Qaidam yellow cattle.
柴达木黄牛
Plant resources in Qaidam Basin.
柴达木盆地资源植物。
Qaidam Basin as a whole, it is a desert scene.
对于整个柴达木盆地, 它是一片沙漠景象。
Precipitation and its characteristics in Qaidam Basin
柴达木盆地的降水及其特性
A study on topsoil pollens in the east of Qaidam Basin
柴达木盆地东部表土花粉分析
Changing the motion state of Tarim Basin and Qaidam Basin.
改变了塔里木和柴达木盆地的运动状态。
Land Types and Their Agricultural Capalility in the Qaidam Basin
柴达木盆地的土地类型和农业生产潜力
Island Arc Volcanic Rocks in the North Qaidam UHP Metamorphic Belt
柴达木北缘超高压变质带中的岛弧火山岩
Altun structural belt and its influence on Tarim and Qaidam basins
阿尔金构造带及其对塔里木和柴达木盆地的影响
Widest point in between Jiuquan and the Qaidam Basin, up to 300 km.
最宽处在酒泉与柴达木盆地之间，达300公里。
Migration of rivers and lakes in the Qarhan Salt playa, qaidam Basin.
察尔汗盐湖的河流改道、湖泊迁移与钾盐富集
Restudy on the Orbital Tuning Time Scale of Deep Core in Qaidam Basin
柴达木盆地深钻孔轨道调谐时间标尺的再研究
Environmental Quality Assessment of the Underground Water in Qaidam Basin
柴达木盆地地下水环境质量评价
TRIGGERING OF LOCAL EARTHQUAKES IN THE QAIDAM BASIN BY THE SUMATRA EARTHQUAKE
苏门答腊地震对柴达木地方震的触发作用
Geological Significance of Paleomagnetic Tests in the Tarim and Qaidam Basins.
塔里木和柴达木盆地的古地磁测试及其地质意义
Eocene Dinoflagellate in Qaidam Basin and Its Significance on Hydrocarbon Source
柴达木盆地始新统沟鞭藻及其油源意义
Paleoclimate evolution in southeast of Qaidam Basin since the last interglacial.
浅析末次间冰期以来柴达木盆地东南部古气候环境演化
Evolution of Ostracoda of the great ice age of last glacial stage in Qaidam Basin
柴达木盆地全球末次冰期介形类动物群的演变
Correlation of Jurassic in Northern Margin of Qaidam Basin and Its Petroleum System
柴达木盆地北缘侏罗系对比及含油气系统
Study on water resources and its reasonable development and use in the Qaidam Basin
柴达木盆地水资源与合理开发利用研究
New Cenozoic Paleomagnetic Data from Qaidam Massif and Their Tectonic Implications.
柴达木地块新生代古地磁新数据及其构造意义
A Study on Origin of Highly Evolutionary Natural Gas in Mahai Gas Field, Qaidam Basin
柴达木盆地马海气田高演化天然气源研究
Petrography Feature of Yingfeng Rapakivi Granite Body in North Margin of Qaidam Basin
柴达木盆地北缘鹰峰环斑花岗岩体的岩相学特征
The Meso Cenozoic basin in the North Qaidam underwent two generations of deformation.
在柴达木北部中、生代盆地发生了二个世代的改造变形。
Mainly in southern Xinjiang, the western Qaidam Basin, Hexi Corridor and other places.
主要分布在新疆南部、柴达木盆地西部，河西走廊等地。
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