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The oasis expansion and eco-environment change over the last 50 years in Manas River Valley, Xinjiang
      
The oasis expansion and economic development of the Manas River Valley is one of the most successful examples in Xinjiang.
      
Geodynamic significance of the A-type granites in the Sawuer region in west Junggar, Xinjiang: Rock geochemistry and SHRIMP zirc
      
Sawuer region is located in west Junggar, Jimunai County of Altay district and Hefeng County of Tacheng district, Xinjiang.
      
Negative NEP (carbon sources) were mainly found in Central China, the south of Southwest China, the north of Xinjiang, west and north of Inner Mongolia, and parts of North China.
      
In contrast to the situation in Xinjiang and South Africa, the sediment sequence of the Permian-Triassic transition in the Chahe section (Beds 56-80) become finer upward.
      
The M-D method is applied to developing a scientific scheme of water resources management in the Bosten Lake Basin, Xinjiang, China.
      
An oligotrophic bacterium was isolated from the biological soil crust underlayer in the Xinjiang Gurbantunggut Desert.
      
Responses of streamflow to climate change in the northern slope of Tianshan Mountains in Xinjiang: A case study of the Toutun Ri
      
The Lucaogou Formation carbonate-rich oil shale source rock is exposed at the southern margin of the Junggar Basin, Xinjiang, NW China.
      
During a 4-month period starting from 21 January, 1997, an earthquake swarm of seven major events (Ms?6.0) struck the Jiashi region at the northwestern corner of the Tarim Basin in Xinjiang,, China.
      
The trend in NDVI time series is smoothly increasing, the increases happen mostly in Taiwan, Fujian, Sichuan and Henan provinces and the decreases occur in Yunnan and Xinjiang.
      
During the last 4.00 ka, the region of southern Xinjiang has experienced alternations of relative cold-wet and relative warm-dry periods.
      
It is shown that human activities have an intimate relation with the evolution of paleoclimate in southern Xinjiang.
      
This model is applied to economic development in the Manas oasis of the Xinjiang Uygur Autonomous Region of China.
      
Compared with wind-blown sand, the floating-dust seldom occurs in the high latitude areas such as North Xinjiang and Northeast China.
      
(2) The affected areas of dust storms can be divided into seven sub-regions, that is, North Xinjiang Region, South Xinjiang Region, Hexi Region, Qaidam Basin Region, Hetao Region, Northeastern China Region and Qinghai-Xizang (Tibet) Region.
      
The area of the most frequent occurrence of dust storms and floating-dust is in South Xinjiang Region, and of wind-blown sand in the Hexi Region.
      
The maximum interannual change and variance of dust events during this time happened in South Xinjiang Region and Hexi Region.
      
However, in South Xinjiang Region and North Xinjiang Region, which was less affected by monsoon climate, dust events may occur at any time of the year, less than 50% of the events in this region occur during spring.
      
 

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