地球科学进展 ›› 2000, Vol. 15 ›› Issue (5): 545 -552. doi: 10.11867/j.issn.1001-8166.2000.05.0545

综述与评述 上一篇    下一篇

热液烃的生成与深部油气藏
张景廉 ①②,王先彬 ,曹正林   
  1. ①中国石油天然气集团公司西北地质研究所,甘肃 兰州 730020;②中国科学院兰州地质研究所,甘肃 兰州 730000
  • 收稿日期:1999-12-01 修回日期:2000-02-21 出版日期:2000-10-01
  • 通讯作者: 张景廉(1941-),男,江苏常熟人,高级工程师,主要从事油气地球化学与成因研究。
  • 基金资助:

    中国科学院“九五”重大项目“深层油气地球化学特征与成因机理研究”(编号KZ951-B1-414)资助。

HYDROTHERMAL HYDROCARBON FORMATION AND DEEP PETROLEUM PROSPECT

ZHANG Jing-lian ①②,WANG Xian-bin ,CAO Zhen-lin   

  1. ①Northwest Institute of Geology,CNPC,Lanzhou 730020;②Lanzhou Institute of Geology,Chinese Academy of Sciences,Lanzhou 730000,China
  • Received:1999-12-01 Revised:2000-02-21 Online:2000-10-01 Published:2000-10-01

热液烃不仅分布于洋底,在大陆也有广泛分布,实验表明:热液对碳酸盐岩和沉积有机质的作用均有油气生成;洋底火山岩流体包裹体、原油、有机质Pb、Sr、Nd同位素均表明地幔流体在油气生成中的作用。认识热液烃的存在对开拓深部油气藏的勘探有重要意义。

Hydrothermal hydrocarbons can occur in the ocean floor and in the continent.Experiments show that hydrothermal fluids catalyze the hydrocarbon generation in carbonates and sedimentary organic matter.The fluid inclusions of the ocean floor volcanic rocks and Pb,Sr and Nd isotopes of petroleum and organic matter also show that mantle fluids play an important role in the hydrocarbon generation.Recognition of hydrothermal hydrocarbon and its implications for the deep petroleum exploration are discussed.

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