地球科学进展 ›› 1996, Vol. 11 ›› Issue (4): 327 -335. doi: 10.11867/j.issn.1001-8166.1996.04.0327

学科发展与研究    下一篇

成烃理论的发展——(Ⅰ)未熟油及有机质成烃演化模式
黄第藩   
  1. 石油勘探开发科学研究院石油地质研究所 北京 100083
  • 收稿日期:1995-08-21 修回日期:1996-02-05 出版日期:1996-07-01
  • 通讯作者: 黄第藩,男,1931年9月出生,教授级高级工程师,国务院学位委员会学科评议组成员,主要从事石油地质地球化学研究。

ADVANCES IN HYDROCARBON GENERATION THEORY-(Ⅰ) IMMATURE OILS AND GENERATING HYDROCARBON AND EVOLUTIONARY MODEL

 Huang Difan   

  1. Research Institute of Petroleum Exploration and Development, Beijing 100083
  • Received:1995-08-21 Revised:1996-02-05 Online:1996-07-01 Published:1996-07-01

世界上特别是中国未成熟石油的普遍存在,突破了干酪根热降解成烃的理论模式。研究表明,沉积岩中可溶和不溶有机质,是一个有机联系的整体,共同参与了油气的生成。在成岩作用阶段,干酪根不产烃,未成熟石油来自可溶类脂物的直接降解成烃作用;干酪根的热降解成烃作用主要发生在深成作用阶段早期(Ro=0.5%~1.2%),产生正常原油;后期是以缩合焦沥青裂解产生高成熟轻质油及油裂解成气为主的湿气阶段(Ro=1.2%~2.0%)。提出了一种新的可溶和不溶有机质共同参与成烃的演化模式 

The wide existence of immature oils throughout the world especially in China broke through the hydrocarbon generation theory through kerogen thermal degradation. Studies have shown that soluble and insoluble organic matter are organically connected in the sedimentary rock, both contributing to hydrocarbon generation. In the diagenesis,kerogen can not produce oils, so immature oils derive directly from the soluble lipids. Hydrocarbon generation process through kerogen thermal degradation takes place mainly in the early catagenesis(R o= 0.2% ~1.2%), and the oils generated are normal. In the late catagenesis, hydrocarbon generation comes into wet gas stage(R o=1.2%~2.0%), with pyrrobitumen degenerating into high mature light oils and oils cracking into gases. In this paper,the author presented a new generating hydrocarbon and evolutionary model with soluble and insoluble organic matter both contributing to the generation of hydrocarbon. 

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