新疆石油地质 ›› 1994, Vol. 15 ›› Issue (2): 95-101.

• •    下一篇

《热·盆·烃》理论模式的建立

刘国璧, 冯福闿   

  1. 地矿部石油地质研究所 北京 100083
  • 收稿日期:1993-12-29 出版日期:1994-06-01 发布日期:2021-01-19
  • 作者简介:高级工程师 石油地质

A PRELIMINARY DISCUSSION OF THEORETICAL MODEL “GEOTHERMICS·BASIN·HYDROCARBON” AND ITS APPLICATION IN PETROLEUM GEOLOGY

Liu Guobi, Feng Fukai   

  1. Petroleum Geology Institute, MGMR, Beijing 100083
  • Received:1993-12-29 Online:1994-06-01 Published:2021-01-19
  • About author:Senior Engineer, Petroleum Geology

摘要: 《热·盆·烃》理论模式是地矿部石油地质研究所以冯福闿先生为首的集体科研成果,它的基本点是:热力学是地球动力学基础;地球深部热活动宏观上控制着地壳的构造作用和沉积盆地的形成、分布与演化;不同类型盆地的热特征控制着盆地内有机质的演化和油气的相态分布。在烃类原始母质向油气转化的过程中,热作用是多种地质—物理化学因素中最为活跃的因素。它是盆地形成的先导,又是联系盆地与油气之间的纽带。

关键词: 热构造, 地热场, 盆地, 油气演化, 相态

Abstract: Theoretical model “Geothermics·Basin·Hydrocarbon" is a scientific result obtained by a group of researchers led by Mr. Feng Fukai at Petroleum Geology Institute of Ministry of Geology and Mineral Resources(MGMR). Its main points can be described as follows: Geodynamics is based on thermodynamic. Thermal activity in the deeper part of the earth is the major macroscopic control on tectonic movement of crust as well as formation, distribution and evolution of a sedimentary basin. Thermal characteristics of various basins control organic matters alternation and hydro-carbon phase behavior distribution within them. In the process of conversion of kerogen to hydrocarbon, thermal effect the most active among masses of geologic and physio-chemical factors, which is the prerequisite condition for formation of basin and also a link between basin and hydrocarbon.

Key words: Thermal structure, Geothermal field, Basin, Hydrocarbon evolution, Phase behavior