石油与天然气地质 ›› 2012, Vol. 33 ›› Issue (1): 10-18.doi: 10.11743/ogg20120102

• 油气地质 • 上一篇    下一篇

四川盆地二叠系烃源岩类型与生烃潜力

刘全有1, 金之钧1, 高波1, 张殿伟1, 徐美娥1, 唐瑞鹏2   

  1. 1. 中国石化 石油勘探开发研究院, 北京 100083;
    2. 中国石化 华北石油局, 河南 郑州 712000
  • 收稿日期:2011-10-08 修回日期:2012-01-15 出版日期:2012-02-28 发布日期:2012-03-22
  • 基金资助:

    国家自然科学基金项目(40802028,41173035);国家重点基础研究发展规划("973"计划)项目(2011CB214800);国家科技重大专项(2011ZX05005)。

Types and hydrocarbon generation potential of the Permian source rocks in the Sichuan Basin

Liu Quanyou1, Jin Zhijun1, Gao Bo1, Zhang Dianwei1, Xu Mei’e1, Tang Ruipeng2   

  1. 1. SINOPEC Petroleum Exploration and Production Research Institute, Beijing 100083, China;
    2. SINOPEC NorthChina Petroleum Company, Zhengzhou, Henan 712000, China
  • Received:2011-10-08 Revised:2012-01-15 Online:2012-02-28 Published:2012-03-22

摘要:

通过野外和岩心样品系统采集,对四川盆地二叠系烃源岩元素组成、Rock-Eval、碳同位素组成等地球化学参数分析,确立了二叠系烃源岩干酪根类型以Ⅱ型为主,局部存在Ⅰ型或Ⅲ型;利用烃源岩TOC和热解生烃参数探讨了其生烃潜力,泥岩有机碳含量一般高于灰岩,生烃潜力大。同时,对于高演化海相泥岩和灰岩生烃潜力进行了恢复,提出了高演化泥岩和灰岩生烃潜力的恢复对客观评价我国南方高演化碳酸盐岩具有一定必要性。四川盆地二叠系烃源岩热演化程度普遍高,已达到高-过成熟阶段;在早白垩世二叠系烃源岩进入生气高峰有利于后期天然气聚集成藏,为我国南方海相上组合天然气勘探提供了雄厚的物质基础。

关键词: 干酪根类型, 生烃潜力, 海相烃源岩, 二叠系, 四川盆地

Abstract:

Based on samples from outcrops and cores,we analyzed various geochemical parameters such as elemental component,Rock-Eval and carbon isotopes of the Permian source rocks.The kerogens of the Permian source rocks are dominated by type Ⅱ,with local occurrence of type Ⅰ and/or Ⅲ kerogens.Their hydrocarbon generation capacity is determined by the total organic carbon(TOC)and Rock-Eval parameters.In general,mudstones have a higher TOC,and greater potential for hydrocarbon generation than limestones.We restored the hydrocarbon generation potentials of marine mudstonse and limestones with high thermal maturity,which is necessary for the evaluation of the highly mature source rocks in South China.The Permian source rocks in Sichuan Basin are generally of high thermal maturity at high to post mature stages.During the Early Cretaceous,the Permian source rocks entered into peak hydrocarbon generation and contributed to late gas accumulation in the upper marine assemblage in South China.

Key words: kerogen type, hydrocarbon generation potential, marine source rock, Permian, Sichuan Basin

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