石油与天然气地质 ›› 1989, Vol. 10 ›› Issue (1): 35-39.doi: 10.11743/ogg19890106

• 论文 • 上一篇    下一篇

利用磷灰石裂变径迹研究准噶尔盆地生油层热史

潘长春1, 周中毅1, 王庆隆2   

  1. 1. 中国科学院地球化学研究所;
    2. 国家地震局地质研究所
  • 收稿日期:1988-04-22 出版日期:1989-03-25 发布日期:2012-01-16

STUDY OF THERMAL HISTORY OF SOURCE BEDS IN JUNGGAR BASIN BY APATITE FISSION-TRACK

Pan Changchun1, Zhou Zhongyi1, Wang Qinglong2   

  1. 1. Institute of Geochemistry, Academia Sinica;
    2. Institute of Geology, State Bureau of Seismology
  • Received:1988-04-22 Online:1989-03-25 Published:2012-01-16

PDF (PC)

796

被引次数

16

摘要：

作者用磷灰石裂变径迹法研究了准噶尔盆地艾参1井和火南1井主要生油层的热历史。作者认为,艾参1井生油层经历过早期增温、晚期降温的历史,降温过程发生在150Ma 以前;火南1井生油层在距今不到31Ma 的时期曾发生抬升。

Abstract:

The authors studied the thermal history of the main source beds of Aican-1and Huonan-1 Wells in Junggar Basin by apatite fission-track.It is suggested thatthe source beds of Aican-1 Well underwent the history of temperature-increasein the early stage and temperature-decrease in the late stage(150 Ma.ago),andthat the source beds of Huonan-1 Well uplifted in recent 31 Ma.