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Geochemical characteristics of organic matter from Rudeis and Kareem source rocks, Ras Budran oilfield, central Gulf of Suez, Egypt

机译:埃及苏伊士湾中部拉斯布德兰油田Rudeis和Kareem烃源岩有机质的地球化学特征

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摘要

The organic matters of Rudeis and Kareem formation from Ras Budran oilfield in the central Gulf of Suez, Egypt, were investigated throughout the study of biomarkers and infrared spectrometric analyses. The results showed that Pr/Ph, Pr-C-17, and Ph-C-18 ratios indicated marine source organic matters deposited under reduced condition with a less effect of biodegradation and mature stage of occurrence. The gammacerane index indicated a low-salinity environment of deposition for the initial organic matters existed in the analyzed samples. Steranes distributions show high percentage of C-28 steranes and C-29 steranes compared with C-27 steranes, and low-concentration C-27 diasteranes show generally low ratios indicating anoxic carbonate source rocks. The diasteranes/steranes showed generally low ratios indicating most marine carbonate sources. The tricyclic terpane reflects mature organic matters and originated from marine organic sources.
机译:在整个生物标记和红外光谱分析的研究过程中,对埃及苏伊士湾中部拉斯布德兰油田的Rudeis和Kareem组有机物进行了研究。结果表明,Pr / Ph,Pr / n-C-17和Ph / n-C-18的比值表明海洋源有机物在还原条件下沉积,生物降解作用较小,且成熟期较轻。 γ-角鲨烷指数表明所分析样品中存在的初始有机物的盐度较低。与C-27甾烷相比,Steranes分布显示C-28甾烷和C-29甾烷的百分比高,而低浓度的C-27硬脂烷的比率通常较低,表明缺氧的碳酸盐烃源岩。非甾烷/甾烷的比例通常较低,表明大多数海洋碳酸盐来源。三环萜烯反映了成熟的有机物,并源自海洋有机物。

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