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

Pan Changchun; Zhou Zhongyi; Wang Qinglong

doi:10.11743/ogg19890106

Views : 0 下载量: 771 CSCD: 0

PDF
Export
Share
Collection
Album

STUDY OF THERMAL HISTORY OF SOURCE BEDS IN JUNGGAR BASIN BY APATITE FISSION-TRACK
Vol. 10, Issue 1, Pages: 35-39(1989)
Online First：25 March 1989，

Published：1989
DOI： 10.11743/ogg19890106
稿件说明：

移动端阅览

DOI：

Pan Changchun, Zhou Zhongyi, Wang Qinglong. STUDY OF THERMAL HISTORY OF SOURCE BEDS IN JUNGGAR BASIN BY APATITE FISSION-TRACK[J]. 1989, 10(1): 35-39. DOI： 10.11743/ogg19890106.

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.