1) Hongliuhe area
红柳河地区
1.
The major elements geochemical characteristics of the Lower Permian tholeiitic basalts from Hongliuhe area show lower Mg, total alkali (Na_2O+K_2O), and higher Fe, Ti.
红柳河地区下二叠统拉斑玄武岩 ,主要表现为低Mg和全碱 (Na2 O +K2 O)以及高Fe和Ti的特征 ,微量元素Rb ,K ,Sr和Ba等大离子亲石元素富集 ,轻稀土元素 (LREE)相对富集。
2.
There are volumes of Hercynian granitoids of Hongliuhe area in eastern Tianshan Mountains, granitoid plutons,according to intrusive order from earlier to later,are Hexi,Hongliuhe,Hexi and Tianhu in.
东天山红柳河地区分布着大量的海西期花岗岩体。
2) Hongliu area
红柳地区
1.
The fault system of structural horizon in Hongliu area was taken as a plane set to be studied with the fractal dimension.
根据分形几何学的重要参数———分形维数可以反映复杂分形体空间分布的特征,将红柳地区构造层断层系作为一个平面集来进行分形维数的研究。
3) Liushuhe area
柳树河地区
1.
Application of gamma-ray spectrum measure to the external prospecting of Wulaga gold deposit,Liushuhe area,Heilongjiang Province
伽马能谱测量在乌拉嘎金矿外围柳树河地区找矿中的应用
4) Hongliuyuan area
红柳园地区
1.
The application effect of TEM for uranium prospecting in Hongliuyuan area
瞬变电磁法在红柳园地区铀矿勘查中的应用效果
5) Hongliuhe
红柳河
1.
The tectonic evolution of the south Tianshan paleo-oceanic crust inferred from the spreading structures and Ar-Ar dating of the Hongliuhe ophiolite,NW China.;
新疆甘肃交界红柳河蛇绿岩中伸展构造与古洋盆演化过程
2.
Climatic Characteristics of Temperature and Precipitation in Hongliuhe
红柳河气温与降水气候特征分析
3.
The later developed Hongliuhe major anticline, extensional lineation by western trend and HongliuheQianjingongqu shear zone of sinistral t.
宏、微观构造特征研究表明 ,红柳河地区造山期韧性变形大致可分两个阶段。
6) Hongliu river basin
红柳河流域
1.
The notable effects of dams to soil and water conservation and the sand decrease of coming into the Yellow river in Hongliu river basin in north Shaanxi province are analyzed.
分析了陕北红柳河流域库坝工程对该地区水土保持及减少入黄泥沙的显著作用 ,强调了工程措施在治理水土流失中的重要地位 ,并根据红柳河流域库坝群的现状 ,指出了存在的主要问题及其严重危害 ,提出必须加快红柳河流域库坝群的治
补充资料：里下河地区
江苏省中部大体上以里运河、通扬运河、串场河和苏北灌溉总渠为四边的低洼地区。地势四周高，中部低，似锅状。河网密，湖泊多。原来洪涝严重。建国后兴修水利，已成为商品粮基地。
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