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New Insight Into Petroleum Systems of Orenburgh Region - Volgo-ural Basin

机译:对奥伦堡地区石油系统的新洞察 - 伏尔加 - 乌拉尔盆地

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Authors have identified a complex Paleozoic petroleum system represented by 5 major source rocks with good up to excellent characteristics from the point of petroleum potential, reservoirs of porous and fractured types, regional and local seals. Processes of generation, migration, accumulation and conservation of HCs occurred within the limits of this system. Moreover, 2 potential hydrocarbon systems were formed: Mezo-Cenozoic oil system which source rocks within the main part of the area have not entered conditions favorable for HC generation; Ordovician-Silurian petroleum system which source rocks have mostly worked out their petroleum potential and have possibly carried out significant input in petroleum potential of the area. Main source rocks reached oil window zone, and Devonian rocks partially reached gas zone. Main critical moment for Paleozoic rocks - Early Permian time at maximal rock submergence at high geothermal gradient. Subsequently Paleozoic deposits did not reach the same temperatures, i.e. secondary activation of HC generation processes did not occur.
机译:作者已经确定了由5个主要源岩的复杂古生代石油系统,从石油潜力点,多孔和碎片类型,区域和局部密封件的储层,良好的特征。在该系统的范围内发生HCS的生成,迁移,累积和保护的过程。此外,形成了2个潜在的碳氢化合物系统:兆 - 新生型油系统在该地区主要部分内的源岩未进入HC生成的条件; ordovician-silurian石油系统主要制定了他们的石油潜力,并且可能在该地区的石油潜力中进行了大量的投入。主要来源岩石到达油窗区,德文郡岩石部分到达了气区。古生代岩石的主要关键时刻 - 高地热梯度最大岩石淹水早期二叠辑。随后古生代沉积物未达到相同的温度,即,没有发生HC生成过程的二次激活。

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