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Geochemical Characterization and Mineralogy of Babouri-Figuil Oil Shale, North-Cameroon

机译:喀麦隆北部Babouri-Figuil油页岩的地球化学特征和矿物学

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Organic geochemistry methods such as high temperature combustion, Rock-Eval pyrolysis and gas analysis were used to analyze oil shale from Babouri-Figuil Basin. Results show that the average content of organic matter is 36.25 %wt, while that of mineral matter is 63.75 %wt. The total organic carbon (TOC) is between 15.93 %wt and 26.82 %wt. The HI vs. Tmax diagram indicates an immature Type I kerogen. The average value of the oil potential (S2b) is 149.95 mg HC/g rock. The gases obtained by retort process are H2, CO2, CO and CnH2n, CnH2n+2. Finally, it emerges that, the organic matter of Babouri-Figuil shales was immature or has just reached the beginning of the oil window. The mineralogical study of Babouri-Figuil oil shale has been carried out by means of XRD (X-Ray Diffractometry) and XRF (X-Ray Fluorescence spectrometry). The results show that mineral matrix contains silica, carbonates, sulphates, oxides and clay minerals. Besides, compounds contain metals and metalloids like Fe, In, Ca. The main oxides are SiO2 (majority), CaO, Fe2O3, Al2O3, SO3, and K2O.
机译:利用有机地球化学方法,例如高温燃烧,Rock-Eval热解和气体分析,分析了巴布依菲吉尔盆地的油页岩。结果表明,有机质的平均含量为36.25 %wt,而矿物质的平均含量为63.75 %wt。总有机碳(TOC)在15.93 %wt和26.82 %wt之间。 HI vs. Tmax图表明未成熟的I型干酪根。油势(S2b)的平均值为149.95 mg HC / g岩石。通过蒸煮过程获得的气体为H2,CO2,CO和CnH2n,CnH2n + 2。最终发现,巴布依-菲吉尔页岩的有机物还不成熟或刚刚到达油窗的起点。 Babouri-Figuil油页岩的矿物学研究已通过XRD(X射线衍射法)和XRF(X射线荧光光谱法)进行。结果表明,矿物基质含有二氧化硅,碳酸盐,硫酸盐,氧化物和粘土矿物。此外,化合物还包含金属和准金属,例如Fe,In,Ca。主要氧化物为SiO2(多数),CaO,Fe2O3,Al2O3,SO3和K2O。

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