摘要
受多期构造运动的控制,中新生代盆地类型由早期三叠纪的陆内浅坳、前陆盆地最终转化为统一的陆内盆地,并由此形成了不同盆地发展阶段的相区-相带组合特征。系统地研究和总结其特征,对盆地的油气勘探具有重要意义。
Under the control of multicycle structural movement, the style of Mesozoic-Cenozoic basin has undergone former Triassic shallow hollow inside land, foreland basin and ultimately changed to unitive basin inside land. Moreover, the different facies areas of facies belt combination feature of different basin development stages have been formed. The deposit evolution of each period is strictly controled by structural movement of basin. To systematically study and summarize the character of Mesozoic-Cenozoic deposit evolution in the Tarim basin of Xinjiang has important significance for the basin exploration of petroleum.
出处
《新疆地质》
CAS
CSCD
2001年第4期246-250,共5页
Xinjiang Geology
关键词
塔里木盆地
中新生代
沉积特征
演化
Tarim basin
Mesozoic-Cenozoic
character of deposit
evolution
