石油与天然气地质 ›› 1992, Vol. 13 ›› Issue (1): 57-70.doi: 10.11743/ogg19920106

• 论文 • 上一篇    下一篇

塔里木盆地凝析油气及其运移模式

刘锦才, 陈志高   

  1. 地质矿产部石油地质综合大队 湖北 江陵 434100
  • 收稿日期:1991-07-31 修回日期:1991-12-30 出版日期:1992-03-25 发布日期:2012-01-16

CONDENSATE OIL AND GAS AND THE MIGRATION MODEL IN TARIM BASIN

Liu Jincai, Chen Zhigao   

  1. Comprehensive Research Institute of Petroleum Geology, MGMR, Jiangling, Hubei
  • Received:1991-07-31 Revised:1991-12-30 Online:1992-03-25 Published:2012-01-16

PDF (PC)

462

被引次数

5

摘要：

依据物系(如地下烃类体系)存在状态的内、外因条件和原理,结合塔里木盆地地质、物探、地化、测试等有关资料和国内外研究成果,论述了该盆地已知油气田(藏)地下烃类体系主要赋存形式,以及油气运移的可能模式。地下烃类主要以凝析气或者带轻质油环、或底油的凝析气形式赋存在凝析油气田(藏)中。在低地温、油气生成门限和生成高峰埋深大的特定地质条件下,初次运移是以微裂隙作为主要排出途径,二次运移以油溶于气和游离态油相为主。

关键词: 塔里木盆地, 油气运移, 凝析油, 地温, 地下流体势

Abstract:

According to the conditions and principles of object occurrence and in association with the data of geology,geophysical exploration,geochemistry and testing,it is pro-posed that hydrocarbons in the Tarim Basin are preserved in condensate oil and gas fields(pools)mainly as condensate gas or condensate gas with light oil-rim or bottom oil.Un-der specific geological conditions of low geothermal temperature and great burial depth in threshold and peak of oil-gas generation,the primary migration was finished through mi-crofractures,and the secondary migration took the form of gas dissolved oil and free state oil.