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四川盆地高石梯—磨溪地区下寒武统筇竹寺组生烃增压定量评价
刘雯,邱楠生,徐秋晨,常健
1 中国石油大学 ( 北京 ) 油气资源与探测国家重点实验室,北京 102249;2 中国石油大学 ( 北京 ) 地球科学学院,北京 102249
The quantitative evaluation of the pressurization caused by hydrocarbon generation in the Cambrian Qiongzhusi Formation of the Gaoshiti-Moxi area, Sichuan Basin
LIU Wen, QIU Nansheng, XU Qiuchen, CHANG Jian
1 State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum-Beijing, Beijing 102249, China; 2 School of Geoscience, China University of Petroleum-Beijing, Beijing 102249, China

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摘要  生烃增压是油气运移的主要动力,目前对其机制的研究逐渐向定量化方向发展。四川盆地中部高石梯—磨溪地区下寒武统筇竹寺组烃源岩经历了晚二叠世末到中侏罗世末的生油阶段、中侏罗世末到早白垩世初的原油裂解生气阶段和后期干酪根生气阶段。考虑到岩石的整体压缩系数和原油组分特征,建立了适用于腐泥型干酪根连续生烃的增压模型。由生油增压模型计算,筇竹寺组晚二叠世末到三叠纪末,生油初期阶段,超压缓慢增大;早侏罗世初到中侏罗世初期,进入生油窗阶段,超压快速累积,压力系数最大约为2.4;中侏罗世初期到中侏罗世末期,生油作用结束,超压程度略有降低。由原油裂解生气增压模型计算,中侏罗世末期到早白垩世初期,在原油裂解生气过程中,筇竹寺组烃源岩发生幕式排烃,超压程度先增大后减小,最终保持平衡,压力系数约为2.2。除有机质类型、有机质丰度和热史背景外,烃源岩的封闭条件和原油组分是影响生烃增压的主要因素。封闭性越好,烃源岩生油阶段产生的超压越大,烃源岩内的含油饱和度越高。生成的原油含硫量越低,油气转化率越高,压力增大程度越大。
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关键词 : 生油增压;原油裂解生气增压;超压成因;四川寒武系筇竹寺组;高石梯—磨溪地区
Abstract

The overpressure caused by hydrocarbon generation is the main driving force of hydrocarbon migration, the research on its mechanism is gradually becoming quantitative. The source rocks of the Cambrian Qiongzhusi Formation in the Gaoshiti-Moxi area of the Sichuan Basin have experienced the oil generation phase from the end of the late-Permian to the end of the mid-Jurassic, the oil cracking phase from the end of the Jurassic to the early-Cretaceous and the kerogen gas phase later. Considering the overall compressibility of the source rock and the oil component, a quantitative model for the overpressure caused by the continuous process of hydrocarbon generation from sapropel kerogen was established. The pressure evolution calculated by the model for the oil production showed that, from the end of the Permian to the end of the Triassic, the initial stage of oil generation, the excess pressure increased slowly. From the early-Jurassic to the beginning of the mid-Jurassic, the oil window stage, the excess pressure accumulated rapidly with a pressure coefficient up to 2.4. From the beginning of the mid-Jurassic to the end of mid-Jurassic when the oil generation ended, the overpressure reduced slightly. Calculated by the model for oil cracking, from the end of the mid-Jurassic to the beginning of the early-Cretaceous, the overpressure increased first and then decreased subsequently. In the process of oil cracking, the episodic hydrocarbon-expulsion developed in the Qiongzhusi Formation until the pressure balance was reached with a pressure coefficient of about 2.2. In addition to the types and abundance of organic matter and the thermal history, the sealing ability of the source rock and the components of cured oil are also the main factors that affect the calculation accuracy of the quantitative model. The better the closure of source rock, the greater the overpressure accumulated during the oil generation, and the higher the oil saturation retained in the source rock. The lower the sulfur content contained in the oil, the higher the conversion rate of oil to gas was and the greater the pressure formed.

Key words: overpressure caused by oil generation; overpressure caused by oil cracking; causes of overpressure; Qiongzhusi
收稿日期: 2018-04-12     
PACS:    
基金资助:国家自然基金项目(41690133)、国家油气专项(2016ZX05007-003)、北京市科技新星和领军人才培养计划(Z171100001117163)联合资助
通讯作者: 邱楠生,qiunsh@cup.edu.cn
引用本文:   
刘雯,邱楠生,徐秋晨,常健 . 四川盆地高石梯—磨溪地区下寒武统筇竹寺组生烃增压定量评价. 石油科学通报 , 2018, 03:262-271.LIU Wen, QIU Nansheng, XU Qiuchen, CHANG Jian. The quantitative evaluation of the pressurization caused by hydrocarbon genera- tion in the Cambrian Qiongzhusi Formation of the Gaoshiti-Moxi area, Sichuan Basin. Petroleum Science Bulletin, 2018, 03: 262-271. doi: 10.3969/j.issn.2096-1693.2018.03.024
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