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。
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.
出处
《石油与天然气地质》
EI
CAS
CSCD
北大核心
1989年第1期35-39,共5页
Oil & Gas Geology