1) Minjiang river terrace
岷江阶地
2) Minjiang upriver region
岷江上游地区
1.
Preliminary floristic study on the seed plants of Minjiang upriver region;
岷江上游地区种子植物区系初步研究
3) Minjiang River
岷江
1.
Edge effects of forest landscape in upper reaches of Minjiang River;
岷江上游森林景观边界效应
2.
Acquiring Scientific Outlook for Properly Developing Water Resources of Minjiang River;
树立科学发展观 合理开发岷江水资源
3.
Analysis on flood encounter of Jinsha river and Minjiang river;
金沙江、岷江洪水遭遇分析
4) Min River
岷江
1.
Landscape pattern change in the upper valley of Min River;
岷江上游景观格局变化研究(英文)
2.
Analysis of Edge Influence's Affecting Factors in Min River upper Reaches' Landscape
岷江上游景观边界效应影响因子分析
3.
In this paper,there has been suggested a method of optimization for calculating longitudinal dispersity of natural river,and studied longitudinal dispersion of Jueqi section in Min River.
提出了计算天然河流纵向离散系数的最优化方法 ,并用此法对岷江蕨溪段的试验数据进行处理 ,计算出了该段河流的纵向离散系
5) Mingjiang River
岷江
1.
Long-term dynamics of dry valleys in the upper reaches of Mingjiang River,China;
岷江上游干旱河谷区域空间变化的定量判定
2.
Based on the actual inquiry data,the author study the distribution regularity of landslide in the Mingjiang River between Maowen and Wenchuan County,especially analysis the controlling factors such as the nature of rock and soil bodies,geological structure,and topographic features.
根据野外调查资料,研究了茂汶-汶川段岷江两岸滑坡的发育及分布规律,重点突出了控制滑坡发育的地层岩性、地质构造和地貌三大因素。
3.
The paper has calculated the real and design waste disposal amounts according to the survey of some hydro-power station in the upper reaches of Mingjiang River in July,2006,and got a loss to disposal ratio(LDR),that is,the ratio of loss to disposal in every waste disposal area.
根据2006年7月对岷江上游部分水电站弃渣场的调查,统计分析各渣场现有堆渣量与设计堆渣量的差值,从而得出各渣场流失量与堆渣量的比值,即为流弃比;分析流弃比产生的原因和组成,提出岷江上游地区以石料为主的临河型渣场流弃比取值范围,为以后该地区和其他类似地区的同类型渣场的水土流失预测提供参考。
6) Minjiang
岷江
1.
Simulation of Distributed Hydrological Cycle Model in Minjiang Upriver and Qingyijiang River Basin;
岷江中上游及青衣江流域分布式水循环模拟研究
2.
Land use pattern of Mao county in upper reaches of Minjiang;
岷江上游茂县土地利用格局
3.
This essay based on many examples and academic analyses of exploitation of Minjiang s upper reaches,wants to call on us to explore the hydroenergy with a scientific,reasonable and ordered method, and shows that the current exploitation situation of Minjiang s upper reaches should give us a warning and recollecting.
文章列举了岷江上游流域水能开发中的大量事例,呼吁应科学、合理、有序地开发利用河流水能资源,岷江上游流域水能资源的开发现状,应给人们以警醒和反思。
补充资料：大陆阶地
又名大陆台阶。高出洋盆的大陆块平台，由大陆架及大陆坡组成。平均宽度102公里，平均坡度0.1～4.3°，平均深度从33米至1400～2500米（有时可达3200米），总面积5500万公里2，约占世界海洋总面积的15.3％。其成因同海平面的变化及地壳构造运动有关。前者因大陆冰川消融，导致海面上升，使部分大陆边缘地区被海水淹没。后者因地壳的垂直升降和水平运动，以及地震与火山活动，使部分地壳陷入海底而成。此外，根据板块构造学说，大陆地壳与大洋地壳发生碰撞、对冲运动时，在俯冲带内，地壳发生断裂、弯曲及向下俯冲等，形成陡峭的斜坡，其上即为面积宽广、坡度较平缓的大陆台阶。
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