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首页> 外文期刊>Chinese science bulletin >Pool-formation and secondary change of biodegraded viscous oils: Case study of reservoir section in the Zhengjia- Wangzhuang Oilfield, Jiyang Depression
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Pool-formation and secondary change of biodegraded viscous oils: Case study of reservoir section in the Zhengjia- Wangzhuang Oilfield, Jiyang Depression

机译:生物降解粘性油的储层形成和二次变化-以济阳De陷郑家王庄油田储层段为例

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摘要

It is demonstrated by various geochemical indexes that the Zhengjia-Wangzhuang Oilfield with viscous crude oil in the Jiyang Depression has been sourced from the contribution of matured source rocks in the upper Es4. The principal cause leading to thedensification of crude oils would be biodegradation, with the degradation level of crude oils being ranked as 2—8; vertically, the biodegradation level increases from the top to bottom of the oil column, with a distinctive biodegradation gradient occurring. Calculated parameters of sterane, terpane and methyl-phenanthrene have indicated that the source-rock's maturity of crude oils and asphaltic sands ranges from 0.7 to 0.9, and based on the calculation of Easy Ro model, the temperature of hydrocarbongeneration in the source rock would be within 120— 140 °C, which coincides with the measurements of reservoir inclusions. The measured homogenization temperature would represent the generation temperature of the source rock, and be fairly different from that of reservoir while being charged with hydrocarbons, which reflects the hydrocarbon-charging to be a fast process, and the period of pool-formation to be consistent with that of peaked generation. According to the evaluation of generation history,the pool-formation could have been occurring in 7—15 Ma. And the biodegradation of crude oils in the study area would be considered to take place in 4—15 Ma based on the examination of biodegradation order and dynamic calculations.
机译:各种地球化学指标表明,济阳De陷郑家王庄油田含黏稠原油,来自Es4上部成熟烃源岩的贡献。导致原油致密化的主要原因是生物降解,原油的降解水平为2-8。在垂直方向上,生物降解水平从油柱的顶部到底部增加,并发生明显的生物降解梯度。甾烷,萜烯和甲基菲的计算参数表明,原油和沥青砂的烃源岩成熟度为0.7至0.9,根据Easy Ro模型的计算,烃源岩的生烃温度为温度在120- 140°C之间,这与储层包裹体的测量值相吻合。测得的均质温度将代表烃源岩的生成温度,并且与充有碳氢化合物时的储层均质温度存在很大差异,这反映了碳氢化合物的充注是一个快速的过程,并且成藏期是一致的与顶峰一代。根据对生成历史的评估,可能在7-15 Ma发生了成藏。根据对生物降解顺序的检查和动态计算,可以认为研究区原油的生物降解发生在4-15 Ma。

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