - 二叠纪腐殖煤生物标志物组成的多样性

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The molecular composition of Carboniferous-Permian coals in the maturity range from 0.66 to 1.63% vitrinite reflectance has been analysed using organic geochemistry to investigate the factors influencing the biomarker compositions of humic coals. The Carboniferous-Permian coal has a variable organofacies and is mainly humic-prone. There is a significant difference in the distribution of saturated and aromatic hydrocarbons in these coals, which can be divided into three types. The Group A coals have biomarker compositions typical of humic coal, characterised by high Pr/Ph ratios, a lower abundance of tricyclic terpanes with a decreasing distribution from C-19 tricyclic terpane to C-24 tricyclic terpane and a high number of terrigenous-related biomarkers, such as C-24 tetracyclic terpane and C-29 steranes. The biomarker composition of Group B coals, which were deposited in a suboxic environment, have a higher abundance of rearranged hopanes than observed in Group A coals. In contrast, in Group C coals, the Pr/Ph ratio is less than 1.0, and the sterane and terpane distributions are very different from those in groups A and B. Group C coals generally have abnormally abundant tricyclic terpanes with a normal distribution maximising at the C-23 peak; C-27 steranes predominates in the m/z 217 mass fragmentograms. The relationships between biomarker compositions, thermal maturity, Pr/Ph ratios and depositional environments, indicate that the biomarker compositions of Carboniferous-Permian coals in Ordos Basin are mainly related to their depositional environment. This leads to the conclusion that the biomarker compositions of groups A and B coals collected from Shanxi and Taiyuan formations in the northern Ordos Basin are mainly related to their marine-terrigenous transitional environment, whereas the biomarker compositions for the Group C coals from Carboniferous strata and Shanxi Formation in the eastern Ordos Basin are associated with marine incursions.
机译:使用有机地球化学分析了成熟度范围为0.66至1.63%的vitriinite反射率的石炭浓度 - 二叠煤的分子组成,以研究影响腐殖质煤的生物标志物组成的因素。石炭纪 - 二叠纪煤具有可变的细胞面积,主要是腐殖质。这些煤中饱和烃的分布存在显着差异,可分为三种类型。该组煤具有典型的腐殖质煤的生物标志物组合物,其特征在于PR / pH比,其特征在于较低的三环萜酯,从C-19三环萜状物与C-24三环萜状物的分布减少和大量有关的人生物标志物,如C-24四环萜壶和C-29 Steranes。沉积在中草核环境中的B族煤的生物标志物组合物具有比在煤中的煤中观察到的重排料较高的丰富。相反,在C煤中,PR / pH比率小于1.0,甾烷和萜状物分布与A和B组中的蛋白分布非常不同。C煤通常具有异常丰富的三环萜座,具有正常分布的异常分布。最大化C-23峰值; C-27 Steranes在M / Z 217质量碎片照片中占主导地位。生物标志物组合物,热成熟度,PR / pH比和沉积环境之间的关系表明鄂尔多斯盆地中石炭酸盐 - 二锰煤的生物标志物组合物主要与其沉积环境有关。这导致得出的结论是,鄂尔多斯盆地山西和太原地层收集的A和B煤的生物标志物组成主要与其海洋植物过渡环境有关,而来自石炭系地层的C煤的生物标志物组合物东部鄂尔多斯盆地的山西形成与海洋侵占有关。

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