甘肃黄土高原是中国黄土高原的一部分。
中国黄土—古土壤堆积是全球冰期—间冰期气候变化与东亚古季风气候变化共同作用的结果。
Chinese Loess Paleosol sediments were just controlled by both the factors of glacial interglacial and paleomonsoon climate.
陕北黄土高原分布于“北山”之北，长城沿线之南，是中国黄土高原地貌景观的重要组成部分。
Shaanbei Loess Plateau, which is located in north Shaanxi from Beishan Mountain to Great Wall, is one of the landscapes of China Loess Plateau.
本文在回顾和分析中国黄土研究历史与现状的基础上，提出了目前中国黄土研究中存在的若干问题。
On the basis of reviewing the study history of China loess and analyzing the present situation in this field, the authors advanced some problems existing in the study of China loess.
中国黄土高原地域广阔，土层深厚，干旱半干旱气候和黄土的特殊性质导致该地区水土流失非常严重。
The loess is thick and widely distributed on loess Plateau in China. The drought and semi-drought climate and the special properties of loess result in serious Soil and water loss in the area.
中国黄土高原的黄土，作为全球变化研究的信息载体，是连续性最好、蕴藏信息最丰富的第四纪陆相沉积物。
As a information carriers of the research of global change, the loess in Chinese loess Plateau is the most consecutive sediment and has the most abundance information since Quaternary.
坐落在陕西省黄土高原上的洛川县，曾经是中国最贫困的地区。
THE county of Luochuan, on the loess plateau of northern Shaanxi Province, used to be one of China'spoorest places.
幸运的是，在中国的一些特殊地理区域，的确存在末次间冰期的一些厚层黄土剖面，其沉积速率与分辨率都特别高。
Fortunately, in some special areas of China, there are some thick loess profiles with higher resolution and sedimentary rate, which were formed in the last interglacial.
唐代以后，随着中国都城东迁北移，导致黄土高原地区发生了深刻的变化，失往了往昔的辉煌。
After the Tang Dynasty, as China capital moving eastward and northward, Loess Plateau underwent profound changes and lost the previous glory.
在中国北方，旧石器文化的很多遗迹都出现在黄土分布区。
Most paleolithic sites were commonly found in loess deposits covering northern China.
黄土地貌属中国典型地貌之一，其分类体系是制图的基础。
Loess geomorphology in China belongs to one of the typical landforms, whose classification system is the foundation of mapping.
中国西北黄土地区产生地震崩落、滑移的最低震级分别为4、5级，或地震烈度5度。
In the loess region of Northwest China, the smallest magnitudes at which the seismic avalanche or slippage can occur individually are MS 4, 5 (about intensity 5).
日本专家学者认为，发生于中国西北沙漠、黄土高原的沙尘通过高空西风气流远距离输送是造成日本黄沙的主要原因。
Specialists and scholars of Japan think that the sand -dust is long -distance transported by upper westerly air from the desert in the northwest China and Loess Plateau in China to Japan.
黄色是地球黄土高原的颜色和黄皮肤中国人的颜色。
Yellow is the color of the earth on the Loess Plateau, the original home of the Chinese people.
中国的黄土高原是人类活动加剧土壤侵蚀，从而使经济受损的一个极端例子。
The Chinese Loess Plateau is an extreme example of human-induced soil erosion and the resulted economic sufferings.
骆亚生。中国典型黄土动力特性及其参数的试验分析。西安：西安理工大学出版社，2000。
Luo Yashang. Experiment analysis on typical loess dynamic features and its parameters in China. Xi 'an: Xi 'an Technology University Publishing House, 2000.
基于中国北方某湿陷性黄土路基工程，利用动力触探和面波法等方法对冲击压实工后的黄土路基进行对比检测。
Based on the collapsible loess subgrade in China northern region, this paper used dynamic sounding method and surface wave method to detect the impact compaction behavior.
黄土是中国独有的特殊地层，不同地域的黄土性质也存有差异。
Loess is a unique special ground in China, the nature of which varies in different regions.
中国西北地区的黄土具有良好的热工特性和结构特性。
Good thermal property and structural quality of loess in northwest region of China makes cave-dwelling local folk house.
黄土高原是中国旱地农业的重要实施区域，降水是其农业生产的主要水分来源。
Loess plateau is the important implement region of dry land agriculture in our country, and the water source of agriculture production mainly depends on precipitation.
干旱和缺水是中国西北黄土高原农业旱作粮食生产区的主要限制因子。
Drought and water shortage is the main limiting factor on the arid-area of agricultural production in the Northwest Loess Plateau.
中国北方连续堆积的晚新生代风成红粘土-黄土，是气候干湿变化的良好地质记录。
There occur thick wind-blown silt deposits which are regarded as a good geological archive of paleoclimatic changes in Late Cenozoic in North China and the central Asia.
黄土高原位于中国中部偏北，内蒙古高原以南，是中国的第三大高原。
Situated in north China and south of the Inner Mongolia plateau, the Loess plateau is the third largest plateau in China.
在分析风水原则和进行实地调查的基础上，我认为山峦起伏，附近又有水的黄土高原很有可能是中国古老风水的发源地。
Based on the analysis of geomantic principles and field observations, I suggest that loess plateau areas where rolling hills and nearby...
在分析风水原则和进行实地调查的基础上，我认为山峦起伏，附近又有水的黄土高原很有可能是中国古老风水的发源地。
Based on the analysis of geomantic principles and field observations, I suggest that loess plateau areas where rolling hills and n...
中国西北地区春季冻结层的融化，也是大规模黄土滑坡发生的诱因。
In Northwest China, the thawing of the frozen layer in spring is the main cause of large-scale landslides in loess region.
我是中国人——黄土高原是我挺起的胸脯，黄河流水是我沸腾的热血；
I am a Chinese -I stood in the Loess Plateau is the chest, Yellow River water is my blood boiling;
我是中国人——黄土高原是我挺起的胸脯，黄河流水是我沸腾的热血；
I am a Chinese -I stood in the Loess Plateau is the chest, Yellow River water is my blood boiling;
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