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Hydrocarbon of source rocks evaluation study of Lokichar Basin, Northwestern Kenya

机译:肯尼亚西北部洛基查尔盆地烃源岩碳氢化合物评价研究

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摘要

The hydrocarbon potential of the sub-surface Tertiary sedimentary rock sequences of the Lokichar basin system (NW-Kenya) has been interpreted using some selective geochemical analysis of rock samples in Loperot-1 Well (denoted as LT-1 Well) for their total organic carbon (TOC) which forms the premise of this study. Understanding the sub-surface structures and depositional environments conducive for hydrocarbon generation and trapping is essential as it forms the basis for exploration. The organic matter richness and degree of thermal alteration and/or maturation are factors useful in evaluating the potential source rocks. Rock-Eval pyrolysis has been employed on selected rock samples with high TOC for quantification of data and this would help in precise identification of phases of hydrocarbon generation.
机译:通过对Loperot-1井(称为LT-1井)中的岩石样品进行了一些选择性地球化学分析,对Lokichar盆地系统(西北-肯尼亚)的地下第三纪沉积岩层的烃潜力进行了解释碳(TOC)构成了这项研究的前提。了解有利于碳氢化合物生成和捕集的地下结构和沉积环境至关重要,因为它构成了勘探的基础。有机物的丰富度和热蚀变和/或成熟度是评估潜在烃源岩有用的因素。 Rock-Eval热解法已用于具有较高TOC的选定岩石样品上,以进行数据定量,这将有助于精确识别烃类生成的阶段。

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