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1)  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。
2)  caojiawu structure
曹家务构造
3)  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
4)  Qiquanhu structural belt
七泉湖构造带
1.
Forming history of the oil-gas reservoir in Qiquanhu structural belt,Turpan-Hami Basin
吐哈盆地七泉湖构造带油气成藏史
2.
Through comprehensive analysis on geological conditions and process of hydrocarbon accumulation as well as the formation and the evolution of the structure,it is thought that the main factors controlling hydrocarbon accumulation in Qiquanhu structural belt are faults,source-reservoir-caprock arrangement,palaeostructure configuration,and the space-time relation between trap and source rock.
通过对成藏地质条件、成藏过程、构造形成和演化等综合分析,认为控制七泉湖构造带成藏的主控因素是断裂、生储盖的配置、古构造的形态、圈闭与烃源的配置关系,其中断裂是控制成藏的最根本因素,其通过沟通油源、形成圈闭和破坏油气藏等作用控制油气成藏。
5)  Wujia structural belt
武家构造带
1.
The comprehensive study indicated that Wujia structural belt of Bazhou sag is the most favorable exploration region in Minhe basin.
综合研究认为武家构造带是巴州凹陷最有利的勘探区带,2003年在巴州凹陷武家鼻隆构造带武家1号构造成功钻探了武1井,测井综合解释气层8。
6)  Jiaojia fault
焦家构造带
1.
Basic geological characteristics of Xincheng gold deposit and Jiaojia faults have been briefly stated.
概略陈述了新城金矿床及焦家构造带的基本地质特征。
补充资料:柳泉
1.清蒲松龄的号。 2.地名。在山东省淄博市淄川区蒲家庄东山谷中。泉流谷底,谷内绿柳成荫,故名。为蒲松龄故居,因而闻名于世。
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