Timahdit油页岩的热行为(摩洛哥)

Ahmed Saoiabi , Anass Doukkali , Mohamed Hamad , Abdallah Zrineh , Mohamed Ferhat , Yolande Debyser
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引用次数: 4

摘要

对摩洛哥Timahdit地区T层油页岩进行热解研究有两个原因。首先,用气相色谱法测定了热解过程中释放的各种气体的含量。根据原油页岩的Rock-Eval热解结果及其分离的干酪根,认为这些油页岩处于II型演化的开始阶段,具有海相成因,具有良好的母岩品质。极性化合物的含量比烃类化合物的含量更重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Comportement thermique des schistes bitumineux de Timahdit (Maroc)

The pyrolysis of the T layer oil shales of Timahdit (Morocco) was carried out for two reasons. Firstly, using gas chromatography, the contents of the various gases given off during this pyrolysis have been determined. Then, according to Rock–Eval pyrolysis results of the crude oil shales and their isolated kerogen, it has been concluded that these oil shales are located towards the beginning of the evolution of type II, have a marine origin and present qualities of a good mother-rock. Their content of polar compounds is more important than that of the hydrocarbon compounds.

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