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1)  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
2)  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。
3)  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。
4)  peripheral area of the Hetianhe gas field
和田河气田周缘
5)  Hetian River
和田河
1.
Study on Water Resources Utilization and Ecological Environmental Building of Hetian River in Xinjiang;
新疆和田河水资源利用与绿色走廊生态建设研究
2.
The green corridor of Hetian river is one of three green corridors which cross Taklamakan desert from south to north in the Tarim basin and have important significance in the ecosystem, transportation,politics,economy and so on.
和田河绿色走廊是塔里木盆地中南北穿越塔克拉玛干沙漠的三条绿色走廊之一,具有重要的政治经济、生态、交通意义。
3.
Hetian River is formed by two branches, Yulongkashi and Kalakashi, at Kuoyelashi, and discharges into Tarim River finally.
和田河主要由2条支流组成,即玉龙喀什河和喀拉喀什河,两河在阔什拉什汇合而成和田河,最终汇入塔里木河。
6)  Hotan River
和田河
1.
Study on the Variation Law of the Annual Runoff in Hotan River;
和田河年径流变化规律研究
补充资料:和田河
和田河

    位于中国新疆维吾尔自治区塔里木盆地西南部,是昆仑山北坡最大的河流。旧称和阗河。有玉龙喀什河与喀拉喀什河两源。主流玉龙喀什河出昆仑山北麓;喀拉喀什河出喀喇昆仑山北麓,汇合后始称和田河。在下游分为两支:东支为老和田河,已完全干涸;西支为新和田河,是主流,穿越塔克拉玛干沙漠,在上游水库附近和阿克苏河及叶尔羌河汇合为塔里木河。长806千米。河水靠山地降水及冰川融水补给。在横跨塔克拉玛干沙漠过程中,蒸发、渗漏严重,水量大减。和田河占三大源流补给量为22.5%。洪水期挟带大量泥沙进入塔里木河。
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