1) source region of the Yangtze River
长江源地区
1.
Morphological features of river valleys in the source region of the Yangtze River, northern Tibet, and their response to neotectonic movement;
藏北长江源地区河流地貌特征及其对新构造运动的响应
2.
Field mapping reveals that the nearly N-S-trending grabens are the present most prominent structural features in the source region of the Yangtze River, which are also the northernmost grabens ever found on the Qinghai-Tibet Plateau.
长江源地区近南北走向的地堑构造是该区现今最为显著的构造现象,也是青藏高原迄今发现的同类构造发育的最北部地区。
2) the Yangtze River headwaters area
长江源头地区
1.
The writer had investigated and analyzed the actuality of the Yangtze River headwaters area and researched the farmland retirement and environment project and ecological emigration demonstration work,consider organic band the fa.
由于长江源头地区地处青藏高原腹地,其特殊的地理位置和高寒多风干旱的气候,以及人口的增加,资源的过度开发利用使之生态环境十分脆弱,极易遭受破坏。
3) headwaters of Yangtze River
长江源区
1.
Assessment of ecosystem integrity in headwaters of Yangtze River;
长江源区生态系统完整性测量与评价
4) Source Region of Yangtze River
长江源区
1.
Study on Biodiversity Conservation in the Source Region of Yangtze River;
长江源区生物多样性保护研究
2.
Desertification of various degrees have been happening in the source region of Yangtze River.
长江源区存在不同程度的沙化现象，沙地种类多样，分布广泛。
5) the source region of Yangtze River
长江源区
1.
Response of Glaciers in the Source Region of Yangtze River to Global Climate Change;
长江源区冰川对全球气候变化的响应
6) headwaters of the Yangtze River
长江源区
1.
In this paper,the typical catchment of Zuomaoxikongqu in the headwaters of the Yangtze River was taken as an example.
土壤水分是连接气候变化和植被覆盖动态的关键因子,以长江源区北麓河一级支流左冒西孔曲典型小流域为研究对象,通过观测降水特征、植被覆盖情况、土壤特性、土壤水分变化、入渗过程以及蒸散发和凝结,分析了不同植被覆盖下土壤水分变化与降水之间的响应关系。
2.
Then the change of annual runoff distribution in the headwaters of the Yangtze River is discussed.
根据长江源区1956-2000年河流月径流资料,分析了年内分配不均匀系数、完全调节系数、集中度、集中期、变化幅度等特性。
补充资料：长江三峡(见长江)
长江三峡(见长江)
Changjiang Sanxia
Changiiang Sanxia长江三峡(Chan幻iang sanxia)见长江。
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