摘要
它日错深凹陷位于青藏措勤盆地北部坳陷中,其内发育有主含油气系统和子含油气系统。主含油气系统的烃源岩为下白垩统郎山组,储层为上白垩统竟柱山组,盖层为下第三系牛堡组。该含油气系统的关键时刻为距今54Ma,有效圈闭主要是燕山运动晚期和喜山运动早期形成的构造圈闭。
here are two hydrocarbon\|bearing systems in Tazicuo deep depression at the north
of the Cuoqin Basin, namely main\|bearing system and sub\|bearing system. Source rock of the
main\|bearing system is in the Early Cretaceous Langshan Formation, and reservoir rock is in
the Late Cretaceous Jingzhushan Formation, and seal rock is in the Niubao Group of Early
Tertiary. The critical moment of the main\|bearing system is at the time before 54 million years.
The structural traps formed during the Late Yenshan movement, and Early Himalayan cycle
may be filled by hydrocarbon compounds. The region where the Cenozoic Era strata is
preserved completely is favourable for oil and gas exploration.\=
出处
《石油大学学报(自然科学版)》
CSCD
1999年第4期13-15,共3页
Journal of the University of Petroleum,China(Edition of Natural Science)
关键词
青藏地区
措勤盆地
它日错深凹陷
烃源岩
油气评价
Qinghai\|Xizang
area
Cuoqin Basin
Tazicuo deep depression
source rock
oil and gas evaluation\