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1)  Warm slope zone
坡地暖带
1.
Warm slope zone is one of obvious climatic boundary effects distributed extensively in mountain areas.
分析指出,气候边际效应在秦岭-黄淮平原交界带中主要表现为坡地暖带、强降水效应和干旱效应,并对这三种气候边际效应的特征及成因进行了探讨。
2)  landslide area
滑坡地带
1.
Construction of rubble retaining wall on landslide area;
滑坡地带上毛石挡土墙的施工
3)  talus slope zone
坡麓地带
1.
After a lot of practices,it is concluded that during an engineering exploration in the talus slope zone, We should demonstrate the chanres of engineering geological environment caused by the engineering construction, assess its suitability and feasibility to the design and construction, and take correspondent engineering technical measures.
在坡麓地带进行工程勘察时,应注意论证工程建设对工程地质环境的改变,评价其对设计、施工的适宜性和可行性,采取相应的工程技术措施。
4)  border region
边坡地带
1.
Variation characteristics of temperature in northeastern border region of Qinghai-Xizang Plateau;
青藏高原东北部边坡地带气温变化特征研究
5)  topographic ramp
地形坡折带
6)  warm belt
暖带
1.
Acording to the characteristics that there are few systeratical statistics when we research the mountain warm belt, the thesis put forword some methods by means of the air sounding statistics.
在分析暖带含义及特征的基础上,针对暖带研究中普遍存在缺乏系统资料的特点,提出了利用当地探空资料、常规地面气象观测资料及附近地区山地气候资料进行暖带研究的若干方
2.
Warm beltof sloping land exists generally in the low.
同时,区内的低山丘陵普遍存在着坡地暖带,暖带的最暖高度约在海拔350—400m左右。
补充资料:板带轧制速度规程(见板带轧制规程设计)


板带轧制速度规程(见板带轧制规程设计)
speed schedule for plate and strip rolling

  bandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
  
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