1) A Gas Field
A气田
2) gas field
气田
1.
Distribution and genesis of hydrogen sulfide in giant carbonate gas fields of China;
中国碳酸盐岩大气田硫化氢分布特征及成因
2.
Influence of flow velocity of gas at Mo Xi gas field on corrosion;
磨溪气田气体流速对腐蚀的影响
3.
Research on Information Integration Platform for Gas Field Based on Virtual Data Center;
基于虚拟数据中心的气田信息整合平台研究
3) CO_2-reservoir gas
CO_2气田气
1.
Experimental determination of flash evaporation for the CO_2-reservoir gas was made in the temperature range from 292 to 299 K by a static apparatu.
0018(摩尔分率);用静态法高压VLE测定装置对CO_2气田气在292至299 K温度下作了闪蒸实验测定。
4) Hetianhe gas field
和田河气田
1.
Water-soluble gas accumulation process of Hetianhe gas field in Tarim Basin,NW China;
塔里木盆地和田河气田水溶气成藏过程
2.
The difference in geochemical characteristics of natural gases between eastern and western parts in Hetianhe gas field of Tarim basin and its origin;
和田河气田天然气东西部差异及原因
3.
A study on the migration and accumulation efficiency and the source area of natural gas in Hetianhe Gas Field of Tarim Basin
和田河气田天然气运聚效率及源区探讨
5) Hetian river gas field
和田河气田
1.
Role of fracture in controlling the reservoir stratum in the carboniferous bioclastic Limestone member in Hetian river gas field,Tarim basin;
裂缝对和田河气田石炭系生屑灰岩段储层的控制作用
2.
Hetian river gas field,a large-scale carbonate gas pool recently found or proved in Tarim basin,is well-developed in karstification for its major reservoirs such as Ordovician buried hill limestone and Carboniferous bioclastic limestone.
和田河气田是塔里木盆地最近探明的大型碳酸盐岩气田,主要储集层为奥陶系潜山灰岩和石炭系生屑灰岩,岩溶作用十分发育。
6) Hetian River Gasfield
和田河气田
1.
The Carboniferous System in Hetian River Gasfield was mainly formed of a set of interbedded clastic rocks,carbonate rocks as well as interbedded gypsum,mixed plateform shore clastic and shelf facies.
和田河气田石炭系主要发育混合台地、碎屑滨岸和浅海 (陆棚 )沉积相。
2.
Three sorts of diagenetic fractures and five stages of structural fractures developed in Ordovician carbonate rocks in Hetian River Gasfield.
和田河气田奥陶系碳酸盐岩中发育 3类成岩缝和 5期构造缝。
补充资料：南海气田
| 南海气田 位于中国海南省东南海盆地崖南凹陷的西侧。即崖13-1气田。第三纪T圈闭面积为51.5平方千米。气田范围内水深约90米左右，潮汐以不规则的日潮为主。构造为一北西向的短轴背斜，是长期发育的披覆构造。构造边部断层发育，内部也有一些断层，且均为正断层。天然气以甲烷为主，二氧化碳含量较高，乙烷以下组分很低，不含硫化氢气体。1983年4月5日开始钻探崖13-1-1井 ，至1988年底共4口井测试所得工业油气流，证实崖13-1构造是中国已知最大的含气构造，储量达900多亿立方米。 |
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