The Chaidamu Basin is situated in the north part of Qinghai Province.
柴达木盆地位于青海省北部。
The paper introduces the general situation of exploitation and utilization of salt lake mineral resources in the Chaidamu basin of Qinghai province.
文章介绍了青海省柴达木盆地盐湖矿产资源的概况、特点以及开发利用现状。
The better districts of response of low clod cover to warming were Chaidamu basin in winter and in autumn and Qilian Mountain in spring and Hexi corridor in summer.
低云量对气温响应较好的区域秋、冬季是柴达木盆地，春季是祁连山区，夏季是河西走廊地区。
Through the comprehensive evaluation of strontium resources in Chaidamu basin, the development direction of strontium resources is stated.
通过对柴达木盆地锶资源的综合评价，提出了锶资源的开发方向。
The regional synoptic process with moderate-to-heavy rain appeared in the eastern Chaidamu basin on 7 to 10 July 2005 is analyzed by means of the averaged field data.
应用平均场资料，对2005年7月7~10日柴达木盆地东部出现的区域性中到大雨天气过程进行了综合分析。
The fossils of algae ostracoda foraminifer a gastropod and polychaeta were found in the tertiary carbonate beds in the west of chaidamu basin.
摘要柴达木盆地西部第三系的碳酸盐岩层中发现有藻类、介形虫、有孔虫、腹足类、多毛类等化石。
The fossils of algae, ostracoda, foraminifera, gastropod and polychaeta were found in the tertiary carbonate beds in the west of chaidamu basin.
摘要柴达木盆地西部第三系的碳酸盐岩层中发现有藻类、介形虫、有孔虫、腹足类、多毛类等化石。
The oasis in the eastern Chaidamu Basin, is the most populated and developed area, and hence with serious bio-environment destruction.
柴达木盆地东部的绿洲地区是盆地社会经济活动和人口最为集中的区域，也是生态环境破坏较为严重的区域。
Based on the 1961-2000 observational data of 11 weather stations in Chaidamu Basin, the time-space distribution characteristics of sandstorm weather in Chaidamu Basin are analyzed.
利用196 1 ~ 2 0 0 0年柴达木盆地11个气象站的沙尘暴观测资料，分析了柴达木盆地沙尘暴天气的时空分布特征。
Based on the 1961-2000 observational data of 11 weather stations in Chaidamu Basin, the time-space distribution characteristics of sandstorm weather in Chaidamu Basin are analyzed.
利用196 1 ~ 2 0 0 0年柴达木盆地11个气象站的沙尘暴观测资料，分析了柴达木盆地沙尘暴天气的时空分布特征。
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