首页> 外文期刊>Egyptian journal of petroleum >The potentiality of hydrocarbon generation of the Jurassic source rocks in Salam-3x well, North Western Desert, Egypt
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The potentiality of hydrocarbon generation of the Jurassic source rocks in Salam-3x well, North Western Desert, Egypt

机译:埃及西北沙漠Salam-3x井侏罗纪烃源岩的生烃潜力

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The present work deals with the identification of the potential and generating capability of oil generation in the Jurassic source rocks in the Salam-3x well. This depending on the organo-geochemical analyses of cutting samples representative of Masajid, Khatatba and Ras Qattara formations, as well as, representative extract samples of the Khatatba and Ras Qattara formations. The geochemical analysis suggested the potential source intervals within the encountered rock units as follows: Masajid Formation bears mature source rocks and have poor to fair generating capability for generating gas (type III kerogen). Khatatba Formation bears mature source rock, and has poor to good generating capability for both oil and gas. Ras Qattara Formation constituting mature source rock has good to very good generating capability for both oil and gas. The burial history modeling shows that the Masajid Formation lies within oil and gas windows; Khatatba and Ras Qattara formations lie within the gas window. From the biomarker characteristics of source rocks it appears that the extract is genetically related as the majority of them were derived from marine organic matters sources (mainly algae) deposited under reducing environment and take the direction of increasing maturity and far away from the direction of biodegradation. Therefore, Masajid Formation is considered as effective source rocks for generating hydrocarbons, while Khatatba and Ras Qattara formations are the main source rocks for hydrocarbon accumulations in the Salam-3x well.
机译:目前的工作涉及在Salam-3x井的侏罗纪烃源岩中生油的潜力和生油能力的识别。这取决于对代表Masajid,Khatatba和Ras Qattara地层的切削样品以及代表性的Khatatba和Ras Qattara地层样品的有机地球化学分析。地球化学分析表明,在所遇到的岩石单元内的潜在烃源层间距如下:Masajid地层具有成熟的烃源岩,并且具有很弱至中等的生成天然气(III型干酪根)的能力​​。哈塔巴组具有成熟的烃源岩,对石油和天然气的生成能力差至良好。构成成熟烃源岩的拉斯卡塔拉地层对石油和天然气具有良好或非常好的成岩能力。埋葬历史模型表明,Masajid地层位于油气窗口内。 Khatatba和Ras Qattara地层位于气窗内。从烃源岩的生物标志物特征来看,提取物具有遗传相关性,因为它们大部分来自还原性环境中沉积的海洋有机物源(主要是藻类),并朝着增加成熟度的方向而远离生物降解的方向。 。因此,Masajid地层被认为是产生烃的有效烃源岩,而Khatatba和Ras Qattara地层是Salam-3x井中油气成藏的主要烃源岩。

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