首页> 外文期刊>Journal of Geosciences and Geomatics >Palynofacies Analysis, Organic Thermal Maturation and Source Rock Evaluation of Sedimentary Succession from Oligocene to Early Miocene Age in X2 Well, Greater Ughelli DepoBelt, Niger Delta Basin, Nigeria
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Palynofacies Analysis, Organic Thermal Maturation and Source Rock Evaluation of Sedimentary Succession from Oligocene to Early Miocene Age in X2 Well, Greater Ughelli DepoBelt, Niger Delta Basin, Nigeria

机译:尼日利亚尼日尔三角洲盆地大Ughelli DepoBelt X2井渐新世至中新世早新世至沉积相的古相分析,有机热成熟和烃源岩评价

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One hundred and ninety (190) ditch cutting samples of depth range within 20ft- 11820ft (6.09m-3603.7m) from X2 Well Greater Ughelli DepoBelt, Niger Delta Basin were subjected to palynological and palynofacies analysis combined with sedimentological studies, with a view to define its organic thermal maturation and source rock potential. The analysis of the ditch cutting samples were carried out using reflected light microscope for lithologic description while the palynofacies analysis was carried out using transmitted light microscope. The sedimentological analysis reveals forty-nine (49) lithozones and seven (7) lithofacies units, which were deduced based on their mineralogical composition, textural properties, fossil content, homogeneity and heterogeneity of the lithofacies units. The major lithofacies units penetrated in the well are sandstone, shaly sand, sandy shale, clay, sandy clay, clayey sand and shale. Its associated minerals include quartz, feldspar, calcium carbonate and glauconite. Identification of the petroleum play elements and hydrocarbon potential of the X2 Well were equally established. The result from the palynofacies analysis reveals miospores (pollen and spores), woody plant materials (black wood and phytoclast), amorphous organic matter which were used to characterize the well of its kerogen type and maturity. Fifty (50) lithofacies units were subjected to palynofacies analysis, this indicates a potential for hydrocarbon generation. Presence of the dark brown to black wood plant material (black wood and phytoclast) suggest gas-prone for this well. However, the high abundance of light brown to brown colour index of spore/pollen shows that the organic matter of X2 Well falls within the zone of mature main phase liquid hydrocarbon generation (Spore Color Index of 4-6). Palynofacies analysis of X2 Well shows that the well can yield about 70% of oil and 30% of gas (kerogen type II).
机译:对尼日尔三角洲盆地X2井大Ughelli DepoBelt的深度范围在20ft-11820ft(6.09m-3603.7m)范围内的一百九十(190)个沟渠切割样品进行了孢粉学和古相分析,并结合了沉积学研究,以期定义其有机热成熟度和烃源岩潜力。沟渠切割样品的分析使用反射光显微镜进行岩性描述,而孢粉分析则使用透射光显微镜进行。沉积学分析显示有四十九(49)个岩性带和七(7)个岩相单元,这是根据岩相单元的矿物学组成,质地特征,化石含量,均质性和非均质性推导出的。渗透到井中的主要岩相单元是砂岩,页岩砂,砂质页岩,粘土,砂质粘土,黏土砂和页岩。其相关矿物包括石英,长石,碳酸钙和青绿石。同样确定了X2井的石油采出元素和烃潜力的识别。孢粉分析的结果显示,孢子(花粉和孢子),木本植物材料(黑木和破骨细胞),无定形有机物被用来表征其干酪根类型和成熟度。对五十(50)个岩相单元进行了古相分析,这表明有产生碳氢化合物的潜力。深棕色至黑色木本植物材料(黑色木本和植物破骨细胞)的存在提示该井易产生气体。然而,孢子/花粉的浅棕色至棕色颜色指数很高,表明X2井的有机物处于成熟的主相液态烃生成区域内(孢子颜色指数为4-6)。 X2井的古相分析表明,该井可产出约70%的石油和30%的天然气(II型干酪根)。

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