1) physical area of Weihe river and its flooding land
渭河河道及滩地自然区
2) Weihe Basin and its neighbouring region
渭河盆地及周邻地区
3) Weihe River bed
渭河河道
1.
The landform evolution of Xianyang since the end of Qin Dynasty contains two aspects,the northward moving of the Weihe River bed and the changing of the edge slope of Xianyang tableland.
秦末以来,秦都咸阳地貌演变包括渭河河道北移和咸阳原边坡地貌变化两个方面。
5) Weihe Terrace
渭河阶地
1.
A high-resolution Holocene loess-soil sequence of the Weihe Terrace at the pediment of the Qinling Mountains was studied multi-disciplinarily.
对秦岭北麓渭河阶地全新世土壤剖面进行的高分辨率分析研究,揭示了该地区全新世土壤剖面的黄土-古土壤序列,是由于季风气候变化引起的以风尘堆积占优势的成黄土期和以生物风化作用占优势的成壤期相互更迭造成的。
6) Weihe basin
渭河盆地
1.
Bearing features of geothermal resources in Weihe basin of Shaanxi;
陕西渭河盆地地热资源赋存特征研究
2.
Analysis of crustal movement feature based on GPS data in Weihe basin and its neighboring region;
用GPS资料分析渭河盆地及邻近地区地壳运动特征
3.
Origin and Source of Soluble Helium Gas in Geothermal Water,Weihe Basin
渭河盆地地热水水溶氦气成因与来源研究
补充资料：河道洪水演进(见河道洪水演算法)
河道洪水演进(见河道洪水演算法)
neaao non郎hUi河道洪水演进yanJ县n 见河道洪水演算法。
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