2) Tanggula Range
唐古拉山
1.
Analysis of Global Radiation and Surface Albedo Features in Summer and Autumn in a Permafrost Region of Tanggula Range,Tibetan Plateau;
青藏高原唐古拉山多年冻土区夏、秋季节总辐射和地表反照率特征分析
2.
A Preliminary Analysis of Summer Monsoon Precipitation Features in the Nothern Slopes of Tanggula Range, Tibetan Plateau;
青藏高原唐古拉山北坡夏季风降水特征的初步分析
3.
The Quaternary Glaciations and Glacier Properties in the Tanggula Range;
唐古拉山地区第四纪冰川作用与冰川特征
3) Tanggula Mountain
唐古拉山
1.
Current situation investigation of grassland resource in Tanggula Mountain and Kekexili in Qinghai-Tibet Plateau;
青藏高原唐古拉山及可可西里草地资源现状调查研究
2.
Cenozoic Thrust System and Uplifting of the Tanggula Mountain, Northern Tibet;
西藏北部新生代大型逆冲推覆构造与唐古拉山的隆起
3.
Bias correction for precipitation mesuament in Tanggula Mountain Tibetan Plateau
青藏高原唐古拉山区降水观测误差修正分析
4) Tanggula Mountains
唐古拉山
1.
Origin and Environmental Significance of Major Elements and Sr Isotope Ratios in Rivers Originating from Tanggula Mountains;
唐古拉山发源的河水主要元素与锶同位素来源及环境意义
2.
The Cenozoic fluvial strata, exposed widely in the Tanggula Mountains, detaily recorded the information of the uplift of the northern Tibet Plateau and the paleoenvironmental evolution.
唐古拉山地区广泛出露早新生代陆相地层,较好地记录了青藏高原北部新生代地质构造演化与古环境变迁的过程。
5) to learn from Tang to gain ancient
宗唐得古
补充资料：念青唐古拉峰
| 念青唐古拉峰 念青唐古拉山脉的主峰。位于中国西藏自治区当雄县境内，纳木错湖南侧。北纬30°16′，东经90°20′。海拔7111米。其东南侧为羊八井—当雄深大断裂，相对高差2000米以上，使山体越发显得挺拔。山体高而狭窄，只有30千米宽，缺乏发育大型冰川的宽绰高山面积，只分布着小型冰斗型冰川。 |
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