1) Gaoliu structural zone
高柳构造带
1.
Sedimentary facies in the Neogene Guantao Formation in the Gaoliu structural zone,Nanpu depression;
南堡凹陷高柳构造带新近系馆陶组沉积相研究
2) Liuquan-Caojiawu play
柳泉-曹家务构造带
1.
More than half of natural gas reserves in Langgu depression is from Liuquan-Caojiawu play, but in recent years, the progress of natural gas exploration in Liuquan-Caojiawu play is slow, the main reason is that the key accumulation elements is still ambiguous.
柳泉-曹家务构造带上天然气储量占整个廊固凹陷的一半,但是近年来勘探进展较慢,其制约因素是该区天然气成因类型、分布规律和成藏主控因素不很明确。
3) high position of strucute
构造高垒带
4) high and steep structural zones
高陡构造带
1.
In this region, there are ten rows of high and steep structural zones.
川东地区是四川盆地稳定地块中的相对构造活动带 ,区内发育 10排高陡构造带 ,90年代以来高陡构造带石炭系成组气田勘探获得巨大突破。
5) Gaoshiti-Moxi structure belt
高石梯-磨溪构造带
1.
Gaoshiti-Moxi structure belt is the important exploration area of Sinian Dengying formation.
高石梯-磨溪构造带在加里东运动后形成了相对古隆起区,在印支、燕山和喜山早期仍为古隆起区,喜山晚期运动形成了大型圈闭。
6) tectono-orogen
构造造山带
补充资料：柳带
1.柳条。因其细长如带，故称。 2.相传唐时洛中名妓柳枝娘曾折柳结带赠李商隐以索诗。见《词林海错》卷二引《花寮集》。后因以"柳带"为情人赠物。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条