loess landform中文是什么意思

• 黄土地貌

• "loess"中文翻译    n. 【地质学；地理学】黄土。 -al, -ial, - ...
• "landform"中文翻译    地形。
• "landform" 中文翻译 :    地形。
• "loess" 中文翻译 :    n. 【地质学；地理学】黄土。 -al, -ial, -ic adj.
• "collapsible loess slumping loess" 中文翻译 :    土的分类湿陷性黄土
• "accumulation landform" 中文翻译 :    堆积地形
• "actual landform" 中文翻译 :    现在地形
• "aeolian landform" 中文翻译 :    风成地形; 风蚀地形
• "ancient landform" 中文翻译 :    古地貌; 古地形; 古老地形
• "arid landform" 中文翻译 :    干旱地形
• "buried landform" 中文翻译 :    埋藏地形
• "classification of landform" 中文翻译 :    地形分类
• "coast landform" 中文翻译 :    海岸地形
• "coastal landform" 中文翻译 :    海岸地貌；海岸地形; 海岸地形
• "colluvial landform" 中文翻译 :    崩积地形
• "comb landform" 中文翻译 :    梳状地形
• "constructional landform" 中文翻译 :    堆积地形
• "depositional landform" 中文翻译 :    堆积地形
• "drift landform" 中文翻译 :    冰碛地形
• "erosion landform" 中文翻译 :    侵蚀地形
• "erosional landform" 中文翻译 :    侵蚀地形
• "fluvial landform" 中文翻译 :    河成地貌; 河流地貌；河流地形; 流水地貌
• "glacial landform" 中文翻译 :    冰川地貌；冰川地形; 冰河地形
• "glaciated landform" 中文翻译 :    冰蚀地貌
• "history of landform" 中文翻译 :    地形发展史

• From that new conclusion , we know the form of loess landform was built by erosion result from outside forces , which is historical and long - term
  并进一步论证了陕北黄土高原地貌的塑造是以外力侵蚀等因素为主导所形成。外力侵蚀是历史性的，是长期性的。
• The unconformability between the loess landform of shaanbei loess plateau and its bedrock shape was pointed out first after the full demonstration . the top of loess formation of the south part in shaanbei is flat which likes " platform " , the shape of the bedrock is rolling that likes ridge , and the bedrock bended to fold . the top of loess formation of the mid - part in shaanbei is rolling , but the shape of the bedrock below begins to get flat , the top of loess formation of the north part in shaanbei , loess mao district , is much more rolling among them , however , its shape of the bedrock below is the flattest relatively likes the platform shape of loess formation in south
  具体地讲，陕北高原南部的洛） 11黄土源，黄上层顶部相对平坦，地貌类型以黄土源为主格调，而其下伏基岩地层诏皱相对发育，古地势起伏相对较大：陕北高原中部的延安一安塞黄土梁状（为主）丘陵沟壑区，黄土层顶部起伏相对增大，地貌类型以黄土梁为主格调，而其下伏基岩地层槽皱程度趋弱，地层较平缓，古地势起伏相对降低；陕北高原北部的绥德一子洲黄土赤状（为主）丘陵沟壑区，黄土层顶部起伏度相对最大，地貌类型以黄上赤为主格调，而其下伏基底地层以平缓为特征，古地势起伏强度亦相对较低。